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15 pages, 19251 KiB  
Article
Mapping Stratigraphy and Artifact Distribution with Unmanned Aerial Vehicle-Based Three-Dimensional Models—A Case Study from the Post Research Area in Northwestern Texas, USA
by Stance Hurst, Eileen Johnson and Doug Cunningham
Drones 2024, 8(11), 684; https://doi.org/10.3390/drones8110684 - 19 Nov 2024
Viewed by 342
Abstract
This study applies UAV-based photogrammetry to map and examine the stratigraphy and archaeological artifact distribution in two localities within the Post research area in northwest Texas. A DJI Inspire 1 UAV equipped with a Zenmuse X5 camera captured nadir and oblique images. These [...] Read more.
This study applies UAV-based photogrammetry to map and examine the stratigraphy and archaeological artifact distribution in two localities within the Post research area in northwest Texas. A DJI Inspire 1 UAV equipped with a Zenmuse X5 camera captured nadir and oblique images. These were processed using Agisoft Metashape to generate 3D models. These models enabled the precise mapping of stratigraphic boundaries, revealing the distinctions between Triassic-age bedrock, Pleistocene-age alluvial deposits, and Holocene-age aeolian sediments. Field surveys from 2022 to 2024 documented over 5000 artifacts with sub-centimeter accuracy, including diagnostic projectile points and ceramics. This research highlights the advantages of UAV-derived 3D models in rapidly and accurately documenting stratigraphy and archaeological data. It demonstrates the value of UAV technology for visualizing landscape-scale processes and artifact contexts, offering a new approach to understanding the interactions between geomorphology and archaeology. The findings contribute to advancing UAV applications in both geomorphological and archaeological research. Full article
(This article belongs to the Special Issue Drone-Based Photogrammetric Mapping for Change Detection)
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<p>The Southern High Plains of northwestern Texas and eastern New Mexico (USA). The Post research area is situated along the eastern escarpment, extending into the westernmost portion of the Rolling Plains of Texas.</p>
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<p>The Post research area and the location of the UAV study area along the South Fork.</p>
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<p>Erosional surface and exposed stratigraphy at Macy Locality 69, documented in 2024 in the Post research area. View to the west.</p>
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<p>Stratigraphic units and the location of mammoth bone within alluvium at Macy Locality 359. View to the southeast.</p>
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<p>Capturing oblique images with DJI Inspire 1 UAV in the Post research area. View to the west.</p>
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<p>Camera location and image overlap of the UAV study area in the Post research area. Figure generated from Agisoft Metashape survey statistics report.</p>
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<p>(<b>A</b>) Field research at Macy Locality 359 within the UAV study area. (<b>A</b>) Crew mapping and collecting archaeological artifacts using the Trimble R8 base station. View to the south. (<b>B</b>) Field crew documenting hearth feature eroding from the top of the aeolian deposit. View to the south.</p>
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<p>Projectile points and ceramic sherd found at Macy Locality 359 and Macy Locality 69 during the 2022–2024 field seasons. (<b>A</b>) Middle Archaic-age projectile point (6000–4500 BP); (<b>B</b>–<b>F</b>) Late Archaic-age projectile points (4500–2000 BP); (<b>G</b>–<b>H</b>) Ceramic-age projectile points (2000–500 BP); (<b>I</b>) ceramic sherd (575–350 BP).</p>
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<p>View of stratigraphic units within the 3D tile model of the UAV study area. View to the southeast. (<b>A</b>) Plan view of the distribution of stratigraphic boundaries, (<b>B</b>) Stratigraphic units mapped across 3D model. Yellow line demarcates scale in meters.</p>
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<p>Three-dimensional view (tile model) of the 90° erosional face of the aeolian unit across the UAV study area, illustrating the distinct vertical exposure of stratigraphy. View to the south. Yellow line demarcates scale in meters.</p>
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<p>Three-dimensional view (tile model) of the aeolian unit and its unconformable boundary above the Triassic Dockum Group in the UAV study area. View to the west. Yellow line demarcates scale in meters.</p>
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<p>Three-dimensional view (tile model) of the columnar erosional pattern of the alluvial unit in the UAV study area. View to the west. Yellow line demarcates scale in meters.</p>
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<p>Three-dimensional view (tile model) of the Triassic Dockum Group bedrock. The distinct red color (10R4/8) of the Triassic bedrock contrasts with other stratigraphic units, showing its topographic influence and forming a lateral boundary to the deposition of alluvial sediments. View to the south. Yellow line demarcates scale in meters.</p>
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<p>Overall distribution of artifacts (white points) across the UAV study area, visualized on the 3D tile model. View to the east. Yellow line demarcates scale in meters.</p>
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<p>Linear distribution of artifacts (white points) influenced by slope and water flow, visualized on the 3D tile model, highlighting the impact of geomorphological processes on artifact dispersal. View to the east. Yellow line demarcates scale in meters.</p>
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<p>Visualization of artifacts (red points) within their stratigraphic context. View to the west. Yellow line demarcates scale in meters.</p>
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<p>Visualization of the distribution of the aeolian sediment unit in relation to the distribution of artifacts across the UAV study area, using the 3D tiled model in Metashape. View to the south. Yellow line demarcates scale in meters.</p>
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29 pages, 13372 KiB  
Article
Identifying Anthropogenic Versus Natural Submerged Prehistoric Landscapes: Two Case Studies from the Sicilian Channel
by Ehud Galili, Liora Kolska Horwitz, Ilaria Patania, Amir Bar and Isaac Ogloblin Ramirez
J. Mar. Sci. Eng. 2024, 12(11), 1981; https://doi.org/10.3390/jmse12111981 - 2 Nov 2024
Viewed by 626
Abstract
In submerged landscapes, distinguishing anthropogenic features versus natural ones is often challenging. We have developed a set of criteria to validate the identification of submerged anthropogenic remains that include examining the geological context, sea-level considerations, associated archaeological finds (including coastal survey), and documenting [...] Read more.
In submerged landscapes, distinguishing anthropogenic features versus natural ones is often challenging. We have developed a set of criteria to validate the identification of submerged anthropogenic remains that include examining the geological context, sea-level considerations, associated archaeological finds (including coastal survey), and documenting the broader archaeological context. Furthermore, our experience demonstrates that, while progress has been made in applying remote-sensing technologies to detect anthropogenic features on the seabed, there is no substitute for direct, visual assessment by an underwater archaeologist for verification of their anthropogenic status. We have applied these criteria to examine two published case studies detailing suspected anthropogenic stone features on the seabed in the Sicilian Channel. Our examination has led us to conclude that both localities are not anthropogenic features. The Pantelleria Vecchia Bank features represent natural outcrops on a submerged paleo-landscape that were shaped by depositional and erosional processes during transgression and regression periods. The suspected Lampedusa cultic site comprises natural features that are located on a submerged neo-landscape formed due to erosion and retreat of the coastal cliff since the mid-Holocene, when the sea level reached its present level. Full article
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<p>Location of the two studied sites depicted by red circles, water depth isobaths in m. (Map: Sara Elettra Zaia, Esri, CGIAR, Source. Esri, USGS.)</p>
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<p>A multibeam image of the Pantelleria Vecchia Bank (modified after [<a href="#B60-jmse-12-01981" class="html-bibr">60</a>]).</p>
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<p>Rock blocks on Ridge 1, modified after [<a href="#B60-jmse-12-01981" class="html-bibr">60</a>].</p>
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<p>Rock blocks on Ridge 2, modified after [<a href="#B59-jmse-12-01981" class="html-bibr">59</a>].</p>
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<p>The isolated monolith, modified after [<a href="#B60-jmse-12-01981" class="html-bibr">60</a>] <span class="html-italic">(</span><a href="#jmse-12-01981-f004" class="html-fig">Figure 4</a>: lateral view from the SW).</p>
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<p>Lampedusa Island and the location of sites mentioned (map: modified after Sentinel-2 cloudless layer for 2023, with bright overlay layer by EOX—4326).</p>
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<p>Photograph showing active cliff retreat in the studied locality creating caves, a sea stack and submerged neo-landscape, and the location of the suspected anthropogenic site (E. Galili).</p>
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<p>Boulders on the sea bottom at the suspected cultic site off Lampedusa (for location, see below in <a href="#jmse-12-01981-f010" class="html-fig">Figure 10</a>, nos. 1,2) (E. Galili).</p>
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<p>Plan of the suspected cultic site (courtesy of Diego Ratti, modified after Figure 2.88 in [<a href="#B63-jmse-12-01981" class="html-bibr">63</a>]).</p>
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<p>Above: multi-beam image of the site with the location of the main features: 1, 2—concentrations of boulders suspected to represent cultic circles, 3—flat surface of in situ eroded rock, 4—suspected zoomorphic feature or natural erosional feature (courtesy of Diego Ratti and CNR Centro Nazionale delle Ricerche). Below: aerial photo of the suspected site (courtesy of Diego Ratti).</p>
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<p>Suspected zoomorphic feature or erosional feature at the Lampedusa site (for location, see <a href="#jmse-12-01981-f010" class="html-fig">Figure 10</a>, no. 4) (E. Galili).</p>
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<p>Typical landscape, fresh avalanches, and cliff retreat on the west and northwest coast of the Lampedusa site (E. Galili).</p>
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<p>Blocks of beachrock outcrop under coastal, landward erosion north of Akko (Israeli coast), looking north (E. Galili).</p>
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<p>Blocks of beachrock outcrop under coastal, landward erosion north of Akko (Israeli coast), looking southwest (E. Galili).</p>
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<p>Lingoid ridge (Lr) developed on a Type 3 intertidal platform (C refers to transversal cracks in the beachrock plates; Ds refers to detached blocks of beachrock washed shoreward), modified after [<a href="#B81-jmse-12-01981" class="html-bibr">81</a>] (see plate 13 in [<a href="#B80-jmse-12-01981" class="html-bibr">80</a>]).</p>
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<p>Water emerging from a geyser chimney (pipe/hole) on a rocky (aeolianite sandstone—kurkar) section of the Israeli coast, near Kibbutz Neve Yam (E. Galili).</p>
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<p>Left: Cala Ocello Bay and location of the MIS5e deposit, center and right: close-ups of <span class="html-italic">Strombus bubonius</span> mollusks (E. Galili).</p>
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<p>Top: ancient rock-cut bollard in the modern Lampedusa harbor, bottom: ancient rock-cut bollard in Cala Pisana Bay (E. Galili).</p>
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<p>Coastal erosion, recent active retreat of the coastal escarpment, and creation of a submerged neo-landscape at the foot of the cliff schematic drawing, modified after Figure 5 in [<a href="#B112-jmse-12-01981" class="html-bibr">112</a>]).</p>
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20 pages, 20958 KiB  
Article
Geology, Archaeology, and Historical Studies of the Late 16th Century Plinian Eruption of Raung Volcano: A Potential Case for Disaster Geotourism in Ijen UNESCO Global Geopark, East Java, Indonesia
by Firman Sauqi Nur Sabila, Mirzam Abdurrachman, Asep Saepuloh, Idham Andri Kurniawan, Abdillah Baraas, Dwi Fitri Yudiantoro and Hery Kusdaryanto
Geosciences 2024, 14(11), 284; https://doi.org/10.3390/geosciences14110284 - 24 Oct 2024
Viewed by 976
Abstract
The enigmatic major eruption in the late 16th century, believed to have originated from Raung, the most active stratovolcano in the Ijen UNESCO Global Geopark in East Java, Indonesia, has ignited significant debate among researchers and historians due to its profound impact on [...] Read more.
