cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/cc8cxm4
title: CCDC 249786: Experimental Crystal Structure Determination

description: Related Article: A.Nakamura, T.Sato, R.Kuroda|2004|Chem.Commun.||2858|doi:10.1039/b409006c
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/rn43-ns25
title: NOAA/WDS Paleoclimatology - B7 Cave Geochemical Data from 17600 to -47 Cal Yr BP

description: Petrographical and geochemical parameters of stalagmites from the B7 cave in Iserlohn–Letmathe (Northern Rhenish Massif, NW Germany) record Late- and postglacial climate changes (temperature and/or precipitation). Fabrics and microfacies of the stalagmite profiles lead to a differentiation of four hierarchies of rhythms. Clastic layers in the stalagmites are caused by flooding events and are time markers. Twenty-four TIMS Th/U-age-dates provide a time calibration of stalagmite growth phases. One stalagmite reveals an early growth period between 17.6 and 16.7 ka BP. Between 9.6 and 5.5 ka BP (Atlantic episode of the Holocene) the growth rate of the stalagmites was higher than before and after this time, with dominant light-porous microfacial laminae and high δ18O and δ13C values representing partly kinetic fractionation effects. This part of the Holocene is interpreted as a mainly warm episode with frequent interruptions of dripping. Within the past 4 ka the profiles with predominant dark compact facies reveal low isotopic values which may be interpreted as a temperature proxy record. The stalagmite records resemble records from an Irish stalagmite. Correlation with the Δ14C record from European tree rings suggests that colder periods in the North Atlantic were accompanied by drier winters in central Europe.
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: STAL-B7-7 (SISAL entity_id=560) has unclear U isotope notation in the original paper (dU). Because of this, U isotope data is missing in the dating table.
DOI: 10.5517/cc6ljny
title: CCDC 196560: Experimental Crystal Structure Determination

description: Related Article: P.Camps, E.Gomez, D.Munoz-Torrero, M.Font-Bardia, X.Solans|2003|Tetrahedron|59|4143|doi:10.1016/S0040-4020(03)00577-5
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/reck-7h38
title: NOAA/WDS Paleoclimatology - Esper - Laubach, Hunsrück EDL05 - PCAB - ITRDB DEU437

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: 10.5517/cc8q7qx
title: CCDC 259709: Experimental Crystal Structure Determination

description: Related Article: M.Amat, M.Perez, N.Llor, C.Escolano, F.J.Luque, E.Molins, J.Bosch|2004|J.Org.Chem.|69|8681|doi:10.1021/jo0487101
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/rd1c-y670
title: NOAA/WDS Paleoclimatology - Alboran Sea Geochemistry, Stable Isotope and Water Temperature Reconstruction Data since the Last Deglaciation

description: Cold-water coral (CWC) mounds are commonly found in the Alboran Sea (westernmost Mediterranean), specifically in the so-called East and West Melilla mound provinces. This study presents a multi-proxy analysis on the environmental changes that occurred in west Melilla since the last deglaciation (~14 kyr), based on the on-mound core MD13–3451 (~370 m). The analyses performed include geochemical measurements of foraminiferal coatings (U/Mn) and skeletal calcite (stable oxygen and carbon isotopes, Mg/Ca-derived deep-water temperatures). Furthermore, the seawater δ18O (δ18Osw) and the ice-volume-corrected seawater δ18O (δ18Osw-ivc) have been estimated via paired analyses of Mg/Ca and δ18Ocarbonate. Our findings suggest that i) pulses of relatively warm deep-water during the last mound flourishing stage, here-referred to as 'Cold Water Coral - Growth Phase 1' (CWC-GP1; ~11–9 kyr), triggered a shift in coral species dominance in the west Melilla province, and ii) a rapid freshening of the waters occurred during CWC-GP1, indicating significant hydrographical changes. To further interpret these results, we combined them with comparable records from neighboring sites. We find that CWC-GP1 is closely coupled with a reorganization of the Alboran Sea water column. More precisely, we discuss the potential emergence of a western Mediterranean intermediate sourced water, which partly replaced intermediate waters from eastern Mediterranean sources and contributed to the enhanced hydrodynamics of the region. We further propose that the interplay between strong near-bottom currents and increased upwelling conditions may have played a crucial role in controlling CWC growth dynamics.
description: New data of deep water temperature (DWT) based on Mg/Ca ratios and oxygen stable isotopes records (d18O). Using the temperatures and the oxygen isotopes we estimate variations in the salinity of the deep waters.
     Provided Keywords:  Sapropel, Mediterranean circulation, foraminifera
DOI: 10.5517/cc5wlyk
title: CCDC 175489: Experimental Crystal Structure Determination

