cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/inscriptifact-ouc110859026
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110853520
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-ouc110859024
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110853522
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-ouc110858948
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110853521
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-ouc110853502
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-ouc110858950
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110858942
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110853494
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-ouc110858930
title: Persepolis Fortification Anepigraphic Tablet 0380.201, PFAnep 0380.201

description: [Text Description:] Administrative tablet with seals ❧ [Text or Publication Number Note:] PFAnep 0380.201, PFUT 0380-201 ❧ [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 impressions on obverse, reverse, upper edge. ❧ [Physical Object Note:] Some cracks and gouges on reverse.
DOI: 10.25549/inscriptifact-ouc110854859
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: 10.5517/ccdc.csd.cc2g3sgv
title: CCDC 2267757: Experimental Crystal Structure Determination

description: Related Article: Xiao-Bao Li, Mark E. Light, Ana Arauzo, Elena Bartolomé, José Giner Planas|2025|J.Mater.Chem.C|13|8020|doi:10.1039/D5TC00280J
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.25921/8b9z-f762
title: NOAA/WDS Paleoclimatology - Lake Chacacocha, Peru, Leaf Wax Stable Isotope Data over the last 1800 Years

description: The late Holocene behavior of the South American Summer Monsoon (SASM) has been a focal point of studies of oxygen isotope ratios in Andean speleothems and other archives, as they primarily reflect large-scale atmospheric circulation over the South American lowlands rather than localized precipitation vs. evaporation. Consequently, the local effective moisture history throughout the Andes has remained poorly constrained. Here we present ~1800-year plant wax hydrogen (d2Hwax) and carbon (d13Cwax) isotope records from Lake Chacacocha, southeastern Peru. d2Hwax and d13Cwax from terrestrial upland and wetland vegetation allow large-scale atmospheric conditions and local-scale effective moisture to be evaluated side-by-side. In agreement with d18O-based proxies from the region, Chacacocha d2Hwax shows that the SASM was strengthened during the Little Ice Age (LIA). However, our record shows that the SASM began this intensification around 1250 CE, well before the external radiative forcings of the LIA, suggesting that long-term shifts in SASM behavior can be catalyzed by internal drivers e.g., teleconnections with the tropical Pacific. Independent of SASM dynamics, Chacacocha d13Cwax reveals two pronounced, centennial to multi-centennial arid intervals between ca. 450-900 CE and ca. 1640-1850 CE – the latter co-occurring with peak SASM intensity. LIA aridity aligns with nearby evidence for reduced net ice accumulation and glacial retreat from the LIA maximum extent around this time, implying that despite enhanced monsoon activity regionally, reduced effective moisture locally affected the glacial mass balance in southern Peru. Our results help reconcile conflicting interpretations of the SASM, glacial, and high-alpine environmental histories in the Central Andes over the past 1,800 years.
description: Provided Keywords: Common Era, South American summer monsoon, leaf wax isotopes
DOI: 10.13140/rg.2.2.24095.56483
title: Fig. 4. Immunofluorescence localization of two maize rhabdoviruses in their plant and insect hosts
DOI: 10.25921/81gp-3729
title: NOAA/WDS Paleoclimatology - Lake CF8 Baffin Island Pleistocene Holocene Fatty Acids

description: Records of past climate and environment derived from lake sediment records.  Parameter keywords describe what was measured in this data set.  Additional summary information can be found in the abstracts of papers listed in the data set citations.

description: No age-depth model for these cores, as they extend through and beyond the radiocarbon interval.
DOI: 10.25921/8vvk-rt23
title: NOAA/WDS Paleoclimatology - Pozzo Cucù Cave Geochemical Data from 106000 to 26600 Cal Yr BP

description: The causes of Neanderthal–modern human (MH) turnover are ambiguous. While potential biocultural interactions between the two groups are still little known, it is clear that Neanderthals in southern Europe disappeared about 42 thousand years ago (ka) after cohabitation for ~3,000 years with MH. Among a plethora of hypotheses on Neanderthal extinction, rapid climate changes during the Middle to Upper Palaeolithic transition (MUPT) are regarded as a primary factor. Here we show evidence for stable climatic and environmental conditions during the MUPT in a region (Apulia) where Neanderthals and MH coexisted. We base our findings on a rare glacial stalagmite deposited between ~106 and ~27 ka, providing the first continuous western Mediterranean speleothem palaeoclimate archive for this period. The uninterrupted growth of the stalagmite attests to the constant availability of rainfall and vegetated soils, while its δ13C–δ18O palaeoclimate proxies demonstrate that Apulia was not affected by dramatic climate oscillations during the MUPT. Our results imply that, because climate did not play a key role in the disappearance of Neanderthals in this area, Neanderthal–MH turnover must be approached from a perspective that takes into account climatic and environmental conditions favourable for both species.
description: Data contributed as part of SISAL v3 Global Speleothem Isotope and Trace Element Database (https://doi.org/10.25921/jajq-qg60). Notes from the SISAL database: Land use: Concrete and build up in the vicinity, not directly above the cave. \\ PC (SISAL entity_id = 842): The ages and their 2σ uncertainties were used in StalAge and COPRA to produce the age model. Both algorithms produced a comparable age–depth curve. To minimize intrinsic artefacts produced by the two algorithms, including unrealistic maxima in growth rate and unjustified large uncertainty propagation, the final age model was obtained by linear regression of average age values between StalAge and COPRA models at the same depths.
DOI: 10.25921/8skj-nz62
title: NOAA/WDS Paleoclimatology - Lévesque - Biel - PCAB - ITRDB CHE490

