cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/cc8r0ll
title: CCDC 260449: Experimental Crystal Structure Determination

description: Related Article: H.Reuter|2004|Z.Kristallogr.-New Cryst.Struct.|219|327|doi:10.1524/ncrs.2004.219.14.347
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/cc86l67
title: CCDC 244658: Experimental Crystal Structure Determination

description: Related Article: J.Clayden, A.Lund, L.Vallverdu, M.Helliwell|2004|Nature (London)|431|966|doi:10.1038/nature02933
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/cc86l78
title: CCDC 244659: Experimental Crystal Structure Determination

description: Related Article: J.Clayden, A.Lund, L.Vallverdu, M.Helliwell|2004|Nature (London)|431|966|doi:10.1038/nature02933
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/pj9t-y769
title: NOAA/WDS Paleoclimatology - Hönisch et al. 2009 Pleistocene ODP 668B Isotope and PCO2 Data

description: The dominant period of Pleistocene glacial cycles changed during the mid-Pleistocene from 40,000 years to 100,000 years, for as yet unknown reasons. Here we present a 2.1-million-year record of sea surface partial pressure of CO2 (Pco2), based on boron isotopes in planktic foraminifer shells, which suggests that the atmospheric partial pressure of CO2 (pco2) was relatively stable before the mid-Pleistocene climate transition. Glacial Pco2 was ~31 microatmospheres higher before the transition (more than 1 million years ago), but interglacial Pco2 was similar to that of late Pleistocene interglacial cycles (<450,000 years ago). These estimates are consistent with a close linkage between atmospheric CO2 concentration and global climate, but the lack of a gradual decrease in interglacial Pco2 does not support the suggestion that a long-term drawdown of atmospheric CO2 was the main cause of the climate transition.
DOI: 10.5517/cc7v035
title: CCDC 233526: Experimental Crystal Structure Determination

description: Related Article: A.K.Miller, D.H.Byun, C.M.Beaudry, D.Trauner|2004|Proc.Nat.Acad.Sci.USA|101|12019|doi:10.1073/pnas.0401787101
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/p6z5-9g74
title: NOAA/WDS Paleoclimatology - Fan - Hengduan Mountains 10GK_P_r - PCLI - ITRDB CHIN037

description: Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period ad 1971-2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years.
description: Purpose of Collection: 
# Climatology - temperature analyses NOAA Template Raw Measurements file added 2019-04-08.
DOI: 10.5517/cc738k4
title: CCDC 211685: Experimental Crystal Structure Determination

description: Related Article: D.B.Fox, R.Liantonio, P.Metrangolo, T.Pilati, G.Resnati|2004|J.Fluorine Chem.|125|271|doi:10.1016/j.jfluchem.2003.07.020
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/ph6f-g356
title: NOAA/WDS Paleoclimatology - Caspian Sea-Level Changes During the Last Millennium

