cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.2jp9vg
title: Occurrence Download

description: A dataset containing 4 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is China",
 "TaxonKey is Cestrum elegans (Brongn. ex Neumann) Schltdl."
 ]
}

 The dataset includes 4 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0093986-240506114902167/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.115316
title: Documentation of sediment core PS2469-3
DOI: 10.1594/pangaea.115317
title: Documentation of sediment core PS2470-4
DOI: 10.1594/pangaea.115485
title: Documentation of sediment core PS2735-4
DOI: 10.1594/pangaea.115043
title: Physical properties of sediment core PS63/099-2

description: Measurements and data processing by R. Usbeck (FIELAX).
DOI: 10.1594/pangaea.115318
title: Documentation of sediment core PS2471-3
DOI: 10.1594/pangaea.115044
title: Physical properties of sediment core PS63/103-1

description: Measurements and data processing by R. Usbeck (FIELAX).
DOI: 10.1594/pangaea.115319
title: Documentation of sediment core PS2471-4
DOI: 10.1594/pangaea.115045
title: Physical properties of sediment core PS63/105-2

description: Measurements and data processing by R. Usbeck (FIELAX).
DOI: 10.1594/pangaea.115160
title: Documentation of sediment core PS2174-3
DOI: 10.1594/pangaea.115320
title: Documentation of sediment core PS2472-3
DOI: 10.1594/pangaea.115321
title: Documentation of sediment core PS2473-3
DOI: 10.1594/pangaea.115046
title: Physical properties of sediment core PS63/106-1

description: Measurements and data processing by R. Usbeck (FIELAX).
DOI: 10.1594/pangaea.115161
title: Documentation of sediment core PS2174-4
DOI: 10.1594/pangaea.115047
title: Physical properties of sediment core PS63/110-1

description: Measurements and data processing by R. Usbeck (FIELAX).
DOI: 10.1594/pangaea.115162
title: Documentation of sediment core PS2174-5
DOI: 10.1594/pangaea.115486
title: Documentation of sediment core PS2736-3
DOI: 10.1594/pangaea.115163
title: Documentation of sediment core PS2175-1
DOI: 10.1594/pangaea.115487
title: Documentation of sediment core PS2737-4
DOI: 10.1594/pangaea.115164
title: Documentation of sediment core PS2175-3
DOI: 10.1594/pangaea.115322
title: Documentation of sediment core PS2473-4
DOI: 10.1594/pangaea.115488
title: Documentation of sediment core PS2739-5
DOI: 10.1594/pangaea.115323
title: Documentation of sediment core PS2474-2
DOI: 10.1594/pangaea.115324
title: Documentation of sediment core PS2474-3
DOI: 10.1594/pangaea.115325
title: Documentation of sediment core PS2475-1
DOI: 10.1594/pangaea.115165
title: Documentation of sediment core PS2175-5
DOI: 10.1594/pangaea.115166
title: Documentation of sediment core PS2176-1
DOI: 10.1594/pangaea.115167
title: Documentation of sediment core PS2176-3
DOI: 10.1594/pangaea.115168
title: Documentation of sediment core PS2176-4
DOI: 10.1594/pangaea.115489
title: Documentation of sediment core PS2740-8
DOI: 10.6084/m9.figshare.28903949
title: <b>Gut Metabolic Signatures in Polycystic Ovary Syndrome: Insights from Fecal Untargeted Metabolomics</b>