The enigmatic major eruption in the late 16th century, believed to have originated from Raung, the most active stratovolcano in the Ijen UNESCO Global Geopark in East Java, Indonesia, has ignited significant debate among researchers and historians due to its profound impact on the region. This research aims to substantiate Raung as the likely source of the major eruption by integrating geological, archaeological, and historical data. This study synthesizes current findings and explores ongoing debates surrounding historical volcanic activities. Eruption parameters suggest that the late 16th century eruption exhibited a Plinian type, characterized by an explosive eruption column reaching the stratosphere, widespread pumiceous tephra fallout, and pyroclastic density current (PDC). Stratigraphic succession reveals that the eruption occurred in five phases, with deposits from 10 eruptive units. These deposits are mainly concentrated on the northwestern flank of Raung. Archaeological findings, historical records, and local legends converge to pinpoint the occurrence of this catastrophic event in the late 16th century. These diverse sources estimate that the eruption resulted in approximately 10,000 casualties, marking it as one of the most significant volcanic disasters in the past 500 years. The implications of this eruption extend beyond historical documentation, providing a critical case study for advancing disaster mitigation strategies through geotourism in the geopark area. Moreover, the eruption record outcrops identified in this study can be proposed as potential new geosites within the Ijen UNESCO Global Geopark, enhancing its educational and touristic value. We propose the Jebung Kidul, Alas Sumur, and Batu Sappar sites as potential disaster-based geosites, considering that these sites record the eruption process and preserve archaeological structures. This addition would not only commemorate the historical event but also promote awareness and preparedness for future volcanic activities in the region. Full article
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<p>The location of Raung Volcano in the Sunda Arc system compared to other active volcanoes (<b>a</b>). Raung Volcano’s position in the western part of the Ijen UNESCO Global Geopark area (<b>b</b>). Geomorphology of the Raung Volcanic cone with summit caldera, in the western Ijen Volcanic Complex (<b>c</b>). Photograph capturing the 2015 eruption, which emitted gas from the active vent inside the caldera and basaltic lava flows on the caldera floor (<b>d</b>).</p>
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<p>Geological map of Raung Volcano showing the distribution of eruptive products and the delineation of different deposits [<a href="#B38-geosciences-14-00284" class="html-bibr">38</a>]. The map illustrates the spatial extent and variety of volcanic deposits across various periods of Raung’s volcanic activity.</p>
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<p>Summary of volcanic activity at Raung Volcano based on Volcanology and Geological Hazard Mitigation Center (CVGHM) records starting from the 16th century (<b>a</b>). The explosivity level of Raung’s eruptions generally transitioned from VEI &gt; 4 (1593, 1638, 1817) with Plinian and sub-Plinian types to VEI &lt; 4 with Vulcanian types and smaller VEI &lt; 3 eruptions with Strombolian-Hawaiian types (<b>b</b>). Plot of eruption intervals against eruption index (VEI) (<b>c</b>). The red cross symbol is an eruption event.</p>
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<p>The composite stratigraphic column of the deposits from the late 16th century Raung’s eruption is divided into 10 units across 5 eruption phases. Units A and B belong to Phase 1, while units C and D are associated with Phase 2. Phases 1 and 2 are identified as the opening stages of the eruption. Unit E represents a lava flow that records the transition from explosive to effusive activity during the eruption. Units F and G are recognized as the climax of the eruption, characterized by massive deposits and widespread pyroclastic material. Finally, units H, I, and J capture the closing phase of the eruption, consisting of smaller eruptions and lahar flows.</p>
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<p>Outcrop recording almost the entire unit in Batu Sappar site (<b>a</b>), massive basaltic lava flow of unit E (<b>b</b>), unit G overriding lava flow of unit E (<b>c</b>), unit G overlying blocky lava unit E (<b>d</b>).</p>
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<p>Exposure of representative deposits of pyroclastic fall units A, C, and F (<b>a</b>). The contact between deposit units G and H (<b>b</b>). Contact of unit A and phase 4 deposits (<b>c</b>). Lahar deposits that overlaid units A, C, and F (<b>d</b>). The massive layer of white lapilli-sized pumiceous rock with the angular-shaped white pumiceous rock has contact without soil separation (<b>e</b>).</p>
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<p>Stratigraphic correlation oriented NE-SW, perpendicular to the wind direction, illustrates the distribution of deposit layers from the northern flank to the western flank of Raung. The PDC deposits of units B, D, and G are concentrated on the northwestern flank of Raung, filling the paleo-valley between Suket and Gadung, with several fall deposits observed on the flank of Gadung.</p>
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<p>Stratigraphic correlation oriented NW-SE, parallel to the wind direction, illustrates the lateral distribution of deposit layers from the northwestern flank of Raung. The PDC deposits of funits B, D, and G are concentrated in the proximal area, while the fall deposits are observed in both the proximal and distal areas.</p>
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<p>Stratigraphic correlation oriented NW-SE, both parallel and against the wind direction, illustrates the lateral distribution of deposit layers from the northwestern and southeastern flanks of Raung. The eruptive deposits are concentrated on the northwestern flank of the volcano and are less observed in the proximal area of the southeastern flank.</p>
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<p>TAS classification of volcanic rocks from the Raung eruption based on alkali and silica content. The geochemical composition of eruptive products ranges from basaltic-trachyandesite to dacite. The sample from another eruption like Ijen Caldera [<a href="#B58-geosciences-14-00284" class="html-bibr">58</a>] and Old Raung [<a href="#B38-geosciences-14-00284" class="html-bibr">38</a>] also plotted.</p>
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<p>Findings of brick structures covered by fallout deposits in Ledokombo (LDK station) (<b>a</b>). Stratigraphy of fallout deposits in Ledokombo site (LDK station) (<b>b</b>). Excavation of bricks in Alas Sumur (<b>c</b>) and excavation of bricks in Jebung Kidul Village (<b>d</b>) with the Tourism and Culture Department of Bondowoso Government and the East Java Cultural Heritage Conservation Center.</p>
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<p>Schematic representation and bibliographical chart of studies on the 16th century eruption of Raung. The chart compiles scripts and key references detailing the eruption’s impact, historical records, and scientific analyses, providing a comprehensive overview of the event’s significance [<a href="#B10-geosciences-14-00284" class="html-bibr">10</a>,<a href="#B25-geosciences-14-00284" class="html-bibr">25</a>,<a href="#B26-geosciences-14-00284" class="html-bibr">26</a>,<a href="#B27-geosciences-14-00284" class="html-bibr">27</a>,<a href="#B28-geosciences-14-00284" class="html-bibr">28</a>,<a href="#B29-geosciences-14-00284" class="html-bibr">29</a>,<a href="#B32-geosciences-14-00284" class="html-bibr">32</a>,<a href="#B34-geosciences-14-00284" class="html-bibr">34</a>,<a href="#B35-geosciences-14-00284" class="html-bibr">35</a>,<a href="#B36-geosciences-14-00284" class="html-bibr">36</a>,<a href="#B37-geosciences-14-00284" class="html-bibr">37</a>,<a href="#B38-geosciences-14-00284" class="html-bibr">38</a>,<a href="#B41-geosciences-14-00284" class="html-bibr">41</a>,<a href="#B53-geosciences-14-00284" class="html-bibr">53</a>,<a href="#B54-geosciences-14-00284" class="html-bibr">54</a>,<a href="#B55-geosciences-14-00284" class="html-bibr">55</a>,<a href="#B56-geosciences-14-00284" class="html-bibr">56</a>,<a href="#B57-geosciences-14-00284" class="html-bibr">57</a>].</p>
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<p>Matrix showing potential sites for additional disaster-based geosites in the Ijen UNESCO Global Geopark. The matrix evaluates sites based on parameters such as a representation of eruptive units and phases, existing legends or myths associated with the locations, and the potential functions of the geosites.</p>
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<p>Map showing the locations of Jebung Kidul, Alas Sumur, and Batu Sappar in comparison with other existing geosites within the Ijen UNESCO Global Geopark. The map highlights the spatial relationships between these sites and their integration into the broader geosites network in the Geopark area.</p>
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<p>The traces of the capital relocation of Blambangan from 1596 or the late 16th century [<a href="#B44-geosciences-14-00284" class="html-bibr">44</a>], starting from Panarukan to the north of Raung, rotating counterclockwise to the south and east until reaching its current position in Banyuwangi (<b>a</b>). The disappearance of the traces of ancient place names, which happens to be in the same area as the estimated distribution of eruption products and the locations of archaeological findings in the west, north, and northwest of Raung based on a Hayam Wuruk journey map [<a href="#B60-geosciences-14-00284" class="html-bibr">60</a>] (<b>b</b>).</p>
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19 pages, 8890 KiB  
Article
Forgotten Ecological Corridors: A GIS Analysis of the Ditches and Hedges in the Roman Centuriation Northeast of Padua
by Tanja Kremenić, Mauro Varotto and Francesco Ferrarese
Sustainability 2024, 16(20), 8962; https://doi.org/10.3390/su16208962 - 16 Oct 2024
Viewed by 768
Abstract
Studying historical rural landscapes beyond their archaeological and cultural significance, as has typically been addressed in previous research, is important in the context of current environmental challenges. Some historical rural landscapes, such as Roman land divisions, have persisted for more than 2000 years [...] Read more.