description: Related Article: L.J.Barbour, M.R.Caira, T.le Roex, L.R.Nassimbeni|2002|J.Chem.Soc.,Perkin Trans.2||1973|doi:10.1039/b110987c
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: 10.5517/cc5wlzl
title: CCDC 175490: Experimental Crystal Structure Determination

description: Related Article: L.J.Barbour, M.R.Caira, T.le Roex, L.R.Nassimbeni|2002|J.Chem.Soc.,Perkin Trans.2||1973|doi:10.1039/b110987c
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: 10.5517/cc7vzrs
title: CCDC 234476: Experimental Crystal Structure Determination

description: Related Article: I.Hung, C.L.B.Macdonald, R.W.Schurko|2004|Chem.-Eur.J.|10|5923|doi:10.1002/chem.200400404
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/r1f2-dj87
title: NOAA/WDS Paleoclimatology - Esper - Pitkäjärvi Lake HLP01 - PISY - ITRDB FIN102

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: wet N-Exp.
DOI: 10.5517/cc7vzst
title: CCDC 234477: Experimental Crystal Structure Determination

description: Related Article: I.Hung, C.L.B.Macdonald, R.W.Schurko|2004|Chem.-Eur.J.|10|5923|doi:10.1002/chem.200400404
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/r9a9-xr89
title: NOAA/WDS Paleoclimatology - Esper - Mount Smolikas EHS10 - PIHE - ITRDB GRC037

description: We present the longest high-elevation tree-ring width dataset in the Mediterranean reaching back to the 6th century CE. The network includes 101 living and 92 relict Pinus heldreichii Christ trees from four differently exposed sites in the 2100-2200 m a.s.l. elevation range of Mt. Smolikas in the Pindus Mountains in Greece. Though the sites were all sampled within a distance of <1 km, inter-site correlations are surprisingly low (r1550-2014 = 0.65-0.87), indicating site exposure might affect tree-ring formation. We here explore the consequence of exposure differences on the climate signals in an eastern Mediterranean treeline ecotone. Temporally stable growth/climate relationships reveal similar seasonal patterns among the four sites, but differences in signal strength. P. heldreichii growth at Mt. Smolikas is significantly controlled by temperature in April (r1951-2014 = 0.33-0.50) and precipitation in June-July (r1951-2014 = 0.23-0.42), which emphasizes the overall importance of an early growth onset and subsequent moisture conditions. The association between stem growth and April climate is strongest in the South-facing stand, supporting the significance of higher insolation rates at this thermally privileged site. Strongest summer precipitation signals are found in the NE-facing stand, where trees seem to benefit least from an early growth onset and where reduced meltwater supply may enhance the dependency on early summer precipitation. The significance of spring temperature on tree growth in all four sites constrains the emergence of a distinct summer precipitation signal in the Mt. Smolikas high elevation ecotone. Exploration of the site-specific influences on a new millennium-long tree-ring width dataset is an important step towards an improved understanding of long-term climate variability in the Eastern Mediterranean. Site-related differences in climate sensitivity in the high-elevation tree-ring network at Mt. Smolikas indicate that both temperature and precipitation during different seasons could potentially be reconstructed if distinct site exposures (S versus NE) are considered.
DOI: 10.5517/cc7vg5p
title: CCDC 233962: Experimental Crystal Structure Determination

