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12 pages, 1287 KiB  
Article
Effectiveness Evaluation of Silicone Oil Emulsion In Situ Polymerization for Dehydration of Waterlogged Wooden Artifacts
by Mengruo Wu, Xiangna Han, Zhiguo Zhang and Jiajun Wang
Molecules 2024, 29(20), 4971; https://doi.org/10.3390/molecules29204971 - 21 Oct 2024
Viewed by 613
Abstract
Organosilicon materials have shown potential as dehydration agents for waterlogged wooden artifacts. These materials can polymerize under normal conditions to form polymers with favorable mechanical strength, antibacterial properties, and aging resistance. However, the insolubility of most organosilicon hindered their penetration into waterlogged wood, [...] Read more.
Organosilicon materials have shown potential as dehydration agents for waterlogged wooden artifacts. These materials can polymerize under normal conditions to form polymers with favorable mechanical strength, antibacterial properties, and aging resistance. However, the insolubility of most organosilicon hindered their penetration into waterlogged wood, which may lead to an unwanted cracking. This study aimed to evaluate the effectiveness of polydimethylsiloxane (PDMS) and hydroxy-terminated polydimethylsiloxane (PDMS-OH) with low viscosity and moderate reactivity for dehydrating waterlogged wooden artifacts from the Nanhai No.1 shipwreck. Four surfactants ((3–aminopropyl) triethoxysilane (APTES), alkyl polyoxyethylene ether (APEO), tri-methylstearylammonium chloride (STAC), and fatty alcohol polyoxyethylene ether (AEO)) and cosurfactant were employed to transform the two kinds of water-repellent silicone oils into eight groups of highly permeable oil-in-water (O/W) emulsions. Under the catalysis of a neutral catalyst, in situ polymerization occurred within the wood cells. Group P2-2 formulated with PDMS-OH and APEO showed the best efficiency in maintaining the dimensions of the wood during dehydration. The dehydrated wood exhibited a natural color and texture with a minimal volume shrinkage rate of 1.89%. The resulting polymer adhered uniformly to the cell walls, effectively reinforcing the wood cell structure. The weight percent gain of the wood was only 218%, and the pores of the cell lumen were well maintained for future retreatment. This method effectively controlled the sol–gel reaction process of the organosilicon and prevented damage to the wooden artifact during the dehydration process. Moreover, the dehydrated wood samples only experienced a low weight gain of 17% at 95% relative humidity (RH), indicating their great environmental stability. Full article
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<p>(<b>a</b>) Schematic diagram of the silicone oil emulsion preparation process. (<b>b</b>) The 8 groups of silicone oil emulsions.</p>
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<p>Schematic diagram of the dehydration process of waterlogged archaeological wood.</p>
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<p>The dehydrated pine wood samples before (<b>left</b>) and after (<b>right</b>) treatment with silicone oil emulsions. (<b>a</b>) P1-1; (<b>b</b>) P1-2; (<b>c</b>) P1-3; (<b>d</b>) P1-4; (<b>e</b>) P2-1; (<b>f</b>) P2-2; (<b>g</b>) P2-3; (<b>h</b>) P2-4; (<b>i</b>) Untreated wood.</p>
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<p>Simulated color according to the CIELab color model of the wood samples.</p>
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<p>The vapor adsorption–desorption curves at 0% to 95% RH of the wood samples treated with (<b>a</b>) P1 and (<b>b</b>) P2.</p>
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<p>Typical distribution of organic silicon polymerization products in archaeological wood cells (<b>a</b>,<b>b</b>). Pattern 1: organosilicon polymers formed in the cell lumens in P1-2 and P2-2; (<b>c</b>,<b>d</b>) pattern 2: organosilicon polymers only adhere to the cell walls of earlywood and latewood cells in P2-2 samples; (<b>e</b>) pattern 3: wood cells in P2-1 samples filled with organosilicon polymers; (<b>f</b>) the control group samples without silicone oil treatment showed severe deformation of wood cells after being dried in normal conditions.</p>
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<p>FT-IR spectrum of wood before and after silicone oil emulsions’ dehydration treatment.</p>
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2 pages, 581 KiB  
Editorial
Waterlogged Archaeological Woods
by Yoon Soo Kim and Adya P. Singh
Forests 2024, 15(8), 1333; https://doi.org/10.3390/f15081333 - 1 Aug 2024
Viewed by 532
Abstract
Ancient wooden structures that are being continually uncovered from waterlogged environments are considered to be precious artefacts that reveal past human history and culture, as well as climatic changes that have occurred over the span of centuries [...] Full article
(This article belongs to the Special Issue Waterlogged Archaeological Woods)
23 pages, 15963 KiB  
Article
Study of the Geological Context of the 7th–6th Century BC Phoenician Era Shipwreck “Mazarrón 2” (Murcia, Spain)
by María-Teresa Doménech-Carbó, Nuria Guasch-Ferré, Carla Álvarez-Romero, Rocío Castillo-Belinchón, Soledad Pérez-Mateo and Milagros Buendía-Ortuño
Minerals 2024, 14(8), 778; https://doi.org/10.3390/min14080778 - 30 Jul 2024
Viewed by 905
Abstract
The Mazarrón 2 shipwreck was found in 1994 on the beach of Playa de la Isla (Mazarrón, Murcia, Spain). This finding is extremely important because the boat and its lead cargo were still in a reasonable conservation state and, therefore, provided new data [...] Read more.
The Mazarrón 2 shipwreck was found in 1994 on the beach of Playa de la Isla (Mazarrón, Murcia, Spain). This finding is extremely important because the boat and its lead cargo were still in a reasonable conservation state and, therefore, provided new data on naval construction, commercial goods, navigation routes, and the relationships between the Phoenicians and the local population in the 7th–6th century BC. Currently, the shipwreck remains underwater, protected by a metallic coffer. In the last 2 years, a Preliminary Studies Project has been carried out, supported by national and regional public institutions. This research aims to know the shipwreck’s conservation state and to determine the extraction and conservation methods at the Museo Nacional de Arqueología Subacuática ARQVA (Cartagena, Spain), where the conservation and restoration treatment will be conducted. The sampling strategy and analytical study included not only wood and other materials from the shipwreck and its cargo but also the seawater and the seabed materials in the vicinity of the shipwreck. This paper presents the results of the geochemical study of the archeological site. The applied methodology included physico-chemical tests, X-ray diffraction, optical microscopy, FTIR spectroscopy, field-emission scanning electron microscopy coupled with X-ray microanalysis, and X-ray microscopy. The results indicated that, despite the wreck being buried at a shallow depth (less than 50 cm) in a marine environment with a water column of 2–2.5 m, influenced by complex coastal dynamics that favor an oxic environment, early diagenetic processes like the formation of pyrite framboids are particularly intense in the pores and internal channels of the wreck’s wood, where a different dysoxic–anoxic environment prevails. These processes have been the main mechanisms to have affected the wreck and are related to the biogeochemistry of sediments. The sediments have been confirmed to be closely related to the geological context of the Mazarrón region. The conducted study found no significant evidence of pollution due to the lead cargo. Full article
(This article belongs to the Special Issue Geomaterials and Cultural Heritage)
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<p>Location of the Mazarrón 2 shipwreck in the Murcia Region (Spain) and its archeological and mining contexts. (<b>a</b>) The Murcia Region in Spain; (<b>b</b>) the Mazarrón district in the Murcia Region; (<b>c</b>) a photograph of the Mazarrón 2 site. Red dots show Punta de los Gavilanes and the Mazarron 2 shipwreck archeological sites from the Phoenician period. The green dot denotes the El Gachero embankment on the El Rincón de Playa de la Isla. Photographs are from the open access database of the Instituto Geográfico Nacional de España (Spanish National Geographic Institute): general maps (<b>a</b>,<b>b</b>) and orthophoto PNOA 2022 (<b>c</b>); figure assembled by Rocío Castillo-Belinchón.</p>
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<p>(<b>a</b>) Metallic coffer used for the wreck’s in situ protection since 1999; (<b>b</b>) image of Mazarrón 2 during works in June 2023 (photographs by Pedro Ortiz (<b>a</b>) and Milagros Buendía-Ortuño (<b>b</b>) archive of the Museo Nacional de Arqueología Subacuática).</p>
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<p>Evolution of the coastal dynamics and profile of Playa de la Isla, with the Mazarrón 2 shipwreck marked by a red dot, and reflected in this aerial photographs series: 1957, American flight (USAF); 1981 regional flight (CARM); 1999, 2007, 2016, and 2022 national orthophotos (PNOA—IGN) (assembled by Rocío Castillo-Belinchón with free access images available at the CARM and the Instituto Geográfico Nacional.</p>