Studying historical rural landscapes beyond their archaeological and cultural significance, as has typically been addressed in previous research, is important in the context of current environmental challenges. Some historical rural landscapes, such as Roman land divisions, have persisted for more than 2000 years and may still contribute to sustainability goals. To assess this topic, the hydraulic and vegetation network of the centuriation northeast of Padua were studied, emphasising their multiple benefits. Their length, distribution, and evolution over time (2008–2022) were vectorised and measured using available digital terrain models and orthophotographs in a geographic information system (GIS). The results revealed a significant decline in the length of water ditches and hedgerows across almost all examined areas, despite their preservation being highlighted in regional and local spatial planning documents. These findings indicate the need for a better understanding of the local dynamics driving such trends and highlight the importance of adopting a more tailored approach to their planning. This study discusses the GIS metrics utilised and, in this way, contributes to landscape monitoring and restoration actions. Finally, a multifunctional approach to the sustainable planning of this area is proposed here—one that integrates the cultural archaeological heritage in question with environmental preservation and contemporary climate adaptation and mitigation strategies. Full article
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<p>Location of the case study in Italy (map by Francesco Ferrarese).</p>
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<p>The Museum of the Roman Centuriation in Borgoricco, located in front of the municipal building (photographed by Tanja Kremenić, 2023).</p>
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<p>Research workflow.</p>
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<p>Research area of the Municipality of Borgoricco, with the primary features of cartographic analysis: ditches, hedges, and the inner grid area. The base map is the DTM from 2022 (map by Tanja Kremenić).</p>
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<p>Land use in the Municipality of Borgoricco according to Corine Land Cover terminology (source: Corine Land Cover 2018, updated 2020, base map OF2022). From the overlap of the OF2022 and CLC2018/20 layers, it can be noted that what was designated as ‘urban fabric’ is not limited to the visible grey segment. Urban sprawl has, in the meantime, taken over a larger part of the municipal area, particularly along roads (cardines and decumani).</p>
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<p>Three of the four major pressures on the ancient Roman hydraulic network of water ditches are the demand for industrial areas (in the upper left) and residential areas (central and dispersed in the photo) and the urban promotion of the ancient grid (in the lower part of the photo), in which the water ditches have been replaced by a small water reservoir, visible in this photo as wetland vegetation (photographed by Tanja Kremenić, 2024).</p>
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<p>The fourth principal threat is intensive agriculture and the resulting land consolidation. Although the landscape presented in the photo is characterised by organic agricultural production, it is a simplified landscape (photographed by Tanja Kremenić, 2024).</p>
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<p>Water ditches are being converted into subsurface pipe networks to accommodate bike paths or being neglected and becoming part of allotments (photographed by Mauro Varotto, 2024).</p>
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<p>The reduction in water ditches in m per <span class="html-italic">centuria</span> for the ‘grid area’ of the Municipality of Borgoricco from 2008 to 2022. Numbers on the map are the <span class="html-italic">centuriae</span>’s identifiers (map by Tanja Kremenić).</p>
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<p>The length of water ditches per <span class="html-italic">centuria</span> derived from the on-screen digitisation of the DTM and OF from 2022 (map by Tanja Kremenić).</p>
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<p>The change in the length of hedgerows between 2007 and 2022, within the grid area of the Municipality of Borgoricco, on a per <span class="html-italic">centuria</span> basis. Green indicates an increase in hedgerows, while colours from yellow to red indicate a reduction in hedgerows, measured in meters (map by Tanja Kremenić).</p>
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<p>The length of hedges per <span class="html-italic">centuria</span> derived from the on-screen digitisation of the OF 2022 (map by Tanja Kremenić).</p>
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<p>The percentage (%) of hedgerows adjacent to water ditches based on the ratio between mapped ditches and hedges from the DTM and OF 2022 (map by Tanja Kremenić).</p>
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<p>The resolution and availability of information from the base cartography used: DTM2008, DTM2022, OF2007, and OF2022. On DTM2022, the tesselation of ditches can be noted, which corresponds to the areas covered by dense rows of trees and hedges (visible on OF2022) that obstructed the LiDAR signal. DTM2008, although older, reveals the ditches more clearly. Location: Borgoricco case study, <span class="html-italic">centuria</span> 25 (Lusore torrent is visible on the left side).</p>
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17 pages, 22884 KiB  
Article
Disconnected Flows, Eroded Landscapes: A Case Study of Human Impact on a Judean Desert Water System
by Nurit Shtober-Zisu and Boaz Zissu
Land 2024, 13(10), 1679; https://doi.org/10.3390/land13101679 - 15 Oct 2024
Viewed by 599
Abstract
The Bir el-Umdan cistern, a prominent archaeological site in the Judean Desert, is one of the largest and best preserved water systems in the region. Hewn in chalk, the cistern area measures 114 m2 and has a ~700 m3 volume. Two [...] Read more.
The Bir el-Umdan cistern, a prominent archaeological site in the Judean Desert, is one of the largest and best preserved water systems in the region. Hewn in chalk, the cistern area measures 114 m2 and has a ~700 m3 volume. Two massive columns, each with a base diameter of 2.5 m, support the ceiling within the cistern’s interior. This impressive structure is estimated to date back to the Hellenistic to Late Antiquity periods based on its architectural characteristics. Historical records indicate that the cistern was documented on 19th-century maps but disappeared from the 1935 and 1943 British Mandate maps. Its reappearance on the 1967 Survey of Israel map includes an upstream road disconnecting the cistern from its natural drainage basin. Despite its renovation in the 2010s, the cistern’s water supply remains limited due to its reduced catchment area, which now constitutes only 25% of its original size. Runoff coefficients calculated for the cistern’s drainage basin are relatively low (1.4% to 8.1%) compared to other desert regions. We analyzed the 21st-century runoff coefficient and recurrence interval over the original drainage basin (0.12 km2) to estimate the water volumes in antiquity. Our analysis suggests that using an 8.1% runoff coefficient, the estimated water volume is 806 m3, implying a cistern overflow every 6–7 years. A more conservative estimate using a 5% runoff coefficient yields a water volume of 500 m3 and a 15-year recurrence interval. Sediment analysis reveals that silt particles dominate the sediment accumulated in the cistern and its upstream sedimentation basins. The consistent grain size distribution throughout the system indicates rapid water flow during flood events. Reconstructing the sedimentation history is challenging due to potential maintenance and possible dredging and cleaning operations. Full article
(This article belongs to the Special Issue Surface Runoff and Soil Erosion in the Mediterranean Region)
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<p>(<b>a</b>) Shaded relief map of the Levant: TA–Tel Aviv, JL–Jerusalem, DS–Dead Sea; (<b>b</b>) regional hydrological drainage net of the studied area with the specific drainage basin of the Bir el-Umdan cistern (red), neighbor drainage basin connected in 2010 (black); (<b>c</b>) geological map and section of the drainage basin, after [<a href="#B39-land-13-01679" class="html-bibr">39</a>]; (<b>d</b>) aerial photo of the Judean Desert and study site (red arrow). Note the road (black arrow) and the vegetated alluvial fan (green arrow) dammed by the road.</p>
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<p>Variability of the water level in the cistern as pictured in November 2020 (<b>left</b>), when the water depth was ca. 100 cm, and January 2022 (<b>right</b>), when the cistern floor was dry. The photos were retrieved from Instagram (<a href="https://www.instagram.com/gili.shani/" target="_blank">https://www.instagram.com/gili.shani/</a>, accessed on 1 September 2024). Publication courtesy of Gili Shani (<a href="https://yoga-gili.com/" target="_blank">https://yoga-gili.com/</a>, accessed on 1 September 2024).</p>
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<p>Bir el-Umdan water system: (<b>a</b>) aerial photo of the upper components of the system: six sedimentation basins constructed to catch the coarse sediments, three troughs to water the herds, part of the hillside conduit, channel and spillway. The upper sedimentation basin is delineated by a double white dashed line, indicating a small depression without surrounding construction. Water enters the cistern after filtration and exits only by manual extraction with a bucket through the outlet opening in the cistern’s roof. Human for scale, encircled white; (<b>b</b>) the underground cistern, freshly plastered and painted. Note the water levels on the walls. (<b>c</b>,<b>d</b>) Lidar images in horizontal and lateral planes, showing the relations between the subaerial and subterranean components of the Bir system. Three-dimensional scan prepared by Dr. Danny Bickson.</p>
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<p>Longitudinal profile of the Bir el-Umdan channel up to the Gorfan stream confluence (see also <a href="#land-13-01679-f001" class="html-fig">Figure 1</a>b).</p>
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<p>Historical maps illustrating the area of the cistern location (red arrows) and the neighboring road: 1880 [<a href="#B50-land-13-01679" class="html-bibr">50</a>], 1943 [<a href="#B51-land-13-01679" class="html-bibr">51</a>], and 1967 [<a href="#B56-land-13-01679" class="html-bibr">56</a>]. Red square in the 1967 map points on the aerial photo frame in <a href="#land-13-01679-f006" class="html-fig">Figure 6</a>b.</p>
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<p>(<b>a</b>) Aerial photo from 1945 (PS; [<a href="#B49-land-13-01679" class="html-bibr">49</a>]) showing the water cistern location (red dot); (<b>b</b>) aerial photo (2021) of the same location [<a href="#B52-land-13-01679" class="html-bibr">52</a>], showing the cistern (red dot). Modern constructions are easily identified, including the dirt road, the hillside conduit, and the buildup of an alluvial fan upstream of the road (visible as a darker area in the channel).</p>
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<p>Aerial photo of the cistern area (red arrow). Note the three gully heads that begin by the road due to back-erosion (blue arrows) and the alluvial fan formed upstream (Af), highlighted by increased vegetation. The road and the alluvial fan disconnect the upper and lower reaches of the channel. The road lacks drainage pipes that cross underneath.</p>
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<p>Aerial photo (2022) and map of cistern Bir el-Umdan. The surrounding slopes, and the two nearby and currently inaccessible cisterns (2 and 3). Note the hillside conduits that convey first-order channels into the cisterns. Conduit 1, in particular, captures a southern channel, expanding the catchment area by approximately 25%. Note the alluvial fan, formed by the road, disconnecting cistern 1 from its natural catchment.</p>
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<p>Daily rainfall at Maàle Amos (<a href="https://ims.gov.il/he/ClimateAtlas" target="_blank">https://ims.gov.il/he/ClimateAtlas</a>, accessed on 1 September 2024) and water depth in the cistern. The water levels represent observations collected by visitors and do not reflect the runoff volume of individual rainfall events. n.d. = no data.</p>
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<p>Sediment samples were collected from the slope (s), the sedimentation basins (1–6) and from the cistern (7–9). (<b>a</b>) Grain size distribution; (<b>b</b>) Lidar imaging of the sedimentation basins and the cistern. Three-dimensional scan prepared by Dr. Danny Bickson; (<b>c</b>) land photo of the sedimentation basins.</p>
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<p>Evaluation of water volume potential at the original drainage basin size, based on the runoff coefficient obtained for an event with a seven-year recurrence interval.</p>
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23 pages, 12592 KiB  
Article
Braiding Fruits and Flowers as a Wish of Prosperity and Victory over Death in the Carved Festoons of Ancient Rome
by Alessandro Lazzara, Alma Kumbaric, Agnese Pergola and Giulia Caneva
Plants 2024, 13(19), 2795; https://doi.org/10.3390/plants13192795 - 5 Oct 2024
Viewed by 704
Abstract
Plant motifs had a significant role in ancient cultures, with decorative, artistic, and communicative values. However, little knowledge exists of the botanical composition of festoons, widely used in Greek-Roman art. We analysed 81 festoons, exclusively from sculpture artworks, collected from 13 museums and [...] Read more.