description: Related Article: M.R.Caira, T.Le Roex, L.R.Nassimbeni|2004|Supramol.Chem.|16|595|doi:10.1080/10610270412331317549
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/rnvg-7968
title: NOAA/WDS Paleoclimatology - Nova Grgosova cave Geochemical Data from 10000 to -52 Cal Yr BP

description: We present the first stable isotope (δ13C and δ18O) speleothem record from continental Croatia retrieved from two coeval stalagmites from Nova Grgosova Cave. U-Th dates constrain the stalagmite growth history from 10 ka to the present, revealing coeval growth between 7.8 and 5.6 ka. We interpret δ18O as an autumn/winter hydrological proxy related to changes of vapor source, precipitation amount, and/or seasonal rainfall distribution, while δ13C predominantly responds to spring/summer vegetation status and soil microbial activity. We identify several centennial to millennial-scale hydroclimate oscillations during this period that result from multiple forcing factors. Along with amount and source effect, it appears that some centennial variations were governed also by seasonal moisture balance. From 9.2 to 8.8 ka BP, the local environmental setting was characterized by enhanced vegetation activity, while during the 8.2 ka event the main feature was a change in precipitation seasonality. The most prominent change, identified in both δ13C records, is a sudden decline of vegetation and soil biological activity around 7.4 ka, indicating a precipitation decrease at a time of maximum plant growth in spring and summer and likely also reduced precipitation in autumn and winter. Although small in magnitude in these speleothems, a peak in δ18O and δ13C values at 4.3–4.1 ka suggests that both summer and winter conditions were substantially drier during the 4.2 ka event, in accordance with increased Mediterranean aridity and consistent with other global climate changes reported at this time. Compared to the present North Atlantic Oscillation (NAO) influence, we assume that millennial Holocene NAO-like variations were persistent through the Holocene via their effect on modifying local/regional air temperature, vapor origin, and inter- and intrannual precipitation distribution. Anthropogenic deforestation, which was the first major human impact on the environment during the Neolithic agricultural revolution, is excluded as a leading factor in δ13C variability since the first sedentary settlements were established further to the east in more arable locations along river valleys. However, the impact of intensive mining around the cave site during the last millennium is evident, with substantial deforestation driving an increase in δ13C.
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: Mixed deciduous and evergreen. \\ NG-3 (SISAL entity_id = 831): Dating table differs from the published. In the paper the top (Event; actively forming) is marked at 0.5 mm with a corrected age of 5 years. In this dataset it has been changed to 0 mm without any given corresponding corrected age.
DOI: 10.5517/cc7vg6q
title: CCDC 233963: Experimental Crystal Structure Determination

description: Related Article: M.R.Caira, T.Le Roex, L.R.Nassimbeni|2004|Supramol.Chem.|16|595|doi:10.1080/10610270412331317549
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/r898-8k15
title: NOAA/WDS Paleoclimatology - Crevice Cave Geochemical Data from 90500 to 53100 Cal Yr BP