description: <b>Background: </b>Polycystic Ovary Syndrome (PCOS) is a complex endocrine and metabolic disorder, increasingly associated with gut microbial dysbiosis. Fecal metabolomics offers a promising approach to explore gut microbial activity and its metabolic consequences, yet remains underexplored in PCOS research, particularly in diverse populations.<b>Objective: </b>To investigate fecal metabolic alterations in women with PCOS compared to healthy controls using an untargeted metabolomics approach.<b>Methods: </b>Fecal samples from 24 PCOS women and 30 age-matched healthy controls were subjected to untargeted metabolite profiling using liquid chromatography-mass spectrometry. Multivariate statistical analyses, including PCA and PLS-DA, were performed to identify significant discriminatory features. Differential metabolites were subjected to pathway enrichment analysis to explore their biological significance.<b>Results: </b>A clear metabolic distinction was observed between PCOS and control groups. In total, 115 metabolites were significantly altered, with 15 upregulated and 118 downregulated in PCOS women. Identified metabolites primarily belonged to classes including bile acids, amino acids, steroid hormones, fatty acids, and phenylpropanoids. Pathway enrichment analysis revealed significant alterations in steroid biosynthesis, bile acid metabolism, tryptophan metabolism, and amino acid biosynthesis. Notably, reduced levels of Glu-CDCA and cholic acid 3,7-diacetate suggested disruptions in bile acid transformation. Additionally, alterations in dehydroepiandrosterone (DHEA) derivatives and tryptophan-related metabolites indicated potential dysregulation of hormonal and neurotransmitter pathways.<b>Conclusion:</b> Fecal metabolomic profiling highlights distinct metabolic perturbations in women with PCOS, particularly involving bile acids, steroids, and amino acids. These findings provide insights into gut-associated metabolic disruptions in PCOS and suggest potential pathways for targeted therapeutic interventions.<b>Keywords:</b> Polycystic Ovary Syndrome, Fecal metabolome, Untargeted metabolomics, Bile acids metabolism, Steroids hormones, Gut microbiota.
DOI: 10.5281/zenodo.15309934
title: Table 2 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 2. Conch ontogeny of Goniatites amarensis sp. nov. from Sidi Amar.
dmconch shapewhorl cross section shapewhorl expansion2 mmspindle-shaped; subinvolute (ww/dm ~ 1.25; uw/dm ~ 0.25)extremely depressed; very strongly embracing (ww/wh 3.00; IZR ~ 0.50)low (WER = 1.55)8 mmthickly globular; subinvolute (ww/dm ~ 1.00; uw/dm ~ 0.20)strongly depressed; extremely embracing (ww/wh ~ 2.25; IZR ~ 0.60)very low (WER ~ 1.48)20 mmthinly globular; subinvolute (ww/dm ~ 0.88; uw/dm ~ 0.20)moderately depressed; extremely embracing (ww/wh ~ 1.80; IZR ~ 0.60)low (WER ~ 1.50)50 mmthinly pachyconic; involute (ww/dm ~ 0.65; uw/dm ~ 0.14)weakly depressed; very strongly embracing (ww/wh ~ 1.30; IZR ~ 0.50)moderately high (WER ~ 1.85)
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 59 in European Journal of Taxonomy 989 on page 59, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309936
title: Table 3 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 3. Conch dimensions and ratios of selected specimens of Goniatites sphaericus (Sowerby, 1814) from sample 3 of Sidi Lamine.