description: Historical literature may constitute a valuable source of information to reconstruct sea-level changes. Here, historical documents and geological records have been combined to reconstruct Caspian sea-level (CSL) changes during the last millennium. In addition to a comprehensive literature review, new data from two short sediment cores were obtained from the south-eastern Caspian coast to identify coastal change driven by water-level changes and to compare the results with other geological and historical findings.
description: additional information, not in the publication, for circle points in fig. 9			
Year (AD)	CSL	Reference	Explanation
1100-1125	<-25	 Varushchenko et al.	Varushchenko et al. (1987) findings, based on
		-1987	dating, are more compatible with our findings
			in this paper than Bruckner (1890) or
			Karpychev (1998, 2001) historical evidence.
1425-1450	-26	Varushchenko et al.	These 2 papers support each other while the
		-1987	findings of Bruckner (1890) seem to be
		Karpychev (1998, 2001)	overestimated. I have chosen the overlapped
			years, reported by the researchers for this
			time. (the extended timeframe is 1350-1478
			AD for -26)
1680	<-24 	Bruckner (1890)	All the graphs of the referenced authors meet
		Karpychev (1998, 2001)	each other in this time that support Komarova
		Varushchenko et al.	(1980) sea level curve for this period.
                -1987	
1700	<-26 	Bruckner (1890)	The reported sea level is around the same for
		Karpychev (1998, 2001)	this time by different researchers. Moreover,
		Fedchina (1980)	this is supported by the findings of Fedchina
		Komarova (1980)	(1980) and Komarova (1980).
1740	>-23	 Bruckner (1890)	There is a good agreement between different
		Karpychev (1998, 2001)	researchers on CSL in this time based on
		Fedchina (1980)	different approaches Komarova (1980)	
1775-1790	<-22 	Bruckner (1890)	In addition to the references, Karpychev
		Varushchenko et al.	(1998, 2001) indicated CSL for 1770-1790
		-1987	and 1790-1810 as -25 and -22, respectively.
		Komarova (1980)	According to radiocarbon dating method and
			its errors, I have preferred to choose the -22 CSL for this time.
1825	>-25	 Bruckner (1890)	Bruckner (1890) indicated CSL as -25.8 m in
		Varushchenko et al.	1825 and Varushchenko et al. (1987) indicated
		-1987	the CSL -25 in 1825-1826. When we plot
			other results from Karpychev (1998, 2001),
			all the graphs meet each other in -25 m in 1825
DOI: 10.5517/cc7238n
title: CCDC 210560: Experimental Crystal Structure Determination

description: Related Article: B.Hoge, C.Thosen, T.Herrmann, P.Panne, I.Pantenburg|2004|J.Fluorine Chem.|125|831|doi:10.1016/j.jfluchem.2004.02.012
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/cc7239p
title: CCDC 210561: Experimental Crystal Structure Determination

description: Related Article: B.Hoge, C.Thosen, T.Herrmann, P.Panne, I.Pantenburg|2004|J.Fluorine Chem.|125|831|doi:10.1016/j.jfluchem.2004.02.012
description: Related Article: B.Hoge, C.Thosen, I.Pantenburg|2006|Chem.-Eur.J.|12|9019|doi:10.1002/chem.200600259
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/pjc7-4s28
title: NOAA/WDS Paleoclimatology - Ha'afera Island, Tonga Annually-Averaged Porites lutea Sr/Ca and d18O Data from 1791-2004 CE

description: In the South Pacific Convergence Zone (SPCZ), the variability in a sub-seasonally resolved microatoll Porites colony Sr/Ca record from Tonga and a previously published high-resolution record from Fiji are strongly influenced by sea surface temperature (SST) over the calibration period from 1981 to 2004 (R^2 = 0.67-0.68). However, the Sr/Ca-derived SST correlation to instrumental SST decreases back in time. The lower frequency secular trend (~1 ºC) and decadal-scale (~2-3 ºC) modes in Sr/Ca-derived SST are almost two times larger than that observed in instrumental SST. The coral Sr/Ca records suggest that local effects on SST generate larger amplitude variability than gridded SST products indicate. Reconstructed d18O of seawater (d18Osw) at these sites correlate with instrumental sea surface salinity (SSS; r = 0.64-0.67) but not local precipitation (r = -0.10 to -0.22) demonstrating that the advection and mixing of different salinity water masses may be the predominant control on d18Osw in this region. The Sr/Ca records indicate SST warming over the last 100 years and appears to be related to the expansion of the western Pacific warm pool (WPWP) including an increasing rate of expansion in the last ~20 years. The reconstructed d18Osw over the last 100 years also shows surface water freshening across the SPCZ. The warming and freshening of the surface ocean in our study area suggests that the SPCZ has been shifting (expanding) southeast, possibly related to the southward shift and intensification of the South Pacific gyre over the last 50 years in response to strengthened westerly winds.
description: d18O Data added to study in November 2021.
DOI: 10.5517/cc7wgzj
title: CCDC 234948: Experimental Crystal Structure Determination