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<p>Distribution of sediment sampling points (MZB2-01 to MZB2-16, MZPI-01 and MZCG-01), measurement points (MP-01 to MP-12), and manual trench MT-01 around the Mazarrón 2 shipwreck in June 2023 (Drawing made by Rocío Castillo-Belinchón y Nuria Guasch-Ferré).</p>
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<p>Manual trench (MT-01) inside the metallic protection structure, northwest of the shipwreck, during works in June 2023 (<b>Left</b>); detail of the prior image (<b>Right</b>) (Photographs by Rocío Castillo-Belinchón, Archive of the Museo Nacional de Arqueología Subacuática).</p>
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<p>(<b>a</b>) Photograph of sediments MZB2-01 (<b>left</b>), MZB2-02 (<b>middle</b>), and MZPI-01 (<b>right</b>); cm scale. (<b>b</b>) Classification of sediment samples according to their color.</p>
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<p>Photographs of the dried sediments obtained by using a stereoscopic microscope operating with episcopic illumination: (<b>a</b>) MZB2-09 and (<b>b</b>) MZPI-01. Backscattered electron images of the sediments, acquired with FESEM at 20 kV: (<b>c</b>) MZB2-01 and (<b>d</b>) MZPI-01. Arrows point out the microcrystalline deposits of formed NaCl on the grains’ surface during laboratory drying of the sediment samples.</p>
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<p>Diffractograms acquired from samples: (<b>a</b>) MZB2-11; (<b>b</b>) MZB2-02; (<b>c</b>) MZB2-01; (<b>d</b>) MZPI-01. B: biotite; C: calcite; D: dolomite; G: goethite; H: hematite; K: kaolinitic clayey minerals; M: magnetite; Mh: maghemite; Kr: kirchseinite; Q: quartz; Fk: K-feldspar; Fn: Na-feldspar; Fp: plagioclase feldspar; Px: pyroxene; Tm: titanomagnetite; W: wollastonite.</p>
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<p>IR absorption spectra acquired from samples: (<b>a</b>) MZCG-01; (<b>b</b>) detail of MZB2-01 and MZCG-01 within the IR spectra as 500–1000 cm<sup>−1</sup>; (<b>c</b>) MZB2-01 and (<b>d</b>) MZPI-01. B: biotite; C: calcite; C<sub>y</sub>: clays; D: dolomite; Fk: potassium feldspar; Fp: plagioclase feldspar; Fy: fayalite; G: goethite; Gh: gehlenite; H: hematite; Kr: kirchsteinite; M: magnetite; Mh: mahemite; Px: pyroxene; Q: quartz; W: wollastonite.</p>
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<p>In-depth projections of sample MAZ-01. Coordinates -x and -y in the cross-section plane of the wood, and orthogonal coordinate -z along images (<b>a</b>–<b>c</b>).</p>
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<p>Backscattered electron images (FESEM, 20 kV): (<b>a</b>) aggregates and clusters of framboidal pyrites in sample MAZ-01; (<b>b</b>) spherulitic aggregates of framboidal pyrite growing in the internal channel of a tracheid in MAZ-02.</p>
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<p>Correlations among sampling points MZB2-01 to MZB2-16, color, particle size distribution types GI<sub>a</sub>, GI<sub>b</sub>, GI<sub>c</sub>, GII and GIII, and silica, iron and calcium oxide content of sediments.</p>
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<p>Backscattered electron image (20 kV) (<b>a</b>,<b>c</b>,<b>d</b>) and the secondary electron image (2 kV) (<b>b</b>) of the framboidal pyrites identified in (<b>a</b>) sample MZB2-05); (<b>b</b>) sample MZB2-08; (<b>c</b>) sample MZB2-01 below the anchor; (<b>d</b>) sample MZPI-01 from El Gachero.</p>
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13 pages, 5018 KiB  
Article
Consolidation and Dehydration Effects of Mildly Degraded Wood from Luoyang Canal No. 1 Ancient Ship
by Weiwei Yang, Wanrong Ma, Xinyou Liu and Wei Wang
Forests 2024, 15(7), 1089; https://doi.org/10.3390/f15071089 - 23 Jun 2024
Cited by 1 | Viewed by 764
Abstract
To ensure the conservation of waterlogged archaeological wood, sustainable, safe, and effective methods must be implemented, with consolidation and dehydration being crucial for long-term preservation to maintain dimensional stability and structural integrity. This study compares the permeability of 45% methyltrimethoxysilane (MTMS) and 45% [...] Read more.
To ensure the conservation of waterlogged archaeological wood, sustainable, safe, and effective methods must be implemented, with consolidation and dehydration being crucial for long-term preservation to maintain dimensional stability and structural integrity. This study compares the permeability of 45% methyltrimethoxysilane (MTMS) and 45% trehalose solutions to evaluate the dimensional changes, hygroscopicity, and mechanical properties of treated wood. Since the collected samples (from an ancient ship, Luoyang Canal No. 1) were mildly degraded, the drying method had a slight impact on the properties of archaeological wood. Consolidated with trehalose and MTMS agents, the longitudinal compressive strength of the waterlogged wood’s cell walls increased by 66.8% and 23.5%, respectively. Trehalose proved to be more advantageous in filling pores and reducing overall shrinkage, while MTMS significantly reduced the hygroscopicity and surface hydrophilicity of the wood substance. Overall, the MTMS treatment has a smaller effect on the appearance of samples, making it more suitable for the consolidation of mildly degraded waterlogged archaeological wood. Full article
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<p>Samples from the ancient ship “Luoyang Canal No. 1” (<b>a</b>) the excavated ship planks and (<b>b</b>) samples submerged in consolidants. Note: The Chinese word “海藻糖” in the (<b>b</b>) means trehalose.</p>
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<p>Compressive strength (MPa) of recent sound elm, untreated archaeological wood (control), and samples treated with trehalose and MTMS.</p>
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<p>Cross-section and radial-section photographs of wood samples after MTMS and trehalose reinforcement.</p>
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<p>Scanning electron microscope (SEM) images of archaeological wood samples in the cross section and tangential section.</p>
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<p>FT-IR spectra (<b>a</b>) and their derivatives (<b>b</b>) of untreated, trehalose-treated, and MTMS-treated WAW.</p>
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11 pages, 14843 KiB  
Article
Evaluation of Deterioration Degree of Archaeological Wood from Luoyang Canal No. 1 Ancient Ship
by Weiwei Yang, Wanrong Ma and Xinyou Liu
Forests 2024, 15(6), 963; https://doi.org/10.3390/f15060963 - 31 May 2024
Cited by 3 | Viewed by 724
Abstract
This study provides a detailed investigation of archaeological wood samples from the Luoyang Canal No. 1 site, focusing on wood species identification, physical properties, mechanical property analyses, and morphological examination. The identified wood species, belonging to the Ulmus genus, exhibited a 43% decline [...] Read more.
This study provides a detailed investigation of archaeological wood samples from the Luoyang Canal No. 1 site, focusing on wood species identification, physical properties, mechanical property analyses, and morphological examination. The identified wood species, belonging to the Ulmus genus, exhibited a 43% decline in compressive strength in waterlogged environments. Further, the wood exhibited increased moisture content, higher porosity, reduced basic density, and elevated shrinkage rates, indicating a mild level of degradation. X-ray diffraction was employed for the observation of cellulose structure, and Fourier transform infrared spectroscopy (FT-IR) demonstrated significant removal of cellulose and hemicellulose components. These findings emphasize the importance of understanding wood degradation mechanisms to evaluate structural integrity and durability in guiding the development of effective preservation strategies for archaeological wood artifacts. Continued research and conservation are crucial to deepen our knowledge of wood deterioration processes and enhance the implementation of preservation techniques. Full article
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<p>Microscopic images of archaeological wood in cross section (<b>a</b>), radial section (<b>b</b>) and tangential section (<b>c</b>).</p>
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<p>Comparison between the compressive strength (MPa) of recent healthy wood and archaeological wood samples.</p>
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<p>Scanning electron microscope (SEM) images of archaeological wood samples in different sections.</p>
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<p>X-RD spectra of archaeological wood and recent healthy wood.</p>
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<p>FT-IR spectra of archaeological wood and recent healthy wood.</p>
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41 pages, 80924 KiB  
Review
The Pivotal Role of Microscopy in Unravelling the Nature of Microbial Deterioration of Waterlogged Wood: A Review
by Adya P. Singh, Jong Sik Kim, Ralf Möller, Ramesh R. Chavan and Yoon Soo Kim
Forests 2024, 15(5), 889; https://doi.org/10.3390/f15050889 - 20 May 2024
Cited by 2 | Viewed by 1076
Abstract
This review focuses on the pivotal role microscopy has played in diagnosing the type(s) of microbial attacks present in waterlogged ancient wooden objects, and to understand the nature and extent of deterioration of such objects. The microscopic journey began with the application of [...] Read more.
