cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/inscriptifact-ouc110853728
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110854966
title: Persepolis Fortification Anepigraphic Tablet 0375.201, PFAnep 0375.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0375.201, PFUT 0375-201 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impression on left edge. ❧ [Physical Object Note:] Large cracks on reverse, upper edge. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110853725
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110854880
title: Persepolis Fortification Anepigraphic Tablet 0375.201, PFAnep 0375.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0375.201, PFUT 0375-201 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impression on left edge. ❧ [Physical Object Note:] Large cracks on reverse, upper edge. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110853613
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110854864
title: Persepolis Fortification Anepigraphic Tablet 0375.201, PFAnep 0375.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0375.201, PFUT 0375-201 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impression on left edge. ❧ [Physical Object Note:] Large cracks on reverse, upper edge. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110853547
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110854860
title: Persepolis Fortification Anepigraphic Tablet 0375.201, PFAnep 0375.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0375.201, PFUT 0375-201 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impression on left edge. ❧ [Physical Object Note:] Large cracks on reverse, upper edge. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110853546
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110859187
title: Persepolis Fortification Anepigraphic Tablet 0381.204, PFAnep 0381.204

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0381.204, PFUT 0381-204 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on bottom edge, left edge, obverse, reverse, upper edge. ❧ [Physical Object Note:] Damage and crack on bottom edge, left edge. Part of obverse damaged. Small break on right edge. Cracks on reverse.
DOI: 10.25549/inscriptifact-ouc110853527
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25549/inscriptifact-ouc110859157
title: Persepolis Fortification Anepigraphic Tablet 0381.204, PFAnep 0381.204

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0381.204, PFUT 0381-204 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on bottom edge, left edge, obverse, reverse, upper edge. ❧ [Physical Object Note:] Damage and crack on bottom edge, left edge. Part of obverse damaged. Small break on right edge. Cracks on reverse.
DOI: 10.25549/inscriptifact-ouc110853528
title: Persepolis Fortification Anepigraphic Tablet 0374.206, PFAnep 0374.206

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0374.206, PFUT 0374-206 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Text ❧ [Physical Object Description:] Clay tablet with seal impressions on left edge, obverse, reverse. ❧ [Physical Object Note:] Right and bottom edges broken. Cracks on reverse. (Upper and bottom edges may be reversed)
DOI: 10.25921/83tk-k668
title: NOAA/WDS Paleoclimatology - Tumajer - Mount Babel West - treeline - PCGL - ITRDB CAN693

description: Tree ring data from the International Tree Ring Data Bank and World Data Center for Paleoclimatology archives.  Most data sets include raw treering measurements (most are annual ring width, with some collections of earlywood or latewood width or wood density), plus chronologies (standardized growth indices for a site compiled from multiple treering samples). Reconstructions of climate variables are included with some of these data sets.  Each data type is stored in a separate data file; the data type is coded into the file name. For details please see: http://www.ncdc.noaa.gov/paleo/treeinfo.htmll
description: two cores per tree (last position of series code)
DOI: 10.15468/dl.m9jaz2
title: Occurrence Download

description: A dataset containing 8542 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Castanea pumila"
 ]
}

 The dataset includes 8542 records from 205 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0025158-251009101135966/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25921/81g7-3637
title: NOAA/WDS Paleoclimatology - Touchan - Bölükandiz - CDLI - ITRDB TUR062

description: The first large-scale network of 79 tree-ring chronologies in the Eastern Mediterranean and Near East (EMNE; 33°N–42°N, 21°E–43°E) is described and analyzed to identify the seasonal climatic signal in indices of annual ring width. Correlation analysis and cluster analysis are applied to tree-ring data and gridded climate data to assess the climate signal embedded in the network in preparation for climate field reconstructions and formal proxy/model intercomparison experiments. The lengths of the 79 combined chronologies range from 89 to 990 years. The monthly correlations and partial correlations reveal a pervasive positive association with May, June, and sometimes July precipitation, positive correlations with winter and spring (December through April) temperatures, and negative relationships with May through July temperature, although as expected, there are site-to-site exceptions to these general patterns. Cluster analysis suggests three groups of sites based on their association with climate. The chronologies for the EMNE have coherent seasonal precipitation and temperature signals across a fairly broad geographical domain. The predominant signal is a positive growth response to May–June precipitation. Collectively, the findings suggest that the network can be exploited to develop season-specific field reconstructions of precipitation and drought history in the EMNE.
DOI: 10.25921/84pb-mj28
title: NOAA/WDS Paleoclimatology - Andrus - Barlow Wayside - THPL - ITRDB OR129