description: Related Article: Chunlin Ni, Yizhi Li, Zhaoping Ni, Qingjin Meng|2004|J.Coord.Chem.|57|1321|doi:10.1080/00958970412331295246
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/p5bp-6q17
title: NOAA/WDS Paleoclimatology - Cook - Zairat Chitral - CDDE - ITRDB PAKI040

description: Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period ad 1971-2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years.
description: Purpose of Collection: 
# Climatology - temperature analyses NOAA Template Raw Measurements file added 2019-04-08. July 2024: Elevation added by WDS-Paleo using get_elev_point() from the elevatr R package with the AWS Terrain Tiles (aws) and WGS 84 reference frame.
DOI: 10.5517/cc63htl
title: CCDC 182119: Experimental Crystal Structure Determination

description: Related Article: Juan Li, Yanfei Qi, Jing Li, Hongfang Wang, Xinyu Wu, Liying Duan, Enbo Wang|2004|J.Coord.Chem.|57|1309|doi:10.1080/00958970412331295237
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/cc63shk
title: CCDC 182388: Experimental Crystal Structure Determination

description: Related Article: Juan Li, Yanfei Qi, Jing Li, Hongfang Wang, Xinyu Wu, Liying Duan, Enbo Wang|2004|J.Coord.Chem.|57|1309|doi:10.1080/00958970412331295237
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/cc63sjl
title: CCDC 182389: Experimental Crystal Structure Determination

description: Related Article: Juan Li, Yanfei Qi, Jing Li, Hongfang Wang, Xinyu Wu, Liying Duan, Enbo Wang|2004|J.Coord.Chem.|57|1309|doi:10.1080/00958970412331295237
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/cc766qb
title: CCDC 214511: Experimental Crystal Structure Determination

description: Related Article: Yan-Qiong Sun, Jie Zhang, Guo-Yu Yang|2004|J.Coord.Chem.|57|1299|doi:10.1080/00958970412331295200
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/pn8m-s076
title: NOAA/WDS Paleoclimatology - Cook - Altai UGLA - LASI - ITRDB RUSS234

description: Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period ad 1971-2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years.
description: Purpose of Collection: 
# Climatology - temperature analyses NOAA Template Raw Measurements file added 2019-04-08. July 2024: Elevation added by WDS-Paleo using get_elev_point() from the elevatr R package with the AWS Terrain Tiles (aws) and WGS 84 reference frame.
DOI: 10.5517/cc766rc
title: CCDC 214512: Experimental Crystal Structure Determination

description: Related Article: Yan-Qiong Sun, Jie Zhang, Guo-Yu Yang|2004|J.Coord.Chem.|57|1299|doi:10.1080/00958970412331295200
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/cc7rj0h
title: CCDC 231136: Experimental Crystal Structure Determination

description: Related Article: D.V.Shevchenko, S.R.Petrusenko, V.N.Kokozay, B.W.Skelton|2004|J.Coord.Chem.|57|1287|doi:10.1080/0095897042000274742
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: 10.15468/dl.dwrxhp
title: Occurrence Download

description: A dataset containing 5344 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Papua New Guinea, Vanuatu, Solomon Islands)",
 "OccurrenceStatus is Present",
 "TaxonKey is Nactus"
 ]
}