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
DOI: 10.13140/rg.2.2.18485.68321
title: Canadian Society for Vascular Surgery Annual Meeting 2015 Survey
DOI: 10.25921/89by-yh62
title: NOAA/WDS Paleoclimatology - Rohner - Krummenlinden Update - PCAB - ITRDB CHE522

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: unpublished
DOI: 10.13140/rg.2.2.28761.72805
title: 2016 Petroglyph Expedition To The West Indies
DOI: 10.25921/8rb5-xw25
title: NOAA/WDS Paleoclimatology - Santo Tomas Cave, Dos Anas Cave Geochemical Data from 12300 to 61 Cal Yr BP

description: We present a speleothem stable oxygen isotope record for the last 12.5 ka based on two stalagmites from western Cuba. The δ18O signal is interpreted to represent past precipitation variability. Both stalagmites show a pronounced transition from higher δ18O values (indicating drier conditions) to more negative δ18O values (suggesting wetter conditions) between 10 and 6 ka. This transition is also visible in a planktonic δ18O record off Haiti. On orbital timescales, the δ18O value of Caribbean precipitation, thus, strongly resembles the oxygen isotope composition of Caribbean surface water. On millenial timescales, the speleothem δ18O record shows a high correlation to a North Atlantic sea surface temperature (SST) record off West Africa as well as a similarity with the Bond events. Periods of lower North Atlantic SST correspond to less precipitation in the Caribbean and vice versa. The potential teleconnection to the Caribbean may reflect the position of the Intertropical Convergence Zone because a further southward position of the ITCZ leads to reduced precipitation in the northern Caribbean.
description: Data contributed as part of SISAL v3 Global Speleothem Isotope and Trace Element Database (https://doi.org/10.25921/jajq-qg60). Notes from the SISAL database: Vegetation: Trees, palms and ferns. \\ CMa (SISAL entity_id = 609) and CMb (entity_id = 610) are two small side stalagmites of CM (entity_id = 608, 388). Agemodel of CMa (entity_id = 609) tuned to the agemodel of CM_2019 (entity_id = 608) via the best correlation of the oxygen isotope records. The given uncertainties are the maximum uncertainties derived by the initial stalage age model.
DOI: 10.25921/8kak-j776
title: NOAA/WDS Paleoclimatology - Peters - Lotschental S22L - LADE - ITRDB CHE529

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
DOI: 10.25921/8vcw-1914
title: NOAA/WDS Paleoclimatology - Lévesque - Goppenstein - LADE - ITRDB CHE533

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
DOI: 10.25921/8c6p-r497
title: NOAA/WDS Paleoclimatology - Zumbrunn - Scharans Mitte - LADE - ITRDB CHE548

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
DOI: 10.25921/8rvv-2h47
title: NOAA/WDS Paleoclimatology - Neycken - Rootriss - FASY - ITRDB CHE562

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
DOI: 10.25921/8m4b-qb53
title: NOAA/WDS Paleoclimatology - Kailash Cave Geochemical Data from 14800 to 12700 Cal Yr BP

description: Although the Indian monsoon during the last deglaciation has been reconstructed from marine sediments from the Indian Ocean, a detailed high resolution (decadal or less) reconstruction from terrestrial records such as speleothems has been lacking from the core monsoon zone of India. Such reconstructions can help determine whether the monsoon is controlled by insolation alone or also other feedbacks within the Earth system. We present here a new data set of high resolution record based on 1186 measurements of δ18O from a 43-cm long speleothem from the Kailash Cave, Central India that record Indian Summer Monsoon (ISM) rainfall changes encompassing the Bølling-Allerød interstadial (14.8 to 12.6 ka). The growth rates varied from 0.6 to 37.1 mm/year, with the monsoon strength. This is also confirmed by the δ18O record, with a rapid increase in the rainfall during 14.8 to 14.5 ka, stabilizing subsequently, and exhibiting centennial and multi-decadal oscillations. Our results corroborate an earlier observation that although the boundary conditions during the last several millennia and the Bølling-Allerød were very different, multi-decadal and centennial climate dynamics may have been similar. In addition to solar insolation, our results show a relation of ISM shifts to coupled ocean-atmospheric processes. Strong link of Indian Summer Monsoon (ISM) variability to proxy records from the southern hemisphere is also noted in this work.
description: Data contributed as part of SISAL v3 Global Speleothem Isotope and Trace Element Database (https://doi.org/10.25921/jajq-qg60).
DOI: 10.13140/rg.2.2.29777.53600
title: The Importance of Sharing Science: Dr. Nilanjan Dey Speaks on Scholarly Publishing and the Promotion of Knowledge Research
DOI: 10.13140/rg.2.2.25268.65921
title: General Bulletin 16-12-02