Plant motifs had a significant role in ancient cultures, with decorative, artistic, and communicative values. However, little knowledge exists of the botanical composition of festoons, widely used in Greek-Roman art. We analysed 81 festoons, exclusively from sculpture artworks, collected from 13 museums and archaeological sites in Rome (1st century BC–3rd century AD). Using iconographic sources and previous data, we identified the represented species and analysed their abundance and composition using statistical methods (Cluster Analysis, Principal Components Analysis) and diversity indexes (Shannon and Evenness). We documented 3081 botanical elements, identifying 30 taxa, in which fruits with leaves (45%) or alone (10%) represented the most common ones. Laurus nobilis and Quercus cfr. robur were the most frequently depicted species, followed by “pomes” (Pyrus, Malus, Cydonia), Vitis vinifera, Punica granatum, and Ficus carica. Festoons with one or two species can be easily distinguished from those with multiple species, often arranged with figs or vine branches at the ends, with symbolic aims related to fertility, rebirth, and abundance values. A balanced botanical composition also exists, with flowers typically in the middle and a species distribution that is not casual. The results enriched our comprehension of ancient Roman society, considering funerary and celebrative events. Full article
(This article belongs to the Special Issue Advances in Vegetation History and Archaeobotany)
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<p>Examples of mono-specific (<b>a</b>,<b>b</b>) and multi-specific (<b>c</b>,<b>d</b>) festoons in different typologies of artworks. (<b>a</b>) Base (inventory number 417) from the <span class="html-italic">Museo Nazionale Romano</span> (PM-8, INV. 417); (<b>b</b>) frieze fragment from the Diocletian baths (TD-82, INV. 78137-78139); (<b>c</b>) funerary altar of <span class="html-italic">Lucius Pinnius Celsus</span> from <span class="html-italic">Palazzo Altemps</span> (PA-3, INV. 8599 bis); (<b>d</b>) festoon from the internal monument of Ara Pacis. (Photos by the Authors,—Courtesy by the Ministry of Culture, <span class="html-italic">Museo Nazionale Romano</span>).</p>
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<p>The analysed festoons of the considered Roman museums and archaeological parks listed in chronological order, showing the number of festoons (first column) from each, the number of artworks and the correlated typology (second column) where the festoons are represented.</p>
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<p>(<b>a</b>) Relative frequency of the species among the festoons, considering the values higher than 1%; (<b>b</b>) occurrence frequency of the species, i.e., number of festoons presenting them.</p>
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<p>The most recurrent botanical elements in the festoons (<b>columns a</b>) compared to correspondent fresh plants in nature (<b>columns b</b>). Photos of the carved elements by the authors, except for n. 1, 2, 11, 13, 14a (<a href="http://www.collezionegalleriaborghese.it" target="_blank">www.collezionegalleriaborghese.it</a> accessed on 6 December 2023); (<b>a</b>): 1, 11, 13, 14a from Festoon F-GB1; 2a from F-CB1; 6, 7, 8, 12a from F-TD 108; 5, 10, 15a from F-AP1; 9a from F-PA 7; 4a from F-CMM3; 3a from F-TAS. (<b>b</b>) Pictures of fresh plants: 1, 7, 9, 10, 11, 12, 14, 15b (from <a href="https://dryades.units.it/cercapiante/index.php" target="_blank">https://dryades.units.it/cercapiante/index.php</a> accessed on 30 March 2024), 5, 8, 3, 12, (GBIF, Global Biodiversity Information Facility, <a href="https://www.gbif.org" target="_blank">https://www.gbif.org</a> accessed on 30 March 2024), 2b, 4b, 13b (Acta plantarum, <a href="https://www.actaplantarum.org/" target="_blank">https://www.actaplantarum.org/</a> accessed on 30 March 2024), 6b (photo by the authors).</p>
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<p>General scheme of the organisation of Roman carved festoons. (<b>a</b>) Festoon with semicircular shape with the central area which divides the festoons into two halves, without a central botanical element (n = 43) as in the sarcophagus with festoon with heroes and marine motifs from the <span class="html-italic">Galleria Borghese</span> (F-GB 3); (<b>b</b>) festoons composed by a central area and a central botanical element (n = 30) as in the Circular Altar <span class="html-italic">from Centrale Montemartini</span> (F-CMM 4); (<b>c</b>) the anomalous festoons in the Altar dedicated to Mars, Venus, and Silvanus from <span class="html-italic">Palazzo Massimo</span> (F-PM 9) with a vertical distribution of the elements, without a central area (n = 8). (<b>a</b>) Courtesy by <span class="html-italic">Galleria Borghese</span> Museum, <a href="http://www.collezionegalleriaborghese.it" target="_blank">www.collezionegalleriaborghese.it</a> accessed on 6 December 2023); (<b>b</b>,<b>c</b>) photo by the authors—Courtesy of the Ministry of Culture, <span class="html-italic">Museo Nazionale Romano</span>).</p>
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<p>Examples of sequences of plants (see the legend for colours) in the four groups of typologies (Altars (I), Sarcophagi (II), Urns (III), Friezes (IV)) of festoons with central elements (n = 44) (numeration starts from the centre until the two ends). The festoons from artwork PM-9 have been excluded for their different structure organisation and the low state of preservation.</p>
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<p>Trends of Shannon (Black line) and Evenness (Red Line) indexes of the multi-specific festoons, related to the plant diversity values across the festoons, in relation to: (<b>a</b>) the context of provenance (Funerary, Sacral, Unknown); (<b>b</b>) the typology of artefacts (Altars, Sarcophagi, Friezes, Urns); (<b>c</b>) the chronology.</p>
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<p>(<b>a</b>) Cluster analysis showing the similarities of species in the different festoons; (<b>b</b>) similarities of festoons according to their botanical composition considering their context of provenance (red = sacral, black = funeral; green = unknown).</p>
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<p>PCA of the species in relation to the typologies of artefacts (Urns, Altars, Sarcophagus, Friezes).</p>
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12 pages, 2225 KiB  
Article
Health and Heritage: The Bioarchaeological Discovery of a Probable Case of Developmental Dysplasia in an Adult Subject
by Nicol Rossetti, Roberta Fusco, Carmelo Messina, Arianna Vanni and Marta Licata
Heritage 2024, 7(10), 5295-5306; https://doi.org/10.3390/heritage7100249 - 24 Sep 2024
Viewed by 685
Abstract
Imagining life before the advent of modern medical treatments is challenging. Today, congenital dysplasia is typically diagnosed within the first months of a child’s life, allowing for timely intervention. In the past, however, this condition often went unrecognized and untreated, as evidenced by [...] Read more.
Imagining life before the advent of modern medical treatments is challenging. Today, congenital dysplasia is typically diagnosed within the first months of a child’s life, allowing for timely intervention. In the past, however, this condition often went unrecognized and untreated, as evidenced by archaeological findings that document the presence of congenital dysplasia persisting into adulthood. We present the case of the individual recovered from the hypogeal cemetery of Santa Maria Maggiore in Vercelli, Italy, a funerary context dated from the 18th to the 19th century. Using macroscopic and radiographic analyses, various morphological irregularities were identified, consistent with the characteristics of developmental hip dysplasia. The skeletal remains identified as FU12 SU151 include a right os coxa and femur, belonging to an adult female. The femur features a 90-degree femoral head angle and a shortened neck with nodules. The acetabulum shows significant morphological changes, including a triangular shape and absence of lunate surfaces, deviating from the normal structure for femoral articulation. CT scans revealed a void within the acetabulum, indicating an absence of material. Despite preservation challenges that restrict the identification of definitive signs, our findings offer valuable insights into possible developmental dysplasia in historic skeletal remains. This research provides insights into the impact of untreated congenital conditions on past populations, underscoring the importance of preserving and studying such remains to enhance our understanding of historical health issues. Full article
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<p>Funerary Unit 12, Sector III. (<b>A</b>) Map of Italy with the location of the site. (<b>B</b>) Planimetry of the hypogeal cemetery: funerary Unit 12, Sector III in the red circle [<a href="#B37-heritage-07-00249" class="html-bibr">37</a>]. (<b>C</b>) Detail of FU12 [<a href="#B38-heritage-07-00249" class="html-bibr">38</a>].</p>
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<p>FU12 SU151. (<b>A</b>) Anterior view of the femur and posterior view of the os coxa individual. (<b>B</b>) Posterior view of the femur and anterior view of the os coxa.</p>
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<p>(<b>A</b>) Anterior view of the femur with magnification of the depression and microporosity in the femur neck and the evident spongy texture, both in the proximal and distal epiphyses. (<b>B</b>) Posterior view of the femur, with the red circle indicating the osteophytic beak.</p>
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<p>(<b>A</b>) Lateral view of the coxa, with the yellow arrow indicating the acetabulum and the red arrow indicating the exostosis. (<b>B</b>) Detail of the posterior view of the coxa, with the red circle indicating the raised bony area. (<b>C</b>) Anterior view of the coxa showing the normal width of the greater sciatic notch.</p>
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<p>Anteroposterior plane CT image in anterior view, with the red circle indicating the void visible in the acetabulum zone.</p>
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24 pages, 3861 KiB  
Article
Aesthetics of Afro-Andean Smoking Culture: Early Modern Peruvian Tobacco Pipes at the Edge of the Atlantic World
by Brendan J. M. Weaver, Jerry Smith Solano Calderon and Miguel Ángel Fhon Bazán
Arts 2024, 13(5), 143; https://doi.org/10.3390/arts13050143 - 20 Sep 2024
Viewed by 1215
Abstract
Although situated at the geographic margin of the early modern Atlantic World, the Pacific coast of Peru was an important region in the development of African diasporic material culture. Adopting an interdisciplinary material historical approach, we present the first systematic discussion of the [...] Read more.