This review focuses on the pivotal role microscopy has played in diagnosing the type(s) of microbial attacks present in waterlogged ancient wooden objects, and to understand the nature and extent of deterioration of such objects. The microscopic journey began with the application of light microscopy (LM) to examine the deterioration of waterlogged woods, notably foundation piles supporting historic buildings, progressing into the use of high-resolution imaging tools (SEM and TEM) and techniques. Although bacteria were implicated in the deterioration of foundation piles, confirmation that bacteria can indeed degrade wood in its native state came when decaying wood from natural environments was examined using electron microscopy, particularly TEM, which enabled bacterial association with cell wall regions undergoing degradation to be clearly resolved. The information base has been a catalyst, stimulating numerous studies in the past three decades or so to understand the nature of microbial degradation of waterlogged archaeological wood more precisely, combining LM, SEM, and TEM with high-resolution chemical analytical methods, including chemical microscopy. The emerging information is aiding targeted developments towards a more effective conservation of ancient wooden objects as they begin to be uncovered from burial and waterlogging environments. Full article
(This article belongs to the Special Issue Wood as Cultural Heritage Material: 2nd Edition)
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<p>TEM of a transverse section through a cell corner region between tracheids of silver fir. The secondary cell wall is a three-layered structure. CC, cell corner; ML, middle lamella; S1, S2, S3, secondary wall layers; warts (arrowheads). Scale bar = 1 µm. The image is reproduced from Singh et al. [<a href="#B6-forests-15-00889" class="html-bibr">6</a>].</p>
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<p>Schematic representation of cell wall model showing the layered cell wall and different orientation of cellulose microfibrils in the cell wall layers.</p>
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<p>LM of a transverse section through a hardwood tissue attacked by soft rot I. Cavities are abundantly present in fibre cell (F) walls (arrowheads) but are few in the vessel (V) wall (arrow). Individual (non-coalesced) cavities appear to be circular-shaped. P, parenchyma. Scale bar = 20 µm. The image is reproduced from Singh et al. [<a href="#B75-forests-15-00889" class="html-bibr">75</a>].</p>
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<p>TEM of a transverse section through a multilamellar fibre cell wall, composed of thick lamellae (S2-1, S2-2, S2-3) alternating with very thin lamellae (arrow). The face of cavities in contact with the thin lamellae (C) has a flattened appearance. The arrowheads indicate a highly lignified part of the S2-1 underlying the S1 wall. CML, compound middle lamella. Scale bar = 2 µm. The image is reproduced from Singh et al. [<a href="#B75-forests-15-00889" class="html-bibr">75</a>].</p>
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<p>A diagram illustrating the types of microbial attacks reported for ancient waterlogged woods. Microscopic techniques used for identification and understanding of the decay patterns are indicated. EB, erosion bacteria; SR, soft rot; TB, tunnelling bacteria; ML, middle lamella; S1, S2, S3, secondary cell wall layers.</p>
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<p>TEM micrograph showing the repeated branching of tunnels (asterisk) radiating from a central point in a wood cell wall. TB, tunnelling bacteria. Scale bar = 2 µm. The image is reproduced from Singh et al. [<a href="#B22-forests-15-00889" class="html-bibr">22</a>].</p>
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<p>TEM micrograph showing the presence of mixed microbial attack on wood cell walls, involving soft rot Type I (diffuse degradation pattern) and bacterial tunnelling in the same tracheid cell wall. SRC, soft rot cavity; T, tunnels; TB, tunnelling bacteria. Scale bar = 2 µm. The image is reproduced from Singh et al. [<a href="#B44-forests-15-00889" class="html-bibr">44</a>].</p>
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<p>TEM micrograph showing the presence of a tunnel (T) with characteristic crescent-shaped periodic slime bands (arrowhead) in a tracheid cell wall. The asterisk marks a tunnelling bacterium within the tunnel. Scale bar = 2 µm. The image is reproduced from Singh et al. [<a href="#B44-forests-15-00889" class="html-bibr">44</a>].</p>
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<p>TEM micrograph showing the extensive degradation of <span class="html-italic">Homalium foetidum</span> (a high-lignin hardwood) fibre cell walls by tunnelling bacteria (arrowhead). All cell wall regions, including the highly lignified middle lamella (asterisks), are tunnelled. The direction of tunnelling (arrows) is variable. Scale bar = 8 µm. The image is reproduced from Singh et al. [<a href="#B144-forests-15-00889" class="html-bibr">144</a>].</p>
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<p>SEM micrograph of wood cell walls undergoing bacterial erosion, with rod-shaped erosion bacteria present in the erosion troughs. The micrograph is courtesy of Professor Charlotte Björdal, University of Gothenburg, Sweden.</p>
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<p>TEM of a transversely cut tracheid cell wall attacked by erosion bacteria (EB). EB are present opposite crescent-shaped erosion troughs formed in the exposed face of the secondary wall (arrowheads). The middle lamella is not degraded (arrow). RM, residual material. Scale bar = 4 µm. The image is reproduced from Singh et al. [<a href="#B22-forests-15-00889" class="html-bibr">22</a>].</p>
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<p>TEM of a transversely cut tracheid cell wall attacked by erosion bacteria (EB). EB are positioned opposite erosion troughs and display a near-circular form (arrowheads). The much smaller bacteria (asterisks) within the residual material (RM) are secondary degraders (scavenging bacteria). Scale bar = 2 µm. The image is reproduced from Singh et al. [<a href="#B44-forests-15-00889" class="html-bibr">44</a>].</p>
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<p>LM of transversely cut sections from the outer part of a waterlogged archaeological wood (Daebudo ship), stained with toluidine blue. The secondary cell wall of tracheids is extensively degraded, but the middle lamella is resistant. The earlywood (EW) and latewood (LW) cells are filled with a residual material, which appears more intensely stained in some cells than others (white vs. black asterisks), reflecting compositional heterogeneity. The images are reproduced from Cha et al. [<a href="#B9-forests-15-00889" class="html-bibr">9</a>].</p>
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<p>Confocal laser scanning micrograph (CLSM) of a transversely cut section from a waterlogged archaeological wood degraded by erosion bacteria. Based on acriflavine-enhanced lignin fluorescence, the strong fluorescence displayed by the residual material (asterisks) reflects its high lignin content. Scale bar = 15 µm. The image is reproduced from Singh et al. [<a href="#B6-forests-15-00889" class="html-bibr">6</a>].</p>
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<p>TEM of a transversely cut section from a waterlogged archaeological wood degraded by erosion bacteria. The micrograph shows the presence of the S3 layer despite the extensive degradation of the S2 layer of tracheid cell walls. Scale bar = 2 µm. The image is reproduced from Cha et al. [<a href="#B9-forests-15-00889" class="html-bibr">9</a>].</p>
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<p>TEM of a transversely cut section through parts of mild compression wood tracheids from a Schöningen spear. The cell wall degradation by erosion bacteria (arrows) is confined to the innermost part of the cell wall (boxed region). Scale bar = 1 µm. The image is reproduced from Schmitt et al. [<a href="#B25-forests-15-00889" class="html-bibr">25</a>].</p>
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<p>CLSM of a semi-thin section from a waterlogged archaeological wood degraded by erosion bacteria. The micrograph from the section, which was stained with acriflavine to enhance lignin fluorescence, shows the resistance of initial pit borders to bacterial erosion (arrowheads). The image is reproduced from Cha et al. [<a href="#B9-forests-15-00889" class="html-bibr">9</a>].</p>
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15 pages, 2487 KiB  
Article
Extraction of Soluble Salts and Iron Sulfides from the Wood of the “Huaguangjiao I” Shipwreck
by Xueyu Wang and Naisheng Li
Forests 2023, 14(12), 2432; https://doi.org/10.3390/f14122432 - 13 Dec 2023
Cited by 1 | Viewed by 1026
Abstract
Shipwreck wood often contains soluble salts and iron sulfides, which pose a threat to its stability. Therefore, desalination treatment must be carried out during protection. In this study, deionized water and ethylene diamine tetraacetic acid disodium salt (EDTA-2Na) solution were used to extract [...] Read more.