description: Aim: Forest dieback is increasing in many forest ecosystems from unfavorable climate conditions. Western redcedar (WRC)–a culturally, ecologically, and economically important species–has recently experienced anomalously high mortality rates and partial canopy dieback. We investigated how WRC tree radial growth and dieback responded to climate variability and drought using tree-ring methods. Location: Pacific Northwest, USA. Taxon: western redcedar (Thuja plicata). Methods: We collected tree cores from three tree health status groups (no canopy dieback, partial canopy dieback, and dead trees) at 11 sites in coastal (maritime climate) and interior (continental climate) WRC populations as well as previously published climate and weather data. From growth rates, we computed four growth indices evaluating the resilience to drought. Results: Warmer and drier climate conditions in May and June that extend the annual July-to-September dry season reduced radial growth in 9 of 11 sites (1975-2020). WRC trees recovered radial growth to pre-drought rates within three years when post-drought climate conditions were average or cooler/wetter than average. However, recovery from drought was slower or absent when conditions were warmer/drier during the post-drought recovery period, which appeared to lead to the widespread mortality event across the coastal populations. WRC tree mortality was portended by 4-5 years of declining radial growth. Annually-resolved tree mortality in coastal populations predominately occurred in 2017-2018 (80% of sampled dead trees) and coincided with exceedingly hot temperatures and the longest regionally dry period from May to September (1970-2020). In interior populations, tree mortality was dispersed among years but associated with warmer and drier conditions from August to September. Main conclusions: Our findings forewarn that a warming climate and more frequent and severe summer droughts, especially in consecutive years, will likely increase the vulnerability of WRC to canopy dieback and mortality and possibly other drought-sensitive trees in one of the world’s largest carbon sinks.
DOI: 10.25921/8kek-3z11
title: NOAA/WDS Paleoclimatology - Andrus - Icicle Creek - THPL - ITRDB WA165

description: Aim: Forest dieback is increasing in many forest ecosystems from unfavorable climate conditions. Western redcedar (WRC)–a culturally, ecologically, and economically important species–has recently experienced anomalously high mortality rates and partial canopy dieback. We investigated how WRC tree radial growth and dieback responded to climate variability and drought using tree-ring methods. Location: Pacific Northwest, USA. Taxon: western redcedar (Thuja plicata). Methods: We collected tree cores from three tree health status groups (no canopy dieback, partial canopy dieback, and dead trees) at 11 sites in coastal (maritime climate) and interior (continental climate) WRC populations as well as previously published climate and weather data. From growth rates, we computed four growth indices evaluating the resilience to drought. Results: Warmer and drier climate conditions in May and June that extend the annual July-to-September dry season reduced radial growth in 9 of 11 sites (1975-2020). WRC trees recovered radial growth to pre-drought rates within three years when post-drought climate conditions were average or cooler/wetter than average. However, recovery from drought was slower or absent when conditions were warmer/drier during the post-drought recovery period, which appeared to lead to the widespread mortality event across the coastal populations. WRC tree mortality was portended by 4-5 years of declining radial growth. Annually-resolved tree mortality in coastal populations predominately occurred in 2017-2018 (80% of sampled dead trees) and coincided with exceedingly hot temperatures and the longest regionally dry period from May to September (1970-2020). In interior populations, tree mortality was dispersed among years but associated with warmer and drier conditions from August to September. Main conclusions: Our findings forewarn that a warming climate and more frequent and severe summer droughts, especially in consecutive years, will likely increase the vulnerability of WRC to canopy dieback and mortality and possibly other drought-sensitive trees in one of the world’s largest carbon sinks.
DOI: 10.25921/8mny-xs88
title: NOAA/WDS Paleoclimatology - Madagascar Speleothem Stable Isotope Data from 13200-11280 year BP