 The dataset includes 5344 records from 45 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0021234-251009101135966/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25921/pyb7-8c92
title: NOAA/WDS Paleoclimatology - Gulf of Alaska 1200 Year Surface Air Temperature Reconstruction

description: A 1200-year-long tree-ring width record from living and subfossil mountain hemlock wood is used to reconstruct February through August temperatures for the Gulf of Alaska, providing a record of past climate variability for the Northeast Pacific sector that captures interannual to centennial timescales. The moderate elevation at the tree-ring sites has allowed these trees to retain their temperature signal without evidence of the so-called divergence effect, or underestimation of tree-ring inferred temperature trends, which is observed at many northern latitude forest locations. This 'divergence-free' reconstruction reveals centennial trends that include a warm interval centered on ad 950 for coastal Alaska that occurs around the time of the 'Medieval Warm Period', a warming that is only rivaled by recent decades. Spectral analysis of this reconstruction supports the centennial pacing identified as a 170-220-year cadence consistent with solar variability. On the decadal to bidecadal scale, the reconstruction reveals ~10- and 18-year cycles, which have been observed elsewhere in climate records for western North America and are linked to solar and lunar tidal forcing, respectively. Temperature minima that occur at ad 969-970 and 1698-1700 correspond with the timing of major volcanic events. This tree-ring reconstruction supports centennial modes of solar forcing as a driver of surface air temperatures in the Gulf of Alaska, with lunar tidal, solar variability, internal variability, and volcanism, impacting climate on annual to decadal timescales. 
description: Gulf of Alaska February-August temperature reconstruction for the past 1200 years, based on living and subfossil mountain hemlock ring widths.
DOI: 10.5517/cc7rj1j
title: CCDC 231137: Experimental Crystal Structure Determination

description: Related Article: D.V.Shevchenko, S.R.Petrusenko, V.N.Kokozay, B.W.Skelton|2004|J.Coord.Chem.|57|1287|doi:10.1080/0095897042000274742
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: 10.6084/m9.figshare.30359167
title: CT30_TRIM28_rep1_IP

description: TRIM28 ChIP seq hTSC
DOI: 10.6084/m9.figshare.30359167.v1
title: CT30_TRIM28_rep1_IP

description: TRIM28 ChIP seq hTSC
DOI: 10.25921/pr21-m443
title: NOAA/WDS Paleoclimatology - Douglas - Blanca Peak - PIAR - CO562, PAGES North America 2K Version

description: Variability in the intensity and magnitude of the Pacific North American (PNA) circulation pattern and the reverse-PNA affects high and low frequency temperature variations on either side of the Continental Divide, on the Colorado Plateau. The PNA circulation pattern corresponds with cooler temperatures on the Colorado Plateau, whereas the reverse-PNA circulation pattern corresponds with warmer temperatures on the Colorado Plateau associated with a high pressure ridge over the Rocky Mountains.

Temperature was reconstructed using three Pinus aristata (bristlecone pine) chronologies and one Pinus flexilis (limber pine) chronology from subalpine sites located on either side of the Continental Divide in Colorado and Arizona. The standardized ring-indices of the four chronologies (scAD 548-1994) were correlated with historic temperature data from twelve ground stations and upper air temperature data from four radiosonde stations in Arizona, Colorado, New Mexico and Utah.

Temperature reconstructions across a transect spanning the Continental Divide on the Colorado Plateau provide valuable insight to temporal changes in large scale circulation patterns. Reconstructions of annual temperature indicate there were several periods when temperatures were below the modern mean east of the Continental Divide when they were above the modern mean west of the Continental Divide. Variability in the direction of temperature change on either side of the Continental Divide may reflect a westward displacement of the high pressure ridge at different times in history. Reconstructions of annual temperature also indicate 850 mb temperature east of the Divide is slightly higher when the PNA circulation pattern occurs as a teleconnection to El Nino Southern Oscillation (ENSO) events. In contrast, annual 700 mb temperature west of the Divide is slightly lower.

Temperature reconstructions also indicate higher mean annual temperatures occurred between scAD 550 to 600, scAD 900-980, and scAD 1040-1080, and scAD 1130-150 than between 1950 and the present. These reconstructions suggest low frequency cycles of above average temperatures have occurred throughout history. These results indicate more research is required to determine whether recent warming trends identified by other researchers reflect anthropogenic warming or natural cycles.