Shipwreck wood often contains soluble salts and iron sulfides, which pose a threat to its stability. Therefore, desalination treatment must be carried out during protection. In this study, deionized water and ethylene diamine tetraacetic acid disodium salt (EDTA-2Na) solution were used to extract soluble salts and iron sulfides from the 511 wood components of the “Huaguangjiao I” shipwreck. The extraction lasted for 1120 days, during which extraction progress was monitored by measuring the electrical conductivity and iron content of the soaking solution. The results indicated that the extraction experiment reached its endpoint when the conductivity of the soaking solution was maintained at 80~100 μs/cm and the iron content was maintained at 8~15 mg/L. More than 143.35 kg of iron were extracted from the wood of the “Huaguangjiao I” shipwreck. After extraction, the content of soluble salt ions in the wood were less than 5 μg/g, with an iron content below 5%. The wood has returned to its original color and with a certain degree of degradation. “Huaguangjiao I” was the first large-scale marine shipwreck to complete the desalination treatment of all wooden components. This study provides guidance for the desalination treatment of large-scale wooden shipwrecks. Full article
(This article belongs to the Collection Historical Wood: Structure, Properties and Conservation)
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<p>Extraction tank: (<b>a</b>) Tank 1; (<b>b</b>) Tank 2.</p>
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<p>Conductivity monitoring points.</p>
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<p>Electrical conductivity of the soaking solution.</p>
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<p>Iron content of the soaking solution.</p>
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<p>Changes of sulfur and iron contents in wood, (<b>a</b>) iron (<b>b</b>) sulfur.</p>
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<p>Changes in wood color: (<b>a</b>) Δ<span class="html-italic">E</span>* (<b>b</b>) <span class="html-italic">L</span>* (<b>c</b>) <span class="html-italic">a</span>* (<b>d</b>) <span class="html-italic">b</span>*.</p>
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21 pages, 11579 KiB  
Article
The Unseen Record: Ninth–Seventh Millennia Cal. BP Wooden and Basketry Objects from Submerged Settlements off the Carmel Coast, Israel
by Danny Rosenberg, Ehud Galili and Dafna Langgut
Forests 2023, 14(12), 2373; https://doi.org/10.3390/f14122373 - 5 Dec 2023
Cited by 2 | Viewed by 2107
Abstract
Wood and basketry artefacts rarely survive in the prehistoric record since they require exceptional conditions for preservation; as a result, the current knowledge about when and how prehistoric societies used these basic organic raw materials is limited. Focusing on the southern Levant, we [...] Read more.
Wood and basketry artefacts rarely survive in the prehistoric record since they require exceptional conditions for preservation; as a result, the current knowledge about when and how prehistoric societies used these basic organic raw materials is limited. Focusing on the southern Levant, we discuss for the first time a collection of 16 late prehistoric organic artefacts found in underwater research conducted in the last forty years off the coast of the Carmel Ridge (Israel). The waterlogged finds, including bowls, shafts, a wedge, a trough, a pitchfork, logs, a mat, and a basket, were found at sites spanning from the Pre-Pottery Neolithic to Middle Chalcolithic periods (ninth–seventh millennia cal. BP), constituting an unprecedented record of prehistoric wood and other perishable materials, providing us with new information about raw material preferences and manufacturing technologies. Full article
(This article belongs to the Collection Historical Wood: Structure, Properties and Conservation)
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<p>A map of the study area and the sites mentioned in the text; (<b>a</b>) general regional map with the study area marked by a red square, and (<b>b</b>) the Carmel Coast and the submerged settlements (modified after [<a href="#B30-forests-14-02373" class="html-bibr">30</a>]).</p>
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<p>(<b>a</b>) A plan of Atlit-Yam and the location of Well S.11 and Pit S.32/A; (<b>b</b>) Well S.11 (E. Galili and I. Grinberg).</p>
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<p>Wooden artefacts recovered from Well S.11: (<b>a</b>) bowl fragment AY 2, (<b>b</b>) shaft fragment AY 3, and (<b>c</b>) wooden wedge AY 5, and (<b>d</b>) a schematic depiction of the use of a wedge to split a wooden log (E. Galili and IAA).</p>
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<p>Fragmented wooden shaft AY 6 from Pit S.32/A (E. Galili).</p>
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<p>A well in Kfar Samir lined with altering courses of wooden branches and stones: (<b>A</b>) the well before the excavation, (<b>B</b>) The well during excavation, and (<b>C</b>), a schematic drawing of the well (E. Galili).</p>
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<p>Wooden bowl KS 1 with a pierced handle from Kfar Samir’s central sector: (<b>a</b>,<b>b</b>) the bowl and (<b>c</b>) a schematic illustration of the bowl’s context of recovery (IAA).</p>
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<p>Fragments of basket KS 2 from Kfar Samir’s central sector: (<b>a</b>) the basket in context, (<b>b</b>) the basket after cleaning, and (<b>c</b>) a schematic drawing of the basket’s braiding technique (E. Galili and IAA).</p>
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<p>Mat fragment KS 3 from Kfar Samir’s central sector: (<b>a</b>) the mat and (<b>b</b>) a schematic illustration of the mat’s braiding technique (IAA).</p>
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<p>Wooden bowl KS 4 from Kfar Samir’s southern sector: (<b>a</b>,<b>b</b>) the bowl, (<b>c</b>) the outer face of the base with production marks on the wall (marked in arrow), (<b>d</b>) a drawing of the bowl, (<b>e</b>) tool mark scars on the bowl’s exterior, and (<b>f</b>) a proposed reconstruction of the bowl’s shaping (E. Galili and IAA).</p>
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<p>Wooden trough KS 5 and two-pronged fork KS 6 from Kfar Samir: (<b>a</b>) the trough and the two-pronged fork in situ, (<b>b</b>) a schematic depiction of their position at the time of recovery, and (<b>c</b>) trough KS 5 (E. Galili).</p>
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<p>Two-pronged fork KS 6 from Kfar Samir: (<b>a</b>) the fork after recovery and (<b>b</b>) a possible function as part of a fishing net (Alexandria, Egypt) (E. Galili).</p>
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<p>Wooden bowl KC 1 from Hishuley Carmel (K. Alaverdian and E. Galili). (<b>a</b>) a photo of the bowl and (<b>b</b>) drawing of the bowl and sections.</p>
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<p>A structure in Kfar Galim made of wooden branches (possibly a water well) containing three wooden logs. The retrieved log (KG 1) is marked with an arrow (E. Galili).</p>
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<p>Worked wooden log KG 1 (K. Alaverdian and E. Galili).</p>
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<p>Wooden bowl TH 1 from Tel Hreiz: (<b>a</b>,<b>b</b>) the bowl and the flint blade found in it; (<b>c</b>) the flint blade; and (<b>d</b>) a drawing of the bowl and the flint blade in it (K. Alaverdian).</p>
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<p>Braided circle TH 2 from Tel Hreiz in situ (E. Galili).</p>
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24 pages, 8046 KiB  
Article
Characterization of Microbial Decay and Microbial Communities in Waterlogged Archaeological Rosewood (Dalbergia Species)
by Jong Sik Kim, Minseok Kim, Ju Won Lim, Mi Young Cha, Kwang Ho Lee, Yong Hee Yoon and Yoon Soo Kim
Forests 2023, 14(10), 1992; https://doi.org/10.3390/f14101992 - 3 Oct 2023
Cited by 4 | Viewed by 1346
Abstract
While numerous studies have examined microbial attacks on waterlogged archaeological wood, limited information is available regarding microbial attacks in waterlogged tropical hardwoods submerged in marine environments. In this context, we explored microbial attacks in waterlogged archaeological rosewood (Dalbergia species), a tropical hardwood [...] Read more.