description: Coastal South Africa draws interdisciplinary interests due to the co-occurrence of a rich record for early human behavioral modernity, hyper-diverse vegetation with very high endemism (the Cape Floral Region), and globally influential oceanic and climate systems. High resolution and continuous climate and environmental records are needed to provide the context for the evolution of behavioral modernity and this diverse flora. Here we present the first such record for climate and environmental change from 90 000 to 53 000 years ago from the southern Cape coast. This important time span covers a burst of expression of several indicators of human behavioral modernity, as well as several key cycles in global climate change. Our research location is ideally placed near the location of several critical archaeological sites, near the boundary of the winter and summer rainfall regimes, and close to isotopically distinct floral zones. We used isotopic analysis of precisely dated speleothems to document shifting vegetation and rainfall, and show that the presence of winter rain and C3 grasses waxes and wanes in response to Southern Hemisphere shifts in SSTs and global temperature. When proxies of global temperatures indicate warmer conditions, δ18O and δ13C indicate more winter rain and more C3 grasses, respectively, and vice versa. This record displays abrupt and short-term changes previously undocumented. It is often argued that the Cape Floral Region partially owes its high diversity to relative climatic stability. Our record shows isotopic variability that at least matches that displayed in the Levantine Mediterranean system, so climatic stability may not have characterized the south coast. One short-lived phase of human technological innovation (the Still Bay) associated with early evidence for behavioral modernity occurs synchronous with an abrupt environmental perturbation. Early modern humans in this region confronted a variable climate and adapted quickly in a manner similar to behaviorally modern humans.
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: The host rock of the site is a Palaeozoic quartzite, the source of the carbonate to form speleothems are overlying aeolianites of Pleistocene age. Current land_use above the cave is a mix of a golf course, shrubland and built-up structures. \\ Entity Crevice_composite (SISAL entity_id = 745) is a composite record of the entities 32206, 46623, 46624, 46856-1C2, 46857-SA3, 46859-SA4, 50103, 110620 (age models for individual samples no longer avaialable). The composite records was constructed by choosing the samples with the highest resolution and good overlap with the stable isotope records of other samples
DOI: 10.5517/cc7vg8s
title: CCDC 233965: Experimental Crystal Structure Determination

description: Related Article: M.R.Caira, T.Le Roex, L.R.Nassimbeni|2004|Supramol.Chem.|16|595|doi:10.1080/10610270412331317549
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: 10.5517/cc7xkrf
title: CCDC 235995: Experimental Crystal Structure Determination

description: Related Article: S.K.Bagal, R.M.Adlington, J.E.Baldwin, R.Marquez|2004|J.Org.Chem.|69|9100|doi:10.1021/jo0488053
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: 10.5517/cc8jxh5
title: CCDC 254587: Experimental Crystal Structure Determination

description: Related Article: S.K.Bagal, R.M.Adlington, J.E.Baldwin, R.Marquez|2004|J.Org.Chem.|69|9100|doi:10.1021/jo0488053
description: Related Article: S.K.Bagal, R.M.Adlington, R.A.B.Brown, J.E.Baldwin|2005|Tetrahedron Lett.|46|4633|doi:10.1016/j.tetlet.2005.04.125
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: 10.3535/5z5-sqg-s5g
title: Arremon aurantiirostris spectabilis

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/k44-5mr-114
title: Atlapetes latinuchus spodionotus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/52y-5rg-en6
title: Larus canus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/6fc-5s3-zyd
title: Morus capensis

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/snc-y61-qs8
title: Euphonia elegantissima

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/33d-gmj-tpr
title: Calidris pugnax

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/ckt-ct4-71h
title: Turdus merula

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/d3d-9fg-23y
title: Contopus cinereus pallescens

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/gp0-pyp-t94
title: Sterna paradisaea

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/mna-egl-tl8
title: Somateria mollissima

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/8tr-kcw-1nk
title: Fringilla coelebs coelebs

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/meh-vv8-z1p
title: Caprimulgus europaeus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/yma-e9l-5tt
title: Buarremon torquatus assimilis

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/0ym-6pw-ehr
title: Passer montanus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/b64-ts5-1ka
title: Chalcomitra amethystina amethystina

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/2z3-l8b-5bk
title: Tringa glareola

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/dx0-y79-kp2
title: Conirostrum cinereum fraseri

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/g8w-d1m-bn0
title: Buteo lagopus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/a2x-sqy-99f
title: Trochilus polytmus

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/cfr-1wx-kml
title: Lonchura nigriceps

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/lxn-gc7-hys
title: Sturnus vulgaris

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.
DOI: 10.3535/8bm-yzp-7mf
title: Catamblyrhynchus diadema diadema

description: Digital Specimen for the physical specimen hosted at Natural History Museum of Denmark.