Although situated at the geographic margin of the early modern Atlantic World, the Pacific coast of Peru was an important region in the development of African diasporic material culture. Adopting an interdisciplinary material historical approach, we present the first systematic discussion of the known Afro-Atlantic-style tobacco pipes to be archaeologically recovered in Peru. Eighteen Afro-Atlantic-style tobacco pipes or pipe sherds dating to Peru’s Spanish colonial period have been identified across sites in the coastal cities of Lima and Trujillo and from a vineyard hacienda in rural Nasca. Tobacco pipes are among the most recognized and debated forms of early modern Atlantic African and diasporic expressions of material culture, as such, they present a powerful entry point to understanding the aesthetic consequences of colonial projects and diverse articulations across the Atlantic World. The material history of Afro-Atlantic smoking culture exemplifies how aesthetics moved between localities and developed diasporic entanglements. In addition to the formal analysis and visual description of the pipes, we examine historical documentation and the work of nineteenth-century Afro-Peruvian watercolorist Francisco (Pancho) Fierro to better understand the aesthetics of Afro-Andean smoking culture in Spanish colonial and early Republican Peru. Full article
(This article belongs to the Special Issue Black Artists in the Atlantic World)
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<p>Map of Peru with the locations of Trujillo, Lima, and Nasca indicated. Map by B. Weaver.</p>
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<p>Map of present-day Lima with the locations of the sites yielding Afro-Atlantic pipes. Map by B. Weaver.</p>
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<p>Afro-Atlantic-style pipes recovered from Quinta de Presa. (<b>A</b>) complete pipe, (<b>B</b>) pipe shank fragment, and (<b>C</b>–<b>F</b>) pipe bowl fragments. Edited from a photograph courtesy of Rubén Garcia Soto. Layout by J. Solano.</p>
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<p>Pipes recovered from Casa Bodega y Quadra. (<b>A</b>,<b>B</b>) Afro-Atlantic-style pipes with short shank, (<b>C</b>) Afro-Atlantic-style pipe with slightly longer shank, and (<b>D</b>) tin-enameled short-shank pipe. Photographs by M. Fhon. Layout by J. Solano.</p>
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<p>Lateral views of Afro-Atlantic-style pipes recovered from Parque de La Muralla (<b>A</b>,<b>B</b>). Photographs by Diana Allccarima Cristómo. Layout by J. Solano.</p>
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<p>Anterior and lateral views of Afro-Atlantic-style pipe recovered from Barrios Altos. Photograph courtesy of ProLima. Layout by J. Solano.</p>
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<p>Anterior and lateral views of Afro-Atlantic-style pipe recovered from Church of the Trinitarians. Photograph courtesy of ProLima. Layout by J. Solano.</p>
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<p>Lateral views of Afro-Atlantic-style pipe recovered from Alameda Chabuca Granda. Photograph courtesy of ProLima. Layout by J. Solano.</p>
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<p>Lateral and posterior views of Afro-Atlantic-style pipe recovered in Trujillo. Photograph and layout by J. Solano.</p>
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<p>Afro-Atlantic-style pipes recovered at the site of the Hacienda San Joseph de la Nasca (<b>A</b>,<b>B</b>). Photographs by B. Weaver. Layout by J. Solano.</p>
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<p>(<b>Left</b>): Detail of Fierro Palas, Francisco (attributed), ca. 1850. Indian Woman Smoking Cigar in Front of Breadstand, watercolor on paper, H 19.7 × 24.6 cm. Accession Number: 1967.36.20. Yale University Art Gallery, New Haven. Photograph in public domain. (<b>Right</b>): Detail of Fierro Palas, Francisco (attributed), ca. 1850. Woman with Basket on her Head, watercolor on paper, H 22.5 × 17.1 cm. Accession Number: 1967.36.32. Yale University Art Gallery, New Haven. Photograph in public domain.</p>
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<p>Upper register: Fierro Palas, Francisco (attributed), ca. 1850. Interior of an Inn, watercolor on paper, H 44.7 × 58.8 cm. Accession Number: 1967.36.40. Yale University Art Gallery, New Haven. Photograph in public domain. Lower register: details of Interior of an Inn featuring an Afro-Peruvian man (<b>left</b>) and woman (<b>right</b>) smoking tobacco pipes.</p>
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15 pages, 3106 KiB  
Article
Ancient Genome of Broomcorn Millet from Northwest China in Seventh Century CE: Shedding New Light to Its Origin and Dispersal Patterns
by Xiaolan Sun, Yifan Wang, Yongxiu Lu, Yongxiang Xu, Bingbing Liu, Yishi Yang, Guoke Chen, Hongru Wang, Zihao Huang, Yuanyang Cai, Zhengquan Gu, Xiaoxia Wang, Guanghui Dong and Yucheng Wang
Agronomy 2024, 14(9), 2004; https://doi.org/10.3390/agronomy14092004 - 2 Sep 2024
Viewed by 793
Abstract
Broomcorn millet (Panicum miliaceum) is among the earliest domesticated staple crops in the world’s agricultural history and facilitated the development of several early agrarian cultures, particularly those originating in northern China. However, the propagation route of broomcorn millet in China from [...] Read more.
Broomcorn millet (Panicum miliaceum) is among the earliest domesticated staple crops in the world’s agricultural history and facilitated the development of several early agrarian cultures, particularly those originating in northern China. However, the propagation route of broomcorn millet in China from the Middle Ages to the present remains unclear. The aim of this study is to explore the genetic affinity between ancient and modern millet samples, trace the genetic origins and diffusion pathways of broomcorn millet, and provide insights into its domestication and spread. To achieve this, we sequence ancient DNA from broomcorn millet remains excavated from the Chashan Village cemetery (AD 691) in Gansu Province, China. Phylogenetic and population genetic analyses, integrating ancient and modern millet genomes, reveal a close genetic relationship between ancient millet and contemporary millet from Ningxia Province (445 km away from Chashan Village), suggesting a potential origin for the Chashan millet. This finding aligns with the tomb’s epitaph, which documents the reburial of the tomb’s owner, who was originally buried in Ningxia, and provides important archaeological evidence for understanding the interaction between geopolitical dynamics and the natural environment in northwest China during the late seventh century. Furthermore, outgroup-f3 and D statistics evidence suggests substantial genetic interactions between ancient millet and modern varieties from the Loess Plateau, Huang-Huai-Hai Plain, and Northeast Plain, indicating the dispersal route of broomcorn millet, along with human migration routes, from the northwest to northern China and ultimately to the northeast region, starting from the Middle Ages onward. This study enhances our understanding of millet’s genetic history, offers a novel perspective on burial archaeology, and provides valuable insights into the origins, domestication, and diffusion of broomcorn millet. Full article
(This article belongs to the Section Farming Sustainability)
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<p>(<b>a</b>) The 9 divisions of agricultural regions in China, including the Northeast China Plain (NE), Southwest Yunnan–Guizhou Plateau (SW), Northern arid and semiarid region (NA), Southern China (SC), Sichuan Basin and surrounding regions (SB), Middle–Lower Yangtze Plain (M), Qinghai–Tibet Plateau (QT), Loess Plateau (LP), and Huang-Huai-Hai Plain (HH). (<b>b</b>) The location of the Chashan Village burial site. (<b>c</b>) West side of the tomb chamber. (<b>d</b>) Ultra-microscopic photos of broomcorn millet plant remains. (<b>e</b>) Plant remains collected from all the torn silk bags.</p>
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<p>(<b>a</b>) Ancient and modern sample locations. (<b>b</b>) The NJ phylogenetic tree of all the samples based on the p-distance. (<b>c</b>,<b>d</b>) PCA clustering of all the samples.</p>
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<p>Population structure of ancient broomcorn millet and modern samples based on the admixture analysis.</p>
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<p>(<b>a</b>) Outgroup-f3 statistics for different millet populations. (<b>b</b>) D-statistic for different millet populations. All results that reach statistical significance are indicated by asterisks (corresponding |Z| &gt; 3).</p>
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<p>Historical patterns of human dispersal in China. Route 1 represents the southward migration of northern populations after the An Lushan Rebellion (~1300 BP). Route 2 traces the migration from the LP region to the HH region (~600 BP). Route 3 reflects the movement from the HH region to the NE region (~200 BP to modern times).</p>
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21 pages, 38212 KiB  
Article
Revisiting Gubbio: Settlement Patterns and Ritual from the Middle Palaeolithic to the Roman Era
by Marianna Negro, Nicholas Whitehead, Caroline Malone and Simon Stoddart
Land 2024, 13(9), 1369; https://doi.org/10.3390/land13091369 - 26 Aug 2024
Viewed by 621
Abstract
The Gubbio Revisited project, initiated to reinterpret the archaeological evidence collected during the 1980s Gubbio Project, primarily by a conversion from a paper to a digital record, has revealed significant insights into the evolving settlement patterns and religious expression in the Gubbio valley [...] Read more.