While numerous studies have examined microbial attacks on waterlogged archaeological wood, limited information is available regarding microbial attacks in waterlogged tropical hardwoods submerged in marine environments. In this context, we explored microbial attacks in waterlogged archaeological rosewood (Dalbergia species), a tropical hardwood species that was submerged in the Yellow Sea for approximately 700 years, using various microscopic techniques and next-generation sequencing (NGS) methods. Based on morphological features, Type-I soft rot decay was identified as the main decay type. Most fibers in waterlogged archaeological rosewood studied were gelatinous (G) fibers of tension wood and the mode of soft rot decay differed from fibers without the G-layer. Differences in decay resistance between vessel/axial parenchyma cells and fibers were not obvious. Vestured- and simple pit membranes showed higher decay resistance than vessel and axial parenchyma cell walls, respectively. Microbial community analysis by NGS revealed the dominance of Ascomycota and Basidiomycota in the fungal community. Various bacterial communities were also identified, although no prominent signs of bacterial decay were noted. The identified bacterial communities markedly differed from those reported previously in terms of their composition and abundance. Together, our results offer detailed insights into the microbial types and communities responsible for degrading waterlogged archaeological rosewood, contributing to a better understanding of microbial attacks in tropical hardwoods exposed to marine environments. Full article
(This article belongs to the Special Issue Wood as Cultural Heritage Material)
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<p>Studied waterlogged archaeological rosewood. (<b>A</b>) Black arrow indicates the sampling site. (<b>B</b>) Surface of waterlogged archaeological rosewood showing brownish coloration with brash fractures. (<b>C</b>) Transverse plane of waterlogged archaeological rosewood showing the formation of cracks along with growth rings (white arrow). Note the semicircular disk cut from the top end of waterlogged archaeological rosewood for the experiment (asterisk).</p>
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<p>Anatomy of fiber cell walls at a depth of 25 mm in waterlogged archaeological rosewood stained with toluidine blue (<b>A</b>,<b>B</b>) and KMnO<sub>4</sub> (<b>E</b>–<b>J</b>). (<b>A</b>) Anatomy of waterlogged archaeological rosewood showing diffuse porous type of vessel (V) porosity, axial parenchyma cells (AP) arranged around vessels (paratracheal), and uniseriate/biseriate rays (R). (<b>B</b>–<b>D</b>) Fibers with and without (white asterisks in (<b>B</b>)) gelatinous (G) layers. G-layers showed strong blue coloration (<b>B</b>), weak lignin autofluorescence (<b>B</b>), and cellulose microfibrils oriented nearly parallel to the fiber axis (double arrowheads in (<b>D</b>)). Several G-fibers showed the formation of a lignified (L) layer between the S<sub>2</sub> and G-layers (inset in (<b>C</b>)). Note the multilayered narrow lignified (nL) layers in the inner secondary cell walls of fibers without the G-layer (inset in (<b>B</b>)) and strong autofluorescence in the lumen and/or lumen wall (white arrows in (<b>C</b>)). (<b>E</b>–<b>J</b>) Fibers with various cell wall structures: S<sub>1</sub>–S<sub>3</sub> (<b>E</b>,<b>F</b>,<b>J</b>), S<sub>1</sub> + S<sub>2</sub> + S<sub>3</sub> + <span class="html-italic">n</span> (nL) (<b>E</b>–<b>G</b>), S<sub>1</sub> + S<sub>2</sub> + G (<b>H</b>,<b>I</b>), and S<sub>1</sub> + S<sub>2</sub> + G + L (<b>E</b>,<b>I</b>). Note the thin lamellae developed within the G-layer (arrowheads in (<b>G</b>,<b>H</b>)), uneven patterns of KMnO<sub>4</sub> staining intensity across the G-layer (asterisks in (<b>J</b>)), thin concentric lines with strong KMnO<sub>4</sub> staining intensity between the nL-layers (white arrowheads in the inset of (<b>G</b>)), and the accumulation of phenolic extractives in the lumen and/or lumen wall (black arrows in (<b>E</b>,<b>F</b>,<b>H</b>,<b>J</b>)).</p>
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<p>Degradation of fibers at a depth of 4 and 25 mm in waterlogged archaeological rosewood stained with toluidine blue. (<b>A</b>) Fibers without gelatinous (G) layers showing the formation of soft rot cavities in secondary cell walls (arrowheads). Inset indicates the SEM micrograph of corresponding fibers. (<b>B</b>) Fibers with G-layers showing degradation at the boundary of the S<sub>2</sub> and G-layers. The inset reveals the SEM micrograph of corresponding G-fibers. (<b>C</b>,<b>D</b>) Longitudinal sections showing the formation of cavities aligned along cellulose microfibrils in fibers without G-layers (arrows in (<b>C</b>)). Note the absence of cavity formation in G-layers (<b>D</b>). (<b>E</b>) Fibers with a relatively wide lumen showing the erosion type of decay (asterisks).</p>
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<p>Degradation of fibers without gelatinous (G) layers at a depth of 4 and 25 mm in waterlogged archaeological rosewood stained with KMnO<sub>4</sub>. (<b>A</b>) Formation of soft rot cavities (asterisks) in S<sub>2</sub> layers at the early stages of decay. Note the absence of cavity formation in the narrow lignified (nL) layer (inset). (<b>B</b>,<b>C</b>) Coalescence between adjoining cavities with the progression of decay. Note the nL-layer with an almost intact structure (<b>C</b>) and electron-dense materials detected around decayed cell wall regions in cavities (arrowheads). (<b>D</b>) Cell wall penetration by fungal hyphae across the middle lamella (ML, arrows).</p>
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<p>Degradation of gelatinous (G) fibers at a depth of 4 and 25 mm in waterlogged archaeological rosewood stained with KMnO<sub>4</sub>. (<b>A</b>) Formation of soft rot cavities at the boundary of S<sub>2</sub> and G-layers at the early stages of decay (asterisks). The cavity was more biased toward the S<sub>2</sub> layers than the G-layers (inset). Note cell wall penetration across the G-layer (white arrowhead). (<b>B</b>,<b>C</b>) Degradation of S<sub>2</sub> and G-layers with the progression of decay. Note the presence of electron-dense materials around decayed cell wall regions in cavities (black arrowheads). (<b>D</b>) Advanced stages of decay showing an almost completely decayed G-layer, with a remaining highly lignified (L) layer. Note the absence of cavity formation and decay (black arrows) in the lignified (L) layer. The inset indicates cell wall penetration by fungal hyphae across the G-layer, normal secondary wall, and middle lamella (white arrows in the inset).</p>
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<p>Erosion type of decay in gelatinous (G) fibers at a depth of 4 and 25 mm in waterlogged archaeological rosewood stained with KMnO<sub>4</sub>. (<b>A</b>) Erosion trough-like localized depressions in the G-layer (arrowheads) across the extractive layer (arrows). Note the relatively wider cell lumen than that of G-fibers described in <a href="#forests-14-01992-f005" class="html-fig">Figure 5</a>. (<b>B</b>,<b>C</b>) Progression of cell wall erosion outward from the G-layer with the progression of decay. Cell wall erosion was occasionally observed together with decay at the boundary of S<sub>2</sub> and G-layers described in <a href="#forests-14-01992-f005" class="html-fig">Figure 5</a> (inset in (<b>C</b>)). (<b>D</b>) Degradation of the S<sub>2</sub> layer beyond the G-layer at the advanced stages of decay.</p>
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<p>Degradation of fibers on the surface of waterlogged archaeological rosewood stained with toluidine blue (<b>A</b>) and KMnO<sub>4</sub> (<b>B</b>–<b>D</b>). (<b>A</b>,<b>B</b>) Fibers showing heavy decay with and without cell wall residues (black arrows in <b>A</b>,<b>B</b>). Cell wall residues showed fluorescence (assessed using CLSM; white arrows in inset) and KMnO<sub>4</sub> staining intensity similar to those noted in normal S<sub>2</sub> layers. (<b>C</b>) Fibers without a G-layer showing heavy degradation of the secondary cell wall, with the innermost layer remaining (asterisks). Note the un-decayed extractive layer even after complete degradation of the secondary cell wall (arrowhead) and more advanced stages of decay in axial parenchyma cells (AP) than in fibers. (<b>D</b>) Fiber showing degradation of the S<sub>1</sub> layer (inset), with the innermost layer (asterisks) and extractives in the lumen remaining. ML, middle lamella.</p>
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<p>Degradation of vessels and axial parenchyma cells in waterlogged archaeological rosewood stained with toluidine blue. (<b>A</b>) A sample with 25 mm axial depth showing vessels (V) in 2 multiples and axial parenchyma cells (AP) with phenolic extractives in the lumen. Note the multilayered axial parenchyma cell wall with deposits in the lumen (inset). (<b>B</b>–<b>D</b>) A surface sample showing severe degradation of vessel and parenchyma cell walls. Many irregular forms of cavities were observed in vessel cell walls (asterisks in (<b>C</b>)). Note the accumulation of materials attached to the vessel lumen (arrowheads in (<b>B</b>)). Intervessel pit membranes remained even though adjacent vessel cell walls were heavily degraded (arrows in (<b>D</b>)).</p>