description: As prominent abrupt climatic events during the last deglaciation and the early Holocene, the Younger Dryas (YD) and the 8.2 ka events have been intensely discussed to reveal the relationship between their phases and intensities, and their underlying mechanisms based on massive marine and terrestrial archives. However, the related paleoclimate records with sufficient resolution and/or precise age constraints from the Southern Hemisphere, especially East Africa, are relatively sparse, hindering our comprehensive understanding about the phases of these two events. Here, we provide a precisely dated record of an aragonite-calcite stalagmite covering 11.3–13.5 ka BP from northwest Madagascar to unravel the arid conditions during the YD, in contrast to the pluvial conditions in the 8.2 ka event that has been evidenced before. Changes in austral summer precipitation related to the Intertropical Convergence Zone (ITCZ) have always been interpreted to be the primary means of controlling regional rainfall amounts and thus the d18O variations in stalagmite. However, ITCZ’s meridional migration alone is not enough to interpret the opposite hydroclimatic conditions during the YD and the 8.2 ka events in northwest Madagascar. The variation in convection intensity within the ITCZ combined with the rainfall dipole mode in East Africa, and the redistribution of the duration of the ITCZ’s presence at different latitudes might be responsible for this phenomenon. In addition, sea surface temperature could play a nonnegligible role.
description: Provided Keywords: speleothem, the Younger Dryas event, precipitation, Northwest Madagascar
DOI: 10.13140/rg.2.2.19075.50720
title: 2.8 Deacon
DOI: 10.13140/rg.2.2.21067.80165
title: A simple, easy-to-use spreadsheet for automatic scoring of the International Physical Activity Questionnaire (IPAQ) Short Form
DOI: 10.13140/rg.2.2.25786.39367
title: 2.7 Comber
DOI: 10.25921/8q4t-z035
title: NOAA/WDS Paleoclimatology - Pacific Ocean Geochemical and Foraminiferal Cleaning Procedure Data at 1Mya, 20Kya and 1999-2009 CE

description: Past ocean conditions are often reconstructed using the elemental composition of foraminiferal calcite. However, foraminiferal remains are often impacted by post-depositional contaminants; thus, they require cleaning prior to element/Ca (El/Ca) analysis. To explore the impact of sample pretreatment on foraminiferal El/Ca ratios (Li, Na, Mg, Al, Mn, Fe, Zn, Sr, I, Ba, and U) we performed six cleaning procedures on four foraminifera populations from distinct depositional environments: Two from South Pacific carbonate ooze (ELT25-11) and two from the hemi-pelagic sediments of the California Margin (ODP1017E, SPR0901-04BC). Despite differences in regional oceanography, sample type (i.e., surface- or deep-dwelling planktic, benthic), and cleaning procedure, the main driver of El/Ca variability in the data set is the sedimentary depositional environment, suggesting site-specific differences in element concentrations and contaminants. This finding challenges the notion that sample cleaning procedures should be informed by the El/Ca of paleoclimate interest, as elements may be found in different contaminants and/or elemental abundances in unique environments. Our data also show that traditional cleaning methods which use a combination of rinsing, sonication, oxidation/reduction, and complexation reactions effectively remove contaminants found on foraminifera in either depositional environment. However, even after contaminant removal, some elements (i.e., U and Fe) remain higher in California Margin foraminifera relative to South Pacific foraminifera. This suggests that the range of acceptable El/Ca values in the literature must be expanded when working with foraminifera from unusual depositional environments (i.e., hemipelagic, siliciclastic sites with high sedimentation regimes) versus values associated with more typical sites (i.e., a pelagic carbonate ooze).
DOI: 10.25921/8pza-rv38
title: NOAA/WDS Paleoclimatology - Klesse - 3M Lugnez - FASY - ITRDB CHE431

description: Ongoing climate warming is increasing evapotranspiration, a process that reduces plant-available water and aggravates the impact of extreme droughts during the growing season. Such an exceptional hot drought occurred in Central Europe in 2018 and caused widespread defoliation in mid-summer in European beech (Fagus sylvatica L.) forests. Here, we recorded crown damage in 2021 in nine mature even-aged beech-dominated stands in northwestern Switzerland along a crown damage severity gradient (low, medium, high) and analyzed tree-ring widths of 21 mature trees per stand. We aimed at identifying predisposing factors responsible for differences in crown damage across and within stands such as tree growth characteristics (average growth rates and year-to-year variability) and site-level variables (mean canopy height, soil properties). We found that stand-level crown damage severity was strongly related to soil water availability, inferred from tree canopy height and plant available soil water storage capacity (AWC). Trees were shorter in drier stands, had higher year-to-year variability in radial growth, and showed higher growth sensitivity to moisture conditions of previous late summer than trees growing on soils with sufficient AWC, indicating that radial growth in these forests is principally limited by soil water availability. Within-stand variation of post-drought crown damage corresponded to growth rate and tree size (diameter at breast height, DBH), i.e., smaller and slower-growing trees that face more competition, were associated with increased crown damage after the 2018 drought. These findings point to tree vigor before the extreme 2018 drought (long-term relative growth rate) as an important driver of damage severity within and across stands. Our results suggest that European beech is less likely to be able to cope with future climate change-induced extreme droughts on shallow soils with limited water retention capacity.