The Gubbio Revisited project, initiated to reinterpret the archaeological evidence collected during the 1980s Gubbio Project, primarily by a conversion from a paper to a digital record, has revealed significant insights into the evolving settlement patterns and religious expression in the Gubbio valley in Central Italy. This reanalysis of the survey evidence underscores the rhythms of settlement and ritual practice from the Neolithic through the Bronze and Iron Ages, into Roman times. Key excavations in the 1980s at Monte Ingino, Monte Ansciano, San Marco Romano, and San Marco Neolitico added details not only of settlement activity but also of embedded ritual, evidenced by material culture including pottery, faunal remains, and votive offerings. The foundation myth of indigenous religious practices, even amidst Roman influence, is documented through the Iguvine Tables alongside the introduction of new cults, showcasing a blend of local and imperial religiosity, a common feature in the Roman world. This research enriches the understanding of Gubbio’s historical and cultural landscape, emphasizing the demographic rhythms of the valley alongside the integral role of ritual in its societal evolution. Full article
(This article belongs to the Special Issue Archaeological Landscape and Settlement II)
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<p>(<b>A</b>) The location of Gubbio in the wider region of Central Italy; (<b>B</b>) The essential geology of the Gubbio basin.</p>
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<p>The areas surveyed in the valley of Gubbio. (<b>A</b>) The fields surveyed; (<b>B</b>) A heat map representation of the fields surveyed to permit a better comparison with the density plots that follow. Essentially five transects (1–5) were placed across the valley.</p>
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<p>(<b>A</b>) Distribution of Palaeolithic sites in the valley; (<b>B</b>) Heatmap of Palaeolithic activity based on the spreads of lithic material recorded during the Gubbio Survey, using kernel densities estimation, with the same range as <a href="#land-13-01369-f004" class="html-fig">Figure 4</a>. Numbers 1–6 refer to clusters of sites cited in the text.</p>
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<p>(<b>A</b>) Distribution of Mesolithic (Epi-palaeolithic) sites in the valley; (<b>B</b>) Heatmap of Mesolithic (Epi-palaeolithic) activity based on the spreads of lithic material recorded during the Gubbio Survey, using kernel densities estimation with the same range as <a href="#land-13-01369-f003" class="html-fig">Figure 3</a>. Numbers 1–5 refer to clusters of sites cited in the text.</p>
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<p>(<b>A</b>) Distribution of Neolithic sites in the valley; (<b>B</b>) Heatmap of Neolithic activity based on the spreads of lithic and ceramic material recorded during the Gubbio Survey, using kernel densities estimation. A. Red dot is San Marco. ‘Numbers 1–4 in B refer to clusters of sites cited in the text.</p>
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<p>Distribution of San Marco Neolithic dates relative to the regional picture presented here [<a href="#B9-land-13-01369" class="html-bibr">9</a>] Calibration data based on [<a href="#B10-land-13-01369" class="html-bibr">10</a>,<a href="#B11-land-13-01369" class="html-bibr">11</a>]. A–H refer to significant changes in the “demographic” curve.</p>
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<p>(<b>A</b>) Distribution of Chalcolithic sites in the valley; (<b>B</b>) Heatmap of Chalcolithic activity based on the spreads of lithic and ceramic material recorded during the Gubbio Survey, using kernel densities estimation.</p>
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<p>(<b>A</b>) Distribution of Bronze Age sites in the valley and (inset) excavated sites around Gubbio; (<b>B</b>) Heatmap of Bronze Age activity based on the spreads of ceramic material recorded during the Gubbio Survey, using kernel densities estimation.</p>
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<p>The Bronze and Early Iron Age radiocarbon dates of Gubbio in the regional context of Central Italy presented here [<a href="#B9-land-13-01369" class="html-bibr">9</a>], showing the clear transition between the sites of Monte Ingino, Monte Ansciano and San Agostino, allowing for the complexities of the Hallstatt plateau in the calibration curve. Calibration data based on [<a href="#B10-land-13-01369" class="html-bibr">10</a>,<a href="#B11-land-13-01369" class="html-bibr">11</a>]. A–H refer to significant changes in the “demographic” curve.</p>
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<p>(<b>A</b>) Distribution of Iron Age sites in the valley; (<b>B</b>) Heatmap of Iron Age activity based on the spreads of ceramic material recorded during the Gubbio Survey, using kernel densities estimation. The same scale of density of pottery is employed for <a href="#land-13-01369-f011" class="html-fig">Figure 11</a> and <a href="#land-13-01369-f012" class="html-fig">Figure 12</a>.</p>
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<p>(<b>A</b>) Distribution of Hellenistic sites in the valley with inset showing the Gubbio area; (<b>B</b>) Heatmap of Hellenistic activity based on the distribution of ceramic material recorded during the Gubbio Survey, using kernel densities estimation. The same scale of density of pottery is employed for <a href="#land-13-01369-f010" class="html-fig">Figure 10</a> and <a href="#land-13-01369-f012" class="html-fig">Figure 12</a>. Numbers 1–6 refer to clusters of sites cited in the text.</p>
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<p>(<b>A</b>) Distribution of Roman sites in the valley (with inset showing sites in the Gubbio area); (<b>B</b>) Heatmap of Roman activity based on the spreads of ceramic material recorded during the Gubbio Survey, using kernel densities estimation. The same scale of density of pottery is employed for <a href="#land-13-01369-f010" class="html-fig">Figure 10</a> and <a href="#land-13-01369-f011" class="html-fig">Figure 11</a>. Numbers 1–6 refer to clusters of sites cited in the text.</p>
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24 pages, 45845 KiB  
Article
Priene, a Monumental Disaster in the Aegean: Digital Approaches to the Doric Stoa’s and the Theater’s Lost Evidence
by Elisabetta Caterina Giovannini, Giorgio Verdiani and Vieri Cardinali
Heritage 2024, 7(8), 4538-4561; https://doi.org/10.3390/heritage7080214 - 21 Aug 2024
Cited by 1 | Viewed by 826
Abstract
This paper uses digital approaches to investigate Priene’s (Turkey) archaeological area. The city was built ex novo, after a catastrophic earthquake around 350 BC, on a new site facing the Mediterranean Sea. The city suffered a slow decline following centuries of development and [...] Read more.
This paper uses digital approaches to investigate Priene’s (Turkey) archaeological area. The city was built ex novo, after a catastrophic earthquake around 350 BC, on a new site facing the Mediterranean Sea. The city suffered a slow decline following centuries of development and was abandoned after the 12th century. The remains of Priene were discovered in the 17th century, and different excavations and studies have been conducted in the last few centuries. The city’s remains have been studied from various archaeological and historical points of view. It is documented that the city suffered different earthquakes during its existence, as demonstrated by the partial restorations and damage patterns visible within the remains. This contribution offers a methodological and interdisciplinary approach for studying and enhancing archaeological heritage. This paper presents the preliminary results of the first comprehensive digital acquisition of the Aegean city of Priene. The digitization approaches here described focused on digital acquisition and 3D modeling restitution in the form of virtual reconstructions of two monumental buildings: the Doric Stoa near the Temple of Athena Polias and the Theater. The procedure was complementary to the analysis and comprehension of previous numerous studies carried out by British and German institutions, where digital acquisition and restitution techniques have led to the validation of previously obtained results. For the first time, digital models have been used as tools for accessing heterogeneous knowledge, and they have been incorporated into the discourse of archeological studies. Indeed, the interdisciplinary team went beyond archaeological data to attempt to digitally reconstruct monumental complexes and conduct preliminary structural evaluations scientifically. Full article
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<p>On the top, a portion of the plan of Priene in ‘Griechische Stadeanlagen’ [<a href="#B6-heritage-07-00214" class="html-bibr">6</a>,<a href="#B7-heritage-07-00214" class="html-bibr">7</a>], with the locations investigated during this study. 1. Terrace of the Doric Stoa near the Temple of Athena Polias. 2. Theater. On the bottom, superimposition with the Google Earth view. (E.C.G. and G.V.).</p>
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<p>Historical photographic from the iDAI platform [<a href="#B19-heritage-07-00214" class="html-bibr">19</a>], and on the bottom, comparisons of images A and B from the 1980 to 2022 photographic campaigns. (E.C.G.).</p>
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<p>On the left are axonometric views of the aligned point clouds of the Temple area: image with 465 scan station positions (<b>top</b>) and a southwest view (<b>bottom</b>). On the right, images of post-processing: a comparison between the raw data (<b>top</b>) and cleaned point cloud (<b>bottom</b>). (E.C.G.).</p>
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<p>Images of the Theater and UAV acquisition. (E.C.G.).</p>
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<p>Images of the post-processing of data for the Theater. From the left, the alignment of cameras (1,256,561 points), dense cloud (261,238,304 points), and textured mesh (43,646,219 faces and 21,831,522 vertices). (E.C.G.).</p>
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<p>The hypothesis of the first configuration of the Theater (image from the <span class="html-italic">Salt Araştırma</span>, <span class="html-italic">Harika-Kemali Söylemezoğlu Arşivi</span>) [<a href="#B26-heritage-07-00214" class="html-bibr">26</a>,<a href="#B27-heritage-07-00214" class="html-bibr">27</a>].</p>
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<p>The hypothesis of the Hellenistic Age of the Theater according to Gerkan [<a href="#B25-heritage-07-00214" class="html-bibr">25</a>,<a href="#B28-heritage-07-00214" class="html-bibr">28</a>].</p>
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<p>The hypothesis of the Roman Age of the Theater according to Gerkan [<a href="#B5-heritage-07-00214" class="html-bibr">5</a>,<a href="#B25-heritage-07-00214" class="html-bibr">25</a>].</p>
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<p>Horizontal misalignment between the three parts of the retaining walls (<b>A</b>–<b>C</b>). The position of the three parts is detailed in the legend. On the left is the west corner of <span class="html-italic">Beilage</span> 4 [<a href="#B18-heritage-07-00214" class="html-bibr">18</a>]. On the right are the two fronts of the east corner from digital acquisition. (V.C.).</p>
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<p>The Masonry Quality Index (MQI) analysis [<a href="#B29-heritage-07-00214" class="html-bibr">29</a>] applied to wall B from <a href="#heritage-07-00214-f009" class="html-fig">Figure 9</a>. (V.C.).</p>
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<p>Superimposition between the digital acquisition (2022) and the archaeological survey drawing from <span class="html-italic">Beilage</span> 1 [<a href="#B18-heritage-07-00214" class="html-bibr">18</a>] (E.C.G. and G.V.).</p>
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<p>Reality-based capital (magenta) and source-based references (cyan) for the virtual reconstruction of the column of Doric Stoa, according to Hennemeyer [<a href="#B18-heritage-07-00214" class="html-bibr">18</a>]. (E.C.G.).</p>
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<p>Extended Matrix visual graph (v.1.4) for the description of the reality-based capital (magenta) and source-based virtual reconstruction of a column (cyan) of the Doric Stoa according to Hennemeyer [<a href="#B18-heritage-07-00214" class="html-bibr">18</a>] (E.C.G.).</p>
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<p>Three-dimensional virtual reconstruction of the Doric Stoa. Superimposition from a reality-based 3D model obtained from the point-cloud and source-based 3D model, according to Hennemeyer [<a href="#B18-heritage-07-00214" class="html-bibr">18</a>]. (E.C.G.).</p>
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<p>On the <b>left</b>, superimposition between the UAV digital acquisition (2022) and the hypothetical reconstructive drawings by Dörpfeld [<a href="#B60-heritage-07-00214" class="html-bibr">60</a>] used as references for the source-based 3D. (E.C.G. and G.V.) On the <b>right</b>, reconstructive hypothesis from ‘The Ancient Theatre Archive’ [<a href="#B61-heritage-07-00214" class="html-bibr">61</a>].</p>
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<p>Three-dimensional virtual reconstruction of the Priene Theater. Superimposition from a reality-based 3D model obtained from the UAV point cloud and source-based 3D model, according to Dörpfeld [<a href="#B60-heritage-07-00214" class="html-bibr">60</a>]. (E.C.G.).</p>
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<p>Reality-based 3D models developed for the VR experience. (E.C.G. and G.V.).</p>
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<p>VR experience with annotations and links to detailed digital assets of <span class="html-italic">prohedria</span> marble seats. (E.C.G. and G.V.).</p>
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<p>VR experience Meta Quest 3 preview using the Direct Link. (E.C.G and G.V.).</p>
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<p>VR visualization with a mobile device of the walkthrough experience. (E.C.G.).</p>
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17 pages, 14390 KiB  
Article
Scan-to-HBIM-to-VR: An Integrated Approach for the Documentation of an Industrial Archaeology Building
by Maria Alessandra Tini, Anna Forte, Valentina Alena Girelli, Alessandro Lambertini, Domenico Simone Roggio, Gabriele Bitelli and Luca Vittuari
Remote Sens. 2024, 16(15), 2859; https://doi.org/10.3390/rs16152859 - 5 Aug 2024
Cited by 1 | Viewed by 1145
Abstract
In this paper, we propose a comprehensive and optimised workflow for the documentation and the future maintenance and management of a historical building, integrating the state of the art of different techniques, in the challenging context of industrial archaeology. This approach has been [...] Read more.