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<p>Degradation of vessels (V) in waterlogged archaeological rosewood stained with KMnO<sub>4</sub> (<b>A</b>–<b>D</b>). (<b>A</b>,<b>B</b>) Vessels at the early stages of decay showing the degradation of certain deposits coating the innermost cell wall layer (black asterisks in (<b>A</b>) and right inset of (<b>A</b>)), cell wall degradation through pit chambers (<b>B</b>), and invasion of fungal hyphae into the cell wall across the extractive layer of the lumen (white arrow in the inset of (<b>B</b>)). Note the presence of vestures in the vessel cell wall (black arrows in the left inset of (<b>A</b>)) and vessel-ray pit (black arrows in the right inset of (<b>A</b>)) with a difference in KMnO<sub>4</sub> staining intensity. (<b>C</b>) A surface sample showing severe degradation of vessel cell walls with many irregular forms of cavities. Note un-decayed layered materials in the lumen (white asterisks) and degradation of the middle lamella between vessel and axial parenchyma cells (AP) (white arrowheads). (<b>D</b>) Vestured intervessel pit membranes (M) at the advanced stages of decay showing an almost intact structure (black arrowheads) even though the adjacent vessel cell walls were extensively degraded. (<b>E</b>) A sample with 1–2 mm axial depth showing fungal hyphae in the vessel lumen (white arrows) together with the formation of many small cavities in the cell wall. (<b>F</b>) Fungal conidia in the lumen showing rough surface ornamentation and an overall globose shape (inset). R, ray cell.</p>
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<p>Degradation of axial parenchyma cells (AP) in waterlogged archaeological rosewood stained with KMnO<sub>4</sub>. (<b>A</b>,<b>B</b>) Axial parenchyma cells at the early stages of decay showing cell wall degradation through simple pit chambers (black arrow in (<b>A</b>)) and across the extractive layer of the lumen (white arrow in the inset of (<b>A</b>)), in addition to the degradation of middle lamella (ML) regions ((<b>B</b>) and inset). Note the intact structure of the simple pit membrane (M) ((<b>A</b>) and inset). (<b>C</b>) Axial parenchyma cells with the formation of soft rot cavities in secondary cell walls (asterisks). (<b>D</b>) Simple pit membrane (M) at the advanced stages of decay showing an almost intact structure even though adjacent axial parenchyma cell walls were extensively degraded. Note cell wall penetration by fungal hyphae (white arrowhead). (<b>E</b>) Fibrillar structure covering the decayed axial parenchyma cell wall at the early stages of decay (black arrowheads). (<b>F</b>) A surface sample showing extensive degradation of axial parenchyma cell walls with many irregular forms of cavities.</p>
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<p>Fungal families (<b>A</b>) and genera (<b>B</b>) with a relative abundance of more than 1% in waterlogged archaeological rosewood. Parenthesis indicates fungal phylum (<b>A</b>) and family/phylum (<b>B</b>) names. AS, Ascomycota; BA, Basidiomycota.</p>
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<p>Bacterial families (<b>A</b>) and genera (<b>B</b>) with a relative abundance of more than 1% in waterlogged archaeological rosewood. Parenthesis indicates bacterial phylum (<b>A</b>) and family (<b>B</b>) names.</p>
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19 pages, 15018 KiB  
Article
Assessment of Various Iron Extraction Treatments on Waterlogged Archaeological Oak
by Charlène Pelé-Meziani, Nicola Macchioni, Lorena Sozzi, Elodie Guilminot, Gwenaël Lemoine, Benedetto Pizzo, Jean Yves Mevellec, Elisa Pecoraro and Mathilde Monachon
Forests 2023, 14(9), 1834; https://doi.org/10.3390/f14091834 - 8 Sep 2023
Cited by 1 | Viewed by 1227
Abstract
Treatments of organic objects to extract ferrous compounds from waterlogged archaeological wood are well documented. For several years, numerous laboratories have been seeking to determine suitable conservation treatments for such organic objects. For chemical treatments, complexing agents such as EDTA and DTPA, along [...] Read more.
Treatments of organic objects to extract ferrous compounds from waterlogged archaeological wood are well documented. For several years, numerous laboratories have been seeking to determine suitable conservation treatments for such organic objects. For chemical treatments, complexing agents such as EDTA and DTPA, along with acids such as citric and oxalic acids, were selected. In addition, oxidants and reducing agents were tested as pre-treatments to improve extraction rates. In fact, chemicals produce a selective reaction on ferrous compounds, which may improve or be inhibited by complexation or dissolution reactions. Their action depends on the type of compound to be extracted and those present inside the wood. The objective of this study was to make a comparative assessment of the various chemical conservation treatments identified and complement the evaluation of their extraction efficiency with a study of their impact on organic matter by adding criteria such as their visual aspect (using a spectrocolorimeter) and physicochemical actions by means of infrared spectroscopy and micromorphological observations. The effectiveness of EDTA was confirmed, as was that of citric acid, despite some questions arising concerning the presence of wood fibers in the treatment solution, even after rinsing. On the other hand, the extraction rate of oxalic acid, which has a very acidic pH, was unsurprisingly lower, but its visual and anatomical results raised the possibility of using it over a short period of time in view of the effectiveness observed on the wood surface. Pre-treatments improved extraction rates, except in the case of EDTA, which independently had a high extraction rate. It was observed that pre-treatments did not appear to cause any significant chemical degradation of the organic matter. This study provides a tool to assist conservators in selecting a chemical treatment that is in line with the state of decay of the wood, the characteristics of the ferrous compounds to be extracted, and the conservation objectives. Full article
(This article belongs to the Special Issue Wood as Cultural Heritage Material)
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<p>Waterlogged archaeological wood from the archaeological site “Saint-Lupien”, Rezé, Nantes (FRANCE), and below, samples after cutting (3 × 3 × 3 cm) used for extraction treatments.</p>
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<p>Raman spectra carried out on a reference sample (#45), pyrite (with bands at 472, 435, 243, 220, and 151 cm<sup>−1</sup>), and hematite (with bands at 617, 410, 295, and 227 cm<sup>−1</sup>).</p>
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<p>Cross sections of archaeological samples after treatment. #1—EDTA, the red arrow shows the decayed material inside the lumen, and the blue arrow shows the compound middle lamella of the same cell; #4—Sodium dithionite, the red arrow points to a black spot of ferrous compounds in cell lumens; #7—Sodium persulfate + EDTA, the picture highlights a section of latewood, while on the right is a large ray well impregnated with black ferrous compounds. Scale bars: 100 µm.</p>
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<p>Sections of archaeological samples after treatment. #10—DTPA cross section showing the decayed secondary wall impregnated with black iron compounds. Scale bar: 200 µm; #22—Sodium dithionite + DTPA, longitudinal tangential section showing blackish tyloses in a vessel lumen; #27—Sodium dithionite + DTPA, cross section: the red arrow points to the decayed secondary wall impregnated with black iron compounds, while the blue arrow points to the remaining compound middle lamella. Scale bar: 100 µm.</p>
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<p>Cross sections of archaeological samples after treatment. #28—Citric acid, a latewood vessel, surrounded by longitudinal parenchymatic cells and some fibers showing decayed blackish secondary walls detached from the compound middle lamella, which are more visible in #31—Sodium persulfate + citric acid—where the red arrow points to the darker secondary wall, detached from the compound middle lamella (blue arrow). Scale bar: 100 µm.</p>
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<p>Cross sections of archaeological samples after treatment. #34—Oxalic acid shows a growth ring limit, with cell walls and cell lumens being quite light colored; #37—Sodium persulfate + Oxalic acid, the red arrow points to the decayed light-colored secondary wall, and the blue arrow points to the compound middle lamella of the same cell. Some of the latewood vessels are losing their rounded/oval shape. Scale bars: 100 µm.</p>
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<p>Ratios of lignin and carbohydrates for impregnated and non-impregnated samples subsequently treated with EDTA. FTIR analysis, carried out after an immersion period of 0.5 months and 6 months.</p>
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<p>Ratios of lignin and carbohydrates for impregnated and non-impregnated references after an immersion period of 0.5 months and 6 months in water.</p>
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<p>FTIR spectra of the reference #43 (in black) and of samples #37 (in green) and #34 (in red) immersed in oxalic acid.</p>
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18 pages, 1648 KiB  
Article
Assessing the Versatility of Bioextraction to Preserve Waterlogged Wood
by Mathilde Monachon, Charlène Pelé-Meziani, Sathiyanarayanan Ganesan, Sabine de Weck, Friederike Moll-Dau, Janet Schramm, Katharina Schmidt-Ott and Edith Joseph
Forests 2023, 14(8), 1656; https://doi.org/10.3390/f14081656 - 16 Aug 2023
Viewed by 1076
Abstract
An innovative bio method was investigated to extract harmful iron and sulfur species from waterlogged wood samples. The method was compared with a chemical treatment. Both approaches were applied on lacustrine and marine samples, from different wood genera, to evaluate the versatility of [...] Read more.