dmwwwhuwahww/dmww/whuw/dmWERIZRMB.C.32207.268.846.032.313.1–0.671.420.19––MB.C.32205.158.235.027.68.911.10.601.270.151.530.60MB.C.32207.450.632.023.58.89.40.631.360.171.510.60MB.C.32206.250.333.625.77.69.90.671.310.151.550.61MB.C.32207.147.630.121.67.49.10.631.390.161.530.58MB.C.32205.243.827.220.47.68.50.621.330.171.540.58MB.C.32206.142.633.320.17.98.70.781.660.191.580.57MB.C.32206.338.527.418.86.07.20.711.460.161.510.62MB.C.32207.336.128.417.05.86.60.791.670.161.500.61MB.C.32204.234.826.516.07.2–0.761.660.21––MB.C.32206.433.322.216.44.7–0.671.350.14––
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 62 in European Journal of Taxonomy 989 on page 62, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309938
title: Table 4 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 4. Conch dimensions and ratios of selected specimens of Goniatites sphaericus (Sowerby, 1814) from Dechra Aït Abdallah.
dmwwwhuwahww/dmww/whuw/dmWERIZRMB.C.32213.152.734.025.38.411.40.651.340.161.630.55MB.C.32214.145.828.421.56.49.60.621.320.141.600.55MB.C.32215.136.925.817.74.77.30.701.460.131.550.59MB.C.32214.236.028.416.65.27.00.791.710.141.540.58MB.C.32213.232.624.516.54.66.30.751.480.141.540.62
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 64 in European Journal of Taxonomy 989 on page 64, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309940
title: Table 5 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 5. Conch ontogeny of Goniatites sphaericus (Sowerby, 1814) from Sidi Lamine.
dmconch shapewhorl cross section shapewhorl expansion2 mmspindle-shaped; subinvolute (ww/dm ~ 1.10; uw/dm ~ 0.20)strongly depressed; very strongly embracing (ww/wh ~ 2.30; IZR ~ 0.55)low to mod. high (WER = 1.60–1.80)8 mmthickly globular to spindle-shaped; involute (ww/dm = 0.95– 1.10; uw/dm = 0.05)moderately to strongly depressed; extremely embracing (ww/wh = 1.80–2.20; IZR ~ 0.60)low (WER = 1.50–1.60)20 mmthickly pachyconic to thinly globular; involute (ww/dm = 0.80–0.95; uw/dm ~ 0.10)moderately depressed; extremely embracing (ww/wh ~ 1.90; IZR ~ 0.60)low (WER ~ 1.50)40 mmpachyconic; involute (ww/dm = 0.65–0.80; uw/dm ~ 0.15)moderately depressed; extremely embracing (ww/wh ~ 1.55; IZR ~ 0.60)low (WER ~ 1.50)
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 65 in European Journal of Taxonomy 989 on page 65, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309942
title: Table 6 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 6. Conch dimensions and ratios of a selected specimen of Goniatites spirifer Roemer, 1850 from the Oujda-Berguent road.
dmwwwhuwahww/dmww/whuw/dmWERIZRMB.C.32220.146.732.222.65.88.10.691.420.121.460.64
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 67 in European Journal of Taxonomy 989 on page 67, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309953
title: Table 11 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 11. Conch ontogeny of Hibernicoceras mediocre Moore & Hodson, 1958 from Sidi Amar (Moroccan Meseta).
dmconch shapewhorl cross section shapewhorl expansion2 mmthickly pachyconic; evolute (ww/dm ~ 0.75; uw/dm ~ 0.45)very strongly depressed; widely embracing (ww/wh ~ 2.70; IZR ~ 0.32)low (WER ~ 1.60)8 mmthickly pachyconic; subinvolute (ww/dm ~ 0.80; uw/dm = 0.20)moderately depressed; extremely embracing (ww/wh ~ 1.70; IZR ~ 0.50)low (WER ~ 1.65)20 mmthickly pachyconic; involute (ww/dm ~ 0.75; uw/dm = 0.12)moderately depressed; extremely embracing (ww/wh ~ 1.60; IZR ~ 0.55)low (WER ~ 1.65)
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 75 in European Journal of Taxonomy 989 on page 75, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15309955
title: Table 12 in Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta

description: Table 12. Conch dimensions and ratios of selected specimens of Girtyoceras ibergense Korn, 1992 from the Iberg in the Harz Mountains and from sample 3 of Sidi Lamine.
dmwwwhuwahww/dmww/whuw/dmWERIZRGPIC C42034.411.619.03.712.70.340.610.112.510.33SMF-Mbg.472616.57.58.42.1–0.450.890.13––MB.C.32210.115.97.48.52.44.60.470.870.151.980.46MB.C.32210.28.24.72.92.91.80.571.620.351.640.38
description: Published as part of Korn, Dieter & Ebbighausen, Volker, 2025, Late Viséan (Mississippian) ammonoids (Cephalopoda) from the Central Moroccan Meseta, pp. 77 in European Journal of Taxonomy 989 on page 77, DOI: 10.5852/ejt.2025.989.2885, http://zenodo.org/record/15298185
DOI: 10.5281/zenodo.15310523
title: TABLE 1 in Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal

description: TABLE 1 | Geographical distribution, morphology and special features of the studied Tamarix speciesa, arranged from the East to the West of their distribution areas.
Tamarix speciesDistributionTypical habitatGrowth formHeight (m)Leaf longevitySpecial featuresT. ramosissimaNorth Korea, China, Russia, Mongolia, Tibet, Central Asia, Afghanistan, Iran, Iraq, Ukraine, Eastern TurkeySalty shores of lakes and marshes, salty riverbanks, salty steppes, desertShrub, shrubby tree1–5 (6)DeciduousPhreatophyte, formation of cone-shaped sand dunes (nebkas)T.hispidaRussia, N China, Mongolia, Central Asia, Afghanistan, IranSandy hills, flats and marshes, salty banks of rivers, sand dunes in desertsShrub or small tree1.5–4 (6)DeciduousPhreatophyte, extreme halophyteT. aphyllaW Asia (to NW India, Pakistan, Afghanistan), Middle East, N Africa (to Eritrea, Somalia, Kenya, Ethiopia)Sandy soil and dunes, banks of canals and rivers, salty desertsShrub or treeUp to 12 (20)DeciduousPhreatophyte, tallest Tamarix species, sheathing leavesT. niloticaIsrael, Palestine, Lebanon, NE Africa to Kenya, Ethiopia and SomaliaOn saline sandy soils at river and canal banks, pond edges, springs, rim of wadis, dry lowlandsShrub or tree2–5EvergreenVery drought-hardy, highly salt tolerantT. negevensisIsrael, PalestineSaline shores and other salty sites, maquis, desertSmall treeUp to 2–4EvergreenThermophilous halophyteT. boveanaSpain, Maghreb to W LibyaWadis, riverbanks, borders of swamps, salt marshesLarge shrub or small treeUp to 10Deciduous or marcescentPhreatophyte, hyper-halophilousT. gallicaWestern Mediterranean countries, MaghrebShrubland of wadis and riverbanks, humid places near the seashore, salt marshesShrub or tree2–10Deciduous or marcescentPhreatophyte, climax vegetation on sandy loam, good resprouting under drought
aInformation retrieved from Abd el-Ghani & Amer (2003), Abdelgawad (2017), Baum (1978), Beech (2018), CABI (2022), Castroviejo et al. (1995), Danin and Fragman-Sapir (2016), Encyclopedia of Life (EOL) (2008), Flora of China
(FOC) (2024), Ighbareyeh, Cano-Ortiz, and Cano (2021, 2022), Iqbal et al. (2024), Lavaine, Evette, and Piégay (2015), Molina et al. (2004), The World Flora Online (WFO) (2024); Villar et al. (2012, 2019), Zohary (1982, 1987).
description: Published as part of Akhmedov, Akbar, Bobokandov, Nodirjon, Krehenwinkel, Henrik, Rzepecki, Andreas, Klein, Tamir, Villar, Jose L. & Thomas, Frank M., 2025, Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal, pp. 4 in Journal of Biogeography (e 15096) 52 (5) on page 4, DOI: 10.1111/jbi.15096, http://zenodo.org/record/15304522
DOI: 10.5281/zenodo.15310525
title: TABLE 2 in Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal

description: TABLE 2 | Tamarix species studied, sampling sites and number of samples, arranged from the East to the West of their distribution.
Tamarix speciesState, regionLocationSite conditionElevation (m a.s.l.)Precipitation of the driest quarter (mm; months)Number of plants sampled; sampling timeT. ramosissimaChina, XinjiangN 37°01′, E 080°48′Uniform silty soil, GW contact13656.1; OND6; August 2003T.hispidaUzbekistan, NavoiyN 40°17.700′, E 065°24.711′Sandy soil4452.4; JAS3; June 2022Uzbekistan, Kyzyl-KumN 39°37.408′, E 063°47.785′Sandy soil, influenced by salt1991.1; JAS3; June 2022Uzbekistan, SamarkandN 39°40.058′, E 067°5.682′Sandy meadow-grey soila7197.5; JAS3; August 2022T. aphyllaIsrael, AravaN 30°36.64′, E 035°11.37′Reg soil, coarse desert alluvium;−360.0; JASb1; July 2022N 30°36.61′, E 035°11.84′influenced by drought and salt−220.0; JASb1; July 2022T.niloticaIsrael, AravaN 30°36.64′, E 035°11.37′Reg soil, coarse desert alluvium; influenced by drought and salt−330.0: JASb3; July 2022T. negevensisIsrael, AravaN 30°44.15′, E 035°16.73′Site influenced by drought and salt−1280.0; JASb4; July 2022T. boveanaSpain, MurciaN 38°16′, W 000°59′Dry riverbed, influenced by salt; GW contactca. 36024; JJA3; March 2007T.gallicaSpain, AndalusiaN 37°02′, W 002°26′Clayey marl soil, GW contactca. 35023; JJA5; March 2007
Abbreviation: GW, groundwater.
aKenjaev and Tursunkulova (2021).
bShared values of the Israeli sites due to their proximity.
description: Published as part of Akhmedov, Akbar, Bobokandov, Nodirjon, Krehenwinkel, Henrik, Rzepecki, Andreas, Klein, Tamir, Villar, Jose L. & Thomas, Frank M., 2025, Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal, pp. 5 in Journal of Biogeography (e 15096) 52 (5) on page 5, DOI: 10.1111/jbi.15096, http://zenodo.org/record/15304522
DOI: 10.5281/zenodo.15310526
title: TABLE 2 in Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal

description: TABLE 2 | Tamarix species studied, sampling sites and number of samples, arranged from the East to the West of their distribution.
Tamarix speciesState, regionLocationSite conditionElevation (m a.s.l.)Precipitation of the driest quarter (mm; months)Number of plants sampled; sampling timeT. ramosissimaChina, XinjiangN 37°01′, E 080°48′Uniform silty soil, GW contact13656.1; OND6; August 2003T.hispidaUzbekistan, NavoiyN 40°17.700′, E 065°24.711′Sandy soil4452.4; JAS3; June 2022Uzbekistan, Kyzyl-KumN 39°37.408′, E 063°47.785′Sandy soil, influenced by salt1991.1; JAS3; June 2022Uzbekistan, SamarkandN 39°40.058′, E 067°5.682′Sandy meadow-grey soila7197.5; JAS3; August 2022T. aphyllaIsrael, AravaN 30°36.64′, E 035°11.37′Reg soil, coarse desert alluvium;−360.0; JASb1; July 2022N 30°36.61′, E 035°11.84′influenced by drought and salt−220.0; JASb1; July 2022T.niloticaIsrael, AravaN 30°36.64′, E 035°11.37′Reg soil, coarse desert alluvium; influenced by drought and salt−330.0: JASb3; July 2022T. negevensisIsrael, AravaN 30°44.15′, E 035°16.73′Site influenced by drought and salt−1280.0; JASb4; July 2022T. boveanaSpain, MurciaN 38°16′, W 000°59′Dry riverbed, influenced by salt; GW contactca. 36024; JJA3; March 2007T.gallicaSpain, AndalusiaN 37°02′, W 002°26′Clayey marl soil, GW contactca. 35023; JJA5; March 2007
Abbreviation: GW, groundwater.
aKenjaev and Tursunkulova (2021).
bShared values of the Israeli sites due to their proximity.
description: Published as part of Akhmedov, Akbar, Bobokandov, Nodirjon, Krehenwinkel, Henrik, Rzepecki, Andreas, Klein, Tamir, Villar, Jose L. & Thomas, Frank M., 2025, Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal, pp. 5 in Journal of Biogeography (e 15096) 52 (5) on page 5, DOI: 10.1111/jbi.15096, http://zenodo.org/record/15304522
DOI: 10.5281/zenodo.15310527
title: TABLE 3 in Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal

description: TABLE 3 | Wood anatomical and hydraulic traits of Tamarix species along a geographical gradient from NW China to SW Spain (cf. Table 2).
Tamarix speciesTrait (statistical test)T. ramosissimaT. hispidaT. aphyllaT. negevensisT. niloticaT. boveanaT. gallica(Partial) η 2Statistical powerPercentage conduit area (KW)15.0 ± 1.2 a12.0 ± 0.6 ab10.5± 2.0 abc14.9 ± 2.3 a15.0 ± 1.8 a7.9 ± 0.4 c9.2± 0.4 bc0.4630.953Conduit density (KW)72.4 ± 7.3 abc57.9± 4.2 bcd42.1± 0.3 cd55.7 ± 5.4 bcd37.3 ± 4.9 d175.6± 69.5 ab324.8 ± 60.6 a0.690>0.999Mean conduit area (µm2) (GLM)2093± 63 b2306± 236 b2666± 370 ab2933± 366 ab4045± 115 a694± 173 c405± 43 c0.866>0.999Maximum conduit area (µm2) (KW)8938 ± 344 a7806± 644 a5572 ± 623 ab8725± 683 a8929 ± 127 a4341 ± 551 b3950 ± 622 b0.5460.996Mean conduit diameter (µm) (GLM)45.6 ± 0.8 bc50.3 ± 2.9 b58.8 ± 4.5 ab59.3± 4.0 ab70.9 ± 1.4 a23.7± 4.2 c17.6 ± 1.2 c0.912>0.999Maximum conduit diameter (µm) (GLM)107.7± 2.1 a101.1± 3.9 ab86.6± 5.2 bc108.7± 4.9 a110.0 ± 1.3 a74.1 ± 4.7 c70.4 ± 5.5 c0.780>0.999k (kg MPa−1 m−1 s−1) (GLM) ttot H2O368 ± 26 a332± 36 ab229 ± 78 abc454 ± 105 a564 ± 82 a100 ± 8 bc89 ± 10 c0.710>0.999k (kg MPa−1 m−1 s−1) (GLM) tcond H2O2457 ± 55 b2588 ± 169 ab2154 ± 324 bc2850 ± 302 ab3427 ± 78 a1180 ± 64 cd966± 112 d0.853>0.999d h (µm) (GLM)76.7± 0.9 a75.2 ± 2.5 a66.1 ± 4.8 ab77.7± 4.0 a83.7± 1.3 a52.4 ± 2.6 b49.5 ± 3.1 b0.845> 0.999Wood density (g cm−3) (GLM)0.80 ± 0.03 a0.62± 0.02 b0.91 ± 0.03 a0.87± 0.03 a0.81± 0.01 a0.98a0.91± 0.04 a0.877> 0.999P 50 (MPa) (KW)−9.74± 2.57 c−2.37± 0.18 a−2.64 ± 0.02 ab−3.05 ± 0.34 ab−3.39± 0.82 ab−7.17 ± 1.23 c−5.45 ± 0.21 bc0.7200.967
Note: k ttot, hydraulic conductivity related to unit cross section of the shoot; k tcond, hydraulic conductivity related to the sum of conduit areas in that cross section; d h, hydraulic diameter of the conduits; P 50, xylem water potential causing 50% loss of hydraulic conductivity by embolism. Species with the same lower-case letter do not differ significantly in a given trait (GLM univariate ANOVAs with post hoc Sidak test, if no deviation from homogeneity
of variances [Levene test] or from homoscedasticity; and Kruskal–Wallis [KW] tests in cases of significant deviations from homogeneity of variances or from homoscedasticity); p <0.05. Means ±1 SE.(Partial) η 2, effect sizes of (ANOVA or) KW tests.
aOnly one value for this species.
description: Published as part of Akhmedov, Akbar, Bobokandov, Nodirjon, Krehenwinkel, Henrik, Rzepecki, Andreas, Klein, Tamir, Villar, Jose L. & Thomas, Frank M., 2025, Wood Anatomical and Hydraulic Traits of Tamarix Species Across a Large Eurasian Gradient Show a Stronger Climatic Than Phylogenetic Signal, pp. 9 in Journal of Biogeography (e 15096) 52 (5) on page 9, DOI: 10.1111/jbi.15096, http://zenodo.org/record/15304522