In this paper, we propose a comprehensive and optimised workflow for the documentation and the future maintenance and management of a historical building, integrating the state of the art of different techniques, in the challenging context of industrial archaeology. This approach has been applied to the hydraulic work of the “Sostegno del Battiferro” in Bologna, Italy, an example of built industrial heritage whose construction began in 1439 and remains in active use nowadays to control the Navile canal water flow rate. The initial step was the definition of a 3D topographic frame, including geodetic measurements, which served as a reference for the complete 3D survey integrating Terrestrial Laser Scanning (TLS), Structured Light Projection scanning, and the photogrammetric processing of Unmanned Aircraft System (UAS) imagery through a Structure from Motion (SfM) approach. The resulting 3D point cloud has supported as-built parametric modelling (Scan-to-BIM) with the consequent extraction of plans and sections. Finally, the Heritage/Historic Building Information Modelling (HBIM) model generated was rendered and tested for a VR-based immersive experience. Building Information Modelling (BIM) and virtual reality (VR) applications were tested as a support for the management of the building, the maintenance of the hydraulic system, and the training of qualified technicians. In addition, considering the historical value of the surveyed building, the methodology was also applied for dissemination purposes. Full article
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<p>The Battiferro lock: view of the main building and upstream canals.</p>
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<p>Workflow of activities for the survey, HBIM and VR implementation for the Battiferro lock.</p>
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<p>Geomatics survey activities: (<b>a</b>) survey area and reference points: the yellow triangles represent the 3D points measured with GNSS-NRTK and total station, the blue circles indicate the elevation landmarks measured with trigonometric levelling; (<b>b</b>) the scan positions of the laser scanner system and distribution of the retro-reflective targets: the white squares indicate the position of the targets, the scan positions are the red triangles with the black border when they were taken below ground level (under the building or in the canals); (<b>c</b>) additional detailed survey of the channel bottom: the circles represent the elevation points measured with total station from the reference points.</p>
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<p>Summary of geomatic tools and techniques used for the survey of the Battiferro Lock.</p>
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<p>Products of the UAS photogrammetric survey: (<b>a</b>) orthomosaic of the surveying area: yellow circles indicate the position of the GCPs; (<b>b</b>) detail of the point cloud of the exterior of the building obtained from the TLS survey coloured in greyscale; (<b>c</b>) detail of the point cloud in real colours of the building obtained from the photogrammetric processing.</p>
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<p>Three-dimensional models of a control wheel: (<b>a</b>) portion of the point cloud derived from TLS, (<b>b</b>) mesh obtained with the Structured Light Projection scanner; (<b>c</b>) BIM object; (<b>d</b>) mesh used in VR.</p>
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<p>Three-dimensional view of the BIM model superimposed to the point cloud model.</p>
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<p>BIM models: (<b>a</b>) 3D view in BIM platform; (<b>b</b>) 3D view of the BIM model imported in a GIS platform.</p>
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<p>Comparison between the tested VR navigation platforms: (<b>a</b>) the technical platform, allowing the user to select elements and visualise the BIM data associated with them; (<b>b</b>) the rendering platform, offering a realistic and impacting virtual representation of the HBIM model.</p>
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<p>Comparison between the tested VR navigation platforms: (<b>a</b>) the technical platform, allowing the user to select elements and visualise the BIM data associated with them; (<b>b</b>) the rendering platform, offering a realistic and impacting virtual representation of the HBIM model.</p>
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40 pages, 31280 KiB  
Article
Integrated Shallow Geophysical Surveys at Two Caddo Period Archaeological Sites within the Limits of a Water Reservoir in Northeastern Texas, USA
by Hector R. Hinojosa-Prieto, Allen M. Rutherford and Jesse D. Brown
Heritage 2024, 7(8), 4045-4084; https://doi.org/10.3390/heritage7080191 - 31 Jul 2024
Viewed by 991
Abstract
The newly constructed Bois d’Arc Lake Reservoir in Fannin County, Texas, USA, inevitably flooded a large ground surface area (67.34 km2) when the reservoir began impounding water in April 2021. Inside this (now) flooded area, land-based archaeological data recovery investigations discovered [...] Read more.
The newly constructed Bois d’Arc Lake Reservoir in Fannin County, Texas, USA, inevitably flooded a large ground surface area (67.34 km2) when the reservoir began impounding water in April 2021. Inside this (now) flooded area, land-based archaeological data recovery investigations discovered and documented several archaeological sites, now registered in the state of Texas; though, only two neighboring sites, namely, 41FN178 and 41FN244, are examined here. The first phase of archaeological testing at these sites included shovel testing, test unit excavations, and geoarchaeological trenching that yielded archaeological artifacts suggesting that Middle Caddo Indian peoples (AD 1200–1400) might have occupied this landscape. As the sites were recognized before the reservoir’s impoundment phase, this merited a non-invasive, non-destructive, high-resolution near-surface geophysical study to map strategic areas within sites 41FN178 and 41FN244 that might yield potential shallow targets of archaeological context. The adopted geophysical survey comprised 3D direct current electrical resistivity imaging (ERI) and land horizontal magnetic gradiometry (HMG), each mapping a total surface area of 2133 and 15,640 m2, respectively. The combination of 3D ERI and land HMG surveys was instrumental in rapidly mapping the horizontal and vertical extent of shallowly buried anomalies within a large area prior to the completion of the dam and the beginning of water impoundment. Based on the geophysical insights, the outline of several Caddo houses with functional internal and external features (e.g., burnt cooking surfaces, storage pits, refuse pits, fired soil, ditches, a dump site, and a compound fence) are thought to exist within the uppermost 2 m of the Quaternary stratigraphy at both sites. At site 41FN244, 3D ERI found numerous resistive anomalies surrounding a conductive anomaly, collectively interpreted as a group of post-holes surrounding the remains of a Caddo house’s inner clay floor. It also found a cluster of several resistive anomalies interpreted as midden or middens. The HMG survey carried across areas from which archaeological test units also yielded positive findings, at sites 41FN178 and 41FN244, identified numerous scattered monopolar and dipolar anomalies interpreted as post-molds of Caddo houses, compound enclosures or fences, and adjacent middens. Archaeological excavations guided by the geophysical results yielded significant cultural material and post-mold features at site 244, which validate the geophysical interpretation in a preliminary context. Additionally, several dispersed magnetic anomalies are thought to be shallowly buried hearths, burn cooking surfaces, storage pits, and ditches. The mapped magnetic anomalies agree with the location and distribution of previously found archaeological artifacts and the extent of resistive and conductive resistivity anomalies. Follow-up archaeological excavations of these geophysical anomalies have preliminarily confirmed interpretations. Full article
(This article belongs to the Special Issue Unveiling the Past: Multidisciplinary Investigations in Archaeology)
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<p>The Upper Nasoni settlement on the Red River, based on Domingo Terán de los Rios 1691–1692 expedition. The map is the earliest known cartographic depiction of a Native American community in Texas. Original map in the Archivo General de Indias, Seville. (source: <a href="https://www.texasbeyondhistory.net/nasoni/" target="_blank">https://www.texasbeyondhistory.net/nasoni/</a> (accessed on 6 May 2024).</p>
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<p>(<b>A</b>) Area overview of the archaeological sites 41FN178 and 41FN244 over the topographic map (<b>A</b>). The geographic location of archaeological sites 41FN178 and 41FN244 was selected for shallow geophysical prospecting (<b>B</b>). The sites were near water resources. The digital elevation model is from the US Geological Survey (<a href="https://earthexplorer.usgs.gov/" target="_blank">https://earthexplorer.usgs.gov/</a> (accessed on 5 May 2024).</p>
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<p>Graphic illustration showing the topographic relief and stratigraphy from the south of Bois d’Arc Creek (<b>left</b>) to the north side of the Red River floodplain (<b>right</b>) (modified from Skinner et al. [<a href="#B6-heritage-07-00191" class="html-bibr">6</a>]).</p>
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<p>Geological map of the area around archaeological sites 41FN178 and 41FN244 (modified from <a href="https://webapps.usgs.gov/txgeology/" target="_blank">https://webapps.usgs.gov/txgeology/</a> (accessed on 7 May 2024).</p>
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<p>(<b>A</b>) The extent of the Caddo Nation’s Homeland (yellow polygon) in the United States. (<b>B</b>) Inside the Caddo area are plotted several well-documented archaeological sites with mound structures (orange triangles) and without (yellow circles). Archaeological sites 41FN178 and 41FN244 (this study) plot in the west-central edge of the Caddo area (redrawn from the Texas Beyond History Special Exhibits Tejas Caddo, <a href="https://www.texasbeyondhistory.net/tejas/map/index.html" target="_blank">https://www.texasbeyondhistory.net/tejas/map/index.html</a> (accessed on 11 May 2024).</p>
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<p>The architecture of a typical Caddo house is displayed in several forms: in live example ((<b>A</b>), <a href="https://www.sfasu.edu/heritagecenter/9614.asp" target="_blank">https://www.sfasu.edu/heritagecenter/9614.asp</a> (accessed 28 April 2024), in profile view (<b>B</b>), in plan view (<b>C</b>), and an archaeologically excavated form (<b>D</b>), redrawn from Jelks and Tunnell [<a href="#B29-heritage-07-00191" class="html-bibr">29</a>]). The backbone of the Caddo house was constituted by a ring of wooden poles or timber, each with its base end set in a deep hole, placed in an upright position. The tops of the poles merged at the center and bound. Trim tree branches and grass were then woven between the upright poles. In some cases, the exterior face was plastered with a coat of clay mud. Interior support posts may be added, and platforms for sleeping or storage were built inside the house. An inner clay mantel and functional features inside a semi-circular/circular or square arrangement of timber post-molds are often the diagnostic evidence revealed in archaeological excavations suggestive of a Caddo house.</p>
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<p>Geophysical survey layout map showing the distribution of the ERI and HMG survey tracks within archaeological sites 41FN178 and 41FN244.</p>
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<p>Deployed true-3D and pseudo-3D ERI electrode grids at zones 178-area3, 244-area1, and 244-area2. RA = roll-along. SA = slide-along. Each grid was oriented differently with respect to the geographic north. See <a href="#heritage-07-00191-t001" class="html-table">Table 1</a> for electrode spacings, horizontal resolutions, and electrode array types.</p>