An innovative bio method was investigated to extract harmful iron and sulfur species from waterlogged wood samples. The method was compared with a chemical treatment. Both approaches were applied on lacustrine and marine samples, from different wood genera, to evaluate the versatility of the proposed bio method. Non-invasive and non-destructive methods were carried out to investigate both bio-based and chemical treatments. The result was that some wood genera were more affected by the bio approach, with a clear distinction between lacustrine beech and pine against oak and lime wood species. The chemical approach showed potential harm for the wooden structure, with acidic pH values and an increase of maximum water content, both implying degradation of the wood structure. In terms of extraction, no iron or sulfur products were detected by Raman spectroscopy on biologically treated samples, in agreement with extraction rates calculated. It was also suggested that iron bonded to wood was extracted with the chemical approach, and calcium content affected by both approaches. Full article
(This article belongs to the Special Issue Wood as Cultural Heritage Material)
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<p>Mean color variation (ΔE*) between before and after extraction for biologically (BT, green) and chemically (CT, blue) treated sets, compared with untreated (NT, grey) samples, with standard error. Black line indicates the threshold of eye-perceivable color variation (ΔE* = 5).</p>
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<p>Representative Raman spectra for sets biologically (green) and chemically (blue) treated, compared with untreated (grey) samples.</p>
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<p>PCA plot for all sets biologically (circle, BT) and chemically (square, CT) treated, compared with untreated (triangle, NT) samples, for the degradation variables pH, maximum water content (Umax) and ATR-FTIR ratio (R1).</p>
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17 pages, 4960 KiB  
Article
Physico-Mechanical Properties of Waterlogged Archaeological Wood: The Case of a Charred Medieval Shipwreck
by Eirini Mitsi, Nikolaos-Alexios Stefanis and Anastasia Pournou
Forests 2023, 14(3), 560; https://doi.org/10.3390/f14030560 - 12 Mar 2023
Cited by 1 | Viewed by 2467
Abstract
In 2008, a late-12th-century merchant ship was discovered off the commercial port of Rhodes. The vessel caught fire before sinking and thus numerous hull timbers were found charred. Three main degrees of charring have been recorded that presented major chemical differences which indicated [...] Read more.
In 2008, a late-12th-century merchant ship was discovered off the commercial port of Rhodes. The vessel caught fire before sinking and thus numerous hull timbers were found charred. Three main degrees of charring have been recorded that presented major chemical differences which indicated different conservation requirements. This study investigated the correlation between the chemistry of the waterlogged timbers and their physico-mechanical properties, to assist in the development of an appropriate conservation strategy. Scanning electron microscopy documented the morphology of charred, semi-charred and uncharred samples. Moisture content and density were measured gravimetrically, while porosity was evaluated using mercury intrusion porosimetry. Hardness was assessed using a modified Janka test and a penetrometer. The results obtained showed that differences in chemistry were highly correlated to the physico-mechanical properties of the timbers. The charred wood presented the lowest moisture content, shrinkage and porosity among the three charring conditions and it also had the highest density, Janka hardness and resistance to penetration. The exact reverse properties were recorded for the uncharred material, which was typical of badly preserved, waterlogged wood. The semi-charred wood presented transitional features. These results indicate that the uncharred wood is in need of consolidation, in contrast to the charred and semi-charred material, which may be left to air-dry untreated. Full article
(This article belongs to the Special Issue Waterlogged Archaeological Woods)
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<p>The frame part used, presenting an outer charred layer, an uncharred inner core and a semi-charred zone in between.</p>
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<p>(<b>a</b>) Graphic representation of the ball penetrated into a depth of ½ and ¼ of its diameter, and (<b>b</b>) the radius (r) of projected contact area that based on Pythagoras’ theorem is equal to <math display="inline"><semantics> <mrow> <mi>r</mi> <mo>=</mo> <msqrt> <mrow> <mrow> <mo>(</mo> <mrow> <msup> <mi>R</mi> <mn>2</mn> </msup> <mo>−</mo> <msup> <mi>h</mi> <mn>2</mn> </msup> </mrow> <mo>)</mo> </mrow> </mrow> </msqrt> </mrow> </semantics></math>, where R = ball radius, h = R − e, and e = extension recorded by Instron.</p>
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<p>SEM micrographs of uncharred, semi-charred and charred wood. Uncharred material (<b>a</b>–<b>c</b>) presented a granular texture (gr) of the secondary cell walls, which were often detached (dt) from the middle lamellae; semi-charred wood (<b>d</b>–<b>f</b>) showed intact cell walls with rare detachment fissures (fs); and charred wood (<b>g</b>–<b>i</b>) presented a vitreous appearance without evident biodeterioration signs. On both uncharred (<b>b</b>,<b>c</b>) and semi-charred (<b>e</b>,<b>f</b>) material, biodeterioration patterns caused by bacteria (bc) and fungi (fg) were recognized. All bars are 10 μm.</p>
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<p>Moisture content (MC), equilibrium moisture content (EMC), basic density (Rg) and cross shrinkage (β<sub>cross</sub>) values recorded for uncharred, semi-charred and charred archaeological material, juxtaposed to controls of <span class="html-italic">P. brutia</span> and <span class="html-italic">P. halepensis</span>.</p>
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<p>Histograms of intruded pore volume as a function of the pore radius of controls (<span class="html-italic">P. brutia</span> and <span class="html-italic">P. halepensis</span>) and archaeological wood (uncharred, semi-charred and charred).</p>
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<p>Differential pore-size distribution curves and cumulative intrusion curves of controls (<span class="html-italic">P. brutia</span> and <span class="html-italic">P. halepensis</span>) and the three conditions of the archaeological wood (uncharred, semi-charred and charred).</p>
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<p>End and side (radial and tangential) hardness of the archaeological wood at the freeze-dried (FD) and at the waterlogged (W) state in comparison to the hardness of sound <span class="html-italic">P. brutia</span> and <span class="html-italic">P. halepensis,</span> of which earlywood-latewood values were averaged.</p>
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<p>Graphical representation of the resistance to penetration values recorded on a sample, where all three charring conditions charred (i), semi-charred (ii) and uncharred (iii) coexisted.</p>
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<p>Correlation between resistance to penetration and Rg for the three charring conditions of uncharred, semi-charred and charred archaeological wood. Penetration points in each charring condition are plotted against the average Rg values of each condition calculated using four replicates. The error bars represent the standard deviation of Rg.</p>
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12 pages, 7898 KiB  
Article
Analyses of Sulfur and Iron in Waterlogged Archaeological Wood: The Case of Polyethylene-Glycol-Treated Yenikapı 12 Shipwreck
by Aslı Gökçe Kılıç, Namık Kılıç and Donna C. Arnold
Forests 2023, 14(3), 530; https://doi.org/10.3390/f14030530 - 8 Mar 2023
Cited by 1 | Viewed by 1954
Abstract
The Yenikapı (YK) 12 shipwreck is 1 of 37 shipwrecks found at Yenikapı, Istanbul. This merchantman has been dated to AD 672–876 by radiocarbon analyses. The conservation of YK 12, which was assembled with iron nails, was completed with the pre-impregnation of polyethylene [...] Read more.
The Yenikapı (YK) 12 shipwreck is 1 of 37 shipwrecks found at Yenikapı, Istanbul. This merchantman has been dated to AD 672–876 by radiocarbon analyses. The conservation of YK 12, which was assembled with iron nails, was completed with the pre-impregnation of polyethylene glycol (PEG) and using vacuum freeze-drying processes. However, after conservation, dust formation was observed on some wooden parts of the shipwreck during storage. In this study, iron–sulfur-related problems detected in the woods of YK 12 were evaluated. We analysed samples taken from YK 12 to study the sulfur and iron content in woods from oak (Quercus), walnut (Juglans), and hornbeam (Carpinus), representing taxa with different wood properties. Fourier-transform infrared spectroscopy (FTIR) analyses, X-ray diffraction (XRD), and pH measurements were conducted on five samples. The results of these studies showed that the dust consisted of wood particles, PEG, and hydrated iron sulfates, such as FeSO4·4H2O and FeSO4·7H2O. Additionally, one sample included SiO2, whilst another exhibited a low pH value. These findings highlight the importance of optimum ambient conditions for the storage and display of these shipwrecks in order to prevent the irreversible degradation of YK 12 and other recovered shipwrecks. Full article
(This article belongs to the Collection Historical Wood: Structure, Properties and Conservation)
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<p>Photo of the Yenikapı 12 shipwreck (<b>©</b> IU Yenikapı Shipwrecks Project Archive).</p>
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<p>Schematic representation of the YK 12 shipwreck showing the sampling points denoted E8, E9, E11, E13, and E17 (I. Özsait-Kocabaş).</p>
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<p>FTIR spectra collected for the E8 and E17 dust samples, PEG, and archaeological wood samples.</p>
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<p>FTIR spectra collected for the E9, E11, and E13 dust samples, PEG, and archaeological wood samples.</p>
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<p>FTIR spectra collected for fresh hornbeam, PEG, and the wood sample collected at the E8 site.</p>
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<p>FTIR spectra collected for fresh oak, PEG, and the E9, E11, and E17 archaeological wood samples.</p>
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<p>FTIR spectra collected for fresh walnut, PEG, and the E13 archaeological wood sample.</p>
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<p>Comparison plot of the X-ray diffraction data collected for the dust samples collected for E8, E9, E11, E13, and E17. Patterns are shifted for clarity, and E17 is enhanced by a factor of 4 to allow comparisons.</p>
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<p>Photographs taken to illustrate the areas where pH values were measured for (<b>a</b>) E8, (<b>b</b>) E9, (<b>c</b>) E11, (<b>d</b>) E13, and (<b>e</b>) E17.</p>
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12 pages, 2609 KiB  
Article
Size Effect on Hygroscopicity of Waterlogged Archaeological Wood by Simultaneous Dynamic Vapour Sorption
by Liuyang Han, Dehao Yu, Tiantian Liu, Xiangna Han, Guanglan Xi and Hong Guo
Forests 2023, 14(3), 519; https://doi.org/10.3390/f14030519 - 7 Mar 2023
Cited by 4 | Viewed by 1536
Abstract
Hygroscopicity is one of the most important properties of wood and plays a decisive role in its dimensional stability. In this context, conservation plans for waterlogged archaeological wood (WAW) and relevant waterlogged artefacts must be created. The size of the sample required for [...] Read more.
