cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.14298402.v1
title: Paleoclimatic and vegetational change in the Siwalik sub-Group of Pakistan and its contemporary geographic regions: a stable isotope perspective

description: Paleoclimatic archives preserved in bioapatite provide long-term temporal records of climatic change and allow us to explore how climate may have affected faunal and floral changes through time. Among the most comprehensively debated research questions is the question of C<sub>4</sub> grassland expansion and its effects on community structure and dynamics. Here, we present compiled datasets of carbon isotopes from fossil tooth enamel and paleosol to evaluate how C<sub>4</sub> grasslands expanded and its apparent causes. The C<sub>4</sub> expansion has been argued to be around <i>ca</i> 8–7 Ma in the Siwalik sub-Group of Pakistan, but the later stages of C<sub>3</sub>/C<sub>4</sub> proportion shifts on the Siwalik floodplains are less understood. We found that although C<sub>4</sub> expansion occurred during the late Miocene, C<sub>3</sub> vegetation never entirely disappeared but was persisted in pockets on floodplain up to the present, as indicated by the C<sub>3</sub> diet consumed by some herbivores. The expansion was further modulated by the microclimate in different regions. The same scenario can be seen in East Africa, South America and low-latitude North America where C<sub>4</sub> grasslands expanded rapidly in late Miocene most likely owing to decrease in global <i>p</i>CO<sub>2</sub>. By contrast, C<sub>4</sub> plants did not expand in high-latitude North America and Palearctic regions during the past <i>ca</i> 17 Ma. Thus, we assume that C<sub>4</sub> plants expanded at low latitudes during the late Miocene owing to one major global factor (decreased <i>p</i>CO<sub>2</sub>) and perhaps other local microclimatic factors like paleofires.KEY POINTSDuring the late Miocene, low-latitude regions experienced a climatic change followed by a transition from C<sub>3</sub> to C<sub>4</sub> vegetation.The timing of C<sub>4</sub> expansion was not synchronous across all the regions and was controlled by global and microclimatic factors.Although C<sub>4</sub> vegetation expanded after the late Miocene, C<sub>3</sub> vegetation did not disappear and was present at the edges of floodplains.The new adaptive physiologies (like hypsodonty) in faunal elements were evolutionary adaptive responses toward new vegetational types available. During the late Miocene, low-latitude regions experienced a climatic change followed by a transition from C<sub>3</sub> to C<sub>4</sub> vegetation. The timing of C<sub>4</sub> expansion was not synchronous across all the regions and was controlled by global and microclimatic factors. Although C<sub>4</sub> vegetation expanded after the late Miocene, C<sub>3</sub> vegetation did not disappear and was present at the edges of floodplains. The new adaptive physiologies (like hypsodonty) in faunal elements were evolutionary adaptive responses toward new vegetational types available.
DOI: 10.6084/m9.figshare.14298402
title: Paleoclimatic and vegetational change in the Siwalik sub-Group of Pakistan and its contemporary geographic regions: a stable isotope perspective

description: Paleoclimatic archives preserved in bioapatite provide long-term temporal records of climatic change and allow us to explore how climate may have affected faunal and floral changes through time. Among the most comprehensively debated research questions is the question of C<sub>4</sub> grassland expansion and its effects on community structure and dynamics. Here, we present compiled datasets of carbon isotopes from fossil tooth enamel and paleosol to evaluate how C<sub>4</sub> grasslands expanded and its apparent causes. The C<sub>4</sub> expansion has been argued to be around <i>ca</i> 8–7 Ma in the Siwalik sub-Group of Pakistan, but the later stages of C<sub>3</sub>/C<sub>4</sub> proportion shifts on the Siwalik floodplains are less understood. We found that although C<sub>4</sub> expansion occurred during the late Miocene, C<sub>3</sub> vegetation never entirely disappeared but was persisted in pockets on floodplain up to the present, as indicated by the C<sub>3</sub> diet consumed by some herbivores. The expansion was further modulated by the microclimate in different regions. The same scenario can be seen in East Africa, South America and low-latitude North America where C<sub>4</sub> grasslands expanded rapidly in late Miocene most likely owing to decrease in global <i>p</i>CO<sub>2</sub>. By contrast, C<sub>4</sub> plants did not expand in high-latitude North America and Palearctic regions during the past <i>ca</i> 17 Ma. Thus, we assume that C<sub>4</sub> plants expanded at low latitudes during the late Miocene owing to one major global factor (decreased <i>p</i>CO<sub>2</sub>) and perhaps other local microclimatic factors like paleofires.KEY POINTSDuring the late Miocene, low-latitude regions experienced a climatic change followed by a transition from C<sub>3</sub> to C<sub>4</sub> vegetation.The timing of C<sub>4</sub> expansion was not synchronous across all the regions and was controlled by global and microclimatic factors.Although C<sub>4</sub> vegetation expanded after the late Miocene, C<sub>3</sub> vegetation did not disappear and was present at the edges of floodplains.The new adaptive physiologies (like hypsodonty) in faunal elements were evolutionary adaptive responses toward new vegetational types available. During the late Miocene, low-latitude regions experienced a climatic change followed by a transition from C<sub>3</sub> to C<sub>4</sub> vegetation. The timing of C<sub>4</sub> expansion was not synchronous across all the regions and was controlled by global and microclimatic factors. Although C<sub>4</sub> vegetation expanded after the late Miocene, C<sub>3</sub> vegetation did not disappear and was present at the edges of floodplains. The new adaptive physiologies (like hypsodonty) in faunal elements were evolutionary adaptive responses toward new vegetational types available.
DOI: 10.6084/m9.figshare.14452039
title: Geochemistry and provenance of lower Permian sedimentary rocks, Nambucca Block, southern New England Orogen

description: It is well documented that sediments record geochemical signatures that reflect the composition and tectonic setting of the rocks providing the detritus for them. This is true of the turbidites in the Nambucca Block that record compositions that vary from basaltic to rhyodacitic but are dominantly andesitic to dacitic. They show chondrite and N-MORB patterns, characteristic of calc-alkaline, continental arc rocks, namely light REE (