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<p>The field setup of the 3D resistivity measurements with the SuperSting R8/IP (<b>A</b>) and for horizontal magnetic gradiometer measurements with the G-858GAP cesium-vapor gradiometer (<b>B</b>); the green and orange marks on the wooden stakes show the start and end of a survey line, respectively. The insert in (<b>B</b>) shows the lateral extent of the horizontal gradiometry measurement and how the interpolation of data is omitted; the sampling swath is perpendicular to the survey direction.</p>
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<p>Contact resistance plots of all 3D ERI sites. In general, all sites are conductive due to their low contact resistance (~1000 Ω, red dotted line). However, site 178-area3 and site 244-area1 are the least and most resistive, respectively. This suggests that inter-site natural conditions are significant despite their close geographic proximity.</p>
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<p>(<b>A</b>) Interpreted 3D electrical resistivity model of zone 178-area3, within archaeological site 41FN244, viewed from multiple angles. (<b>B</b>) The same resistivity model is sliced horizontally in increments of 0.50 m. The high resistivity anomalies (resistive structures) and the sizeable low resistivity (conductive structure) are interpreted as a silty-clay lens and clay-rich matrix within the Quaternary alluvial terrace.</p>
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<p>Three-dimensional electrical resistivity model of site 244-area1 (<b>A</b>) within archaeological site 41FN244 and horizontal depth slices of electrical resistivity at 0.25 m intervals (<b>B</b>). The high-resistivity anomalies (resistive structures) and the large, low-resistivity anomalies (conductive structures) are interpreted as the post-holes and remains of a Caddo house’s inner clay floor. The open circle (dashed line) delineates the perimeter of the Caddo house structure marked by the post-holes.</p>
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<p>(<b>A</b>) Three-dimensional electrical resistivity model of zone 244-area2 within archaeological site 41FN244. (<b>B</b>) The horizontal depth slices every 0.50 m of the same model. The high-resistivity anomalies (resistive structures) surrounded by low-resistivity (conductive) materials are likely a large midden or several smaller middens.</p>
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<p>The land horizontal magnetic gradient map from zones 178-area1, 178-area2, and 178-area3 within archaeological site 41FN178. Numerous monopoles and dipoles are mapped. The coordinates are NAD83 UTM zone 15 N.</p>
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<p>The archaeological interpretation of the mapped horizontal magnetic gradient anomalies based on the anomaly class from search blocks 178-area1, 178-area2, and 178-area3. The interpreted outline of two Caddo houses with functional features (burnt cooking surfaces, storage pits, refuse pits, fired soil, and a large midden) is drawn to scale. The coordinates are NAD83 UTM zone 15 N.</p>
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<p>The land horizontal magnetic gradient map from zones 244-area1 to 244-area7 within archaeological site 41FN244. Numerous monopoles and dipoles are mapped. The coordinates are NAD83 UTM zone 15 N.</p>
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<p>The archaeological interpretation of the mapped horizontal magnetic gradient anomalies based on the anomaly class from search blocks 244-area1 to 244-area7. The outline of several Caddo houses with functional internal and external features (burnt cooking surfaces, storage pits, refuse pits, fired soil, ditches, dump site, and compound fence) is drawn to scale. The coordinates are NAD83 UTM zone 15 N.</p>
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<p>Field photographs of archaeological excavation at block 580 E 823 N. (<b>A</b>) shows feature 46 at 673 cm below the datum. Units 584–585 E 828–829 N. Loamy sand feature with burned clay inclusions and an excavated post-mold. (<b>B</b>) shows a central hearth area at 683 cm below the datum and a silty sand feature with ash and burned clay inclusions. Units: 584–585 E 826–828 N; the view is facing north. (<b>C</b>) shows a cultural surface at 693 cm below the datum. Southeast to northwest post-mold outline with bioturbated root stains and animal burrows; the view is facing north. (<b>D</b>) shows feature 46 and cultural surface at 688 cm below datum with large, dark brown sandy loam feature with excavated pit feature; the view is facing north. (<b>E</b>) shows cultural surface at 703 cm below datum. Excavated post-molds, pit features, and rodent burrows; the view is facing south.</p>
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20 pages, 4572 KiB  
Article
Identification of Social Status through Grave Goods Using a Biocultural Approach in Interpreting the Alpine Context of Borca Di Cadore, Belluno, Veneto, Italy (18th–19th Centuries)
by Lisa De Luca, Alessandro Asta, Pacitti Davide and Ilaria Gorini
Heritage 2024, 7(8), 3997-4016; https://doi.org/10.3390/heritage7080188 - 30 Jul 2024
Viewed by 671
Abstract
The cemetery of the Church of Santi Simone e Giuda in Borca di Cadore (Belluno province, Veneto region, Italy) was excavated between 2021 and 2023 as part of an archaeological intervention. The excavation area yielded a total of 21 graves dating back to [...] Read more.
The cemetery of the Church of Santi Simone e Giuda in Borca di Cadore (Belluno province, Veneto region, Italy) was excavated between 2021 and 2023 as part of an archaeological intervention. The excavation area yielded a total of 21 graves dating back to the 18th–19th century; this was intriguing due to the presence of grave goods and taphonomic indicators that allowed these burials to be interpreted as clothed burials. This contribution examines 14 of the 21 graves, representing the available sample considering preservation conditions. Fieldwork was carried out through close synergy between archaeological and anthropological methodologies, involving careful excavation to verify funerary rituals through taphonomic data analysis. Anthropological methods were applied to determine the biological profile of the individuals, while aspects related to their health status were investigated through paleopathological analyses. Data obtained from field and laboratory observations were cross-referenced with historical and anthropological-cultural data from bibliographic and archival research. Reconstructing the social status of the deceased within the burial context is crucial for understanding the social and cultural dynamics of past populations, achievable only through a biocultural approach integrating information from archaeology, cultural anthropology, and bioarchaeology. Modern burial contexts offer privileged realities due to abundant historical and anthropological-cultural documentation, allowing for a more precise contextualization of bioarchaeological findings with significant support from documentary sources. Studies applied to these periods closer to the present enable the continuous refinement of an investigative method attentive to the synergy of different aspects of biocultural research, enhancing the importance of this approach in reconstructing the life histories of populations. Full article
(This article belongs to the Section Biological and Natural Heritage)
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<p>The figure combines orthophotos of the portion of the cemetery area pertaining to the church of S.S. Simon and Jude, investigated through archaeological excavation. The orthophoto was obtained through three-dimensional photogrammetric processing. The excavation trench plan highlights its position relative to the church, still in use by the community. The map of Italy shows the location of the Veneto region within Italy and the position of the municipality of Borca di Cadore within the Veneto region.</p>
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<p>The most significant bone alterations found: caries (<b>A</b>–<b>C</b>), antemortem tooth loss (<b>D</b>), insertion of the costoclavicular ligament (<b>E</b>), insertion of the biceps brachii tendon on the radial tuberosity (<b>F</b>), insertion of the triceps brachii on the olecranon of the ulna (<b>G</b>), palmar and dorsal interossei muscles (<b>H</b>), eburnation of the femoral head and flattening of the corresponding acetabular cavity in individual from grave 8 (<b>I</b>,<b>N</b>), Poirier’s facets from grave 15 (<b>L</b>,<b>M</b>), plantar and dorsal interossei muscles (<b>O</b>), fusion of the second and third metatarsals of traumatic origin (<b>P</b>).</p>
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<p>The figure shows the skeletal elements with metal imprints from grave 8 and their relative positioning.</p>
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<p>The figure shows the skeletal elements with metal imprints from grave 15 and their relatives positioning.</p>
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16 pages, 3466 KiB  
Article
The First Apocalypse of James in a Socio-Linguistic Perspective: Three Greek and Coptic Versions from Ancient Monastic Egypt
by David W. Kim
Religions 2024, 15(8), 881; https://doi.org/10.3390/rel15080881 - 23 Jul 2024
Viewed by 1086
Abstract
The discovery of the Nag Hammadi Codices (NHC) in 1945 rates as one of the two most profound occurrences for Biblical archaeology and interpretation during the last hundred years, along with the Dead Sea Scrolls (1946–1956). The codices allow us to document Christian [...] Read more.
The discovery of the Nag Hammadi Codices (NHC) in 1945 rates as one of the two most profound occurrences for Biblical archaeology and interpretation during the last hundred years, along with the Dead Sea Scrolls (1946–1956). The codices allow us to document Christian monastic culture, gnostic Christianity and gnostic offshoots in the desert climate of Late Ancient Egypt. The recovery of the related Codex Tchacos (CT) brought further excitement for contemporary readers by 2006, it being sensational that narratives of “Judas the betrayer” and “doubting Thomas” were found in the whole collection of writings. The text named the [First] Apocalypse of James, significantly, was found to be in both NHC and CT in different Coptic versions (from near the sacred sites of Chenoboskion and El Minya), but yet another more fragmentary version in Greek had turned up much earlier among the huge cache of papyri found at Oxyrhynchus (also, like the other places, on the banks of the Nile). Given the opportunity for comparison, what distinguishes the three versions? Does comparative analysis better tell us what this ancient text is about? Does the strong presence of Gnostic Christian insights in the Coptic texts still imply a historical Jamesian community is being honoured? This paper concentrates on three comparable passages in the three versions that apparently contain historical memories of James and his followers. It works on the reasonable hypothesis that the Greek version of Oxyrhynchus Papyri (P.Oxy. 5533) (hereafter = PO) is prior and read with different purposes than the two Coptic translated versions of CT (CT 2.10–30) and NHC (NHC V,3. 24–44). When a critical approach, involving a socio-linguistic comparison, is applied, we will see that the three versions of the text were not directly related to each other, but that narratives about James the Just were available to desert monastics from the second century CE. The paper argues for a literal transmission of traditions from a Jewish Christian community around James into Egypt, that the textual figure of James in the Oxyrhynchus fragments points to a ‘mutual familiarity’ between PO and CT, while the NHC tradition of James has been further elaborated by processes of compilation and addition. Full article
(This article belongs to the Special Issue Patristics: Essays from Australia)
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Figure 1

Figure 1
<p>P.Oxy. 5533, Leaf A (a Greek fragment of the First Apocalypse of James).</p>
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