Hygroscopicity is one of the most important properties of wood and plays a decisive role in its dimensional stability. In this context, conservation plans for waterlogged archaeological wood (WAW) and relevant waterlogged artefacts must be created. The size of the sample required for a moisture sorption assessment may affect the results for (and thus the perception of) the hygroscopicity of a testing artefact. Herein, to investigate the effects of the sample size on the hygroscopicity of WAW as measured via dynamic vapour sorption (DVS), typical WAW and recent (i.e., sound) wood are processed into four differently sized samples, ranging in thickness from 200 mesh to millimetre. The equilibrium moisture contents (EMCs) of the wood samples are simultaneously measured using simultaneous DVS. The sorption isotherms show that the EMC values of the recent wood at each relative humidity increase as the sample size decreases, with the superfine powder sample achieving the highest EMC of all of the recent samples. Although the WAW has a higher EMC than that of recent wood, the effect of the size of the WAW sample on its hygroscopic properties is surprisingly not as pronounced as that for the recent wood. In addition, the hysteresis between the samples of different sizes of the archaeological wood is significantly smaller than that for the reference samples. Furthermore, regarding the standard deviations of the parameters obtained from the Guggenheim Anderson de Boer and Hailwood–Horrobin models, the values for WAW are all much smaller than those for the reference wood. This further verifies the disappearance of the size effect of the hygroscopicity for WAW. Full article
(This article belongs to the Special Issue Wood Conversion, Engineered Wood Products and Performance Testing)
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<p>Scheme for the preparation and the testing of the DVS samples.</p>
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<p>Equilibrium moisture content (EMC) sorption isotherms of the reference samples (<b>A</b>) and WAW samples (<b>B</b>) versus relative humidity (RH) ranging from 0 to 98%.</p>
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<p>Hysteresis values of reference samples (<b>A</b>) and WAW samples (<b>B</b>) versus RH.</p>
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<p><span class="html-italic">M</span><sub>h</sub> of reference samples (<b>A</b>) and WAW samples (<b>B</b>) in adsorption process. <span class="html-italic">M</span><sub>s</sub> of reference samples (<b>C</b>) and WAW samples (<b>D</b>) in adsorption process.</p>
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<p><span class="html-italic">M</span><sub>h</sub> of reference samples (<b>A</b>) and WAW samples (<b>B</b>) in desorption process. <span class="html-italic">M</span><sub>s</sub> of reference samples (<b>C</b>) and WAW samples (<b>D</b>) in desorption process.</p>
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16 pages, 13100 KiB  
Article
Earlywood Anatomy Highlights the Prevalent Role of Winter Conditions on Radial Growth of Oak at Its Distribution Boundary in NW Iberia
by Ignacio García-González and Manuel Souto-Herrero
Plants 2023, 12(5), 1185; https://doi.org/10.3390/plants12051185 - 6 Mar 2023
Viewed by 1713
Abstract
We compared climate–growth relationships (1956–2013) of two natural pedunculate oak (Quercus robur L.) stands with different water-holding capacities growing at the species distribution limit of the Mediterranean Region in NW Iberia. For this, tree-ring chronologies of earlywood vessel size (separating the first [...] Read more.
We compared climate–growth relationships (1956–2013) of two natural pedunculate oak (Quercus robur L.) stands with different water-holding capacities growing at the species distribution limit of the Mediterranean Region in NW Iberia. For this, tree-ring chronologies of earlywood vessel size (separating the first row from the other vessels) and latewood width were obtained. Earlywood traits were coupled to conditions during dormancy, whereby an elevated winter temperature appears to induce a high consumption of carbohydrates, resulting in smaller vessels. This effect was reinforced by waterlogging at the wettest site, whose correlation to winter precipitation was strongly negative. Soil water regimes caused differences between vessel rows, since all earlywood vessels were controlled by winter conditions at the wettest site, but only the first row at the driest one; radial increment was related to water availability during the previous rather than the current season. This confirms our initial hypothesis that oak trees near their southern distribution boundary adopt a conservative strategy, prioritizing reserve storage under limiting conditions during the growing period. We believe that wood formation is highly dependent on the balance between the previous accumulation of carbohydrates and their consumption to maintain both respiration during dormancy and early spring growth. Full article
(This article belongs to the Section Plant Ecology)
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<p>Boxplots of vessel size distribution (area in µm<sup>2</sup>) at each site (<b>a</b>), percentage of conductivity carried out by the first row or other vessels (<b>b</b>), and descriptive statistics (mean ± standard deviation) (<b>c</b>); values in brackets represent the coefficient of variation. Tree codes are numbered correlatively according to their site (WET or DRY).</p>
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<p>Comparison between site and variable chronologies, with their corresponding descriptive statistics, for hydraulically weighted diameter of first row vessels (<span class="html-italic">D</span><sub>H</sub>-r1), mean vessel diameter outside that row (<span class="html-italic">mvd</span>-nr1), and latewood width (LW) along the common interval 1956–2013. <span class="html-italic">Rbt</span>: mean correlation between trees; <span class="html-italic">SNR</span>: signal-to-noise ratio, <span class="html-italic">EPS</span>: expressed population signal; <span class="html-italic">MS</span>: mean sensitivity; <span class="html-italic">AR1</span>: first order autocorrelation coefficient.</p>
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<p>Climate–growth relationships for the earlywood (<span class="html-italic">D</span><sub>H</sub>-r1 and <span class="html-italic">mvd</span>-nr1) and latewood (LW) chronologies for the period 1956–2013 (58 years); results are expressed as Pearson’s correlation coefficients, with their significance obtained by 10,000 bootstrap replications. Only significant correlations are highlighted. <span class="html-italic">D</span><sub>H</sub>-r1: hydraulically weighted diameter of the first row; <span class="html-italic">mvd</span>-nr1: mean vessel diameter of vessels not belonging to the first row; LW: latewood width; <span class="html-italic">P</span>: total precipitation; <span class="html-italic">T</span>: mean temperature; <span class="html-italic">Tmin</span>: mean of minimum daily temperatures; <span class="html-italic">Tmax</span>: mean of maximum daily temperatures. Lower and uppercase letters correspond to the months of the previous and current growth years, respectively; climate variables are expressed as monthly records.</p>
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<p>Correlations between monthly values of the standardized precipitation-evaporation index (SPEI) at different time scales (1–21) for the earlywood (<span class="html-italic">D</span><sub>H</sub>-r1 and <span class="html-italic">mvd</span>-nr1) and latewood (LW) chronologies for the period 1956–2013 (58 years). <span class="html-italic">D</span><sub>H</sub>-r1: hydraulically weighted diameter of the first row; <span class="html-italic">mvd</span>-nr1: mean vessel diameter of vessels not belonging to the first row; LW: latewood width. Lower and uppercase letters correspond to the months of the previous and current growth years, respectively.</p>
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<p>Adjustment between growth variables and SPEI values for the months and time scales maximizing correlation at both stands for the period 1956–2013 (58 years). <span class="html-italic">D</span><sub>H</sub>-r1: hydraulically weighted diameter of the first row; <span class="html-italic">mvd</span>-nr1: mean vessel diameter of vessels not belonging to the first row; LW: latewood width.</p>
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<p>Natural distribution of <span class="html-italic">Quercus robur</span> (source: EUFORGEN 2009, <a href="https://www.euforgen.org/" target="_blank">https://www.euforgen.org/</a>, accessed on 23 July 2015) and location of the study area at its southern range boundary in the Iberian Peninsula (<b>a</b>), showing the climate diagram from a nearby weather station. Digital Terrain Models with sampled trees as white dots and physiographic characterization of the two chronology sites are also included (<b>b</b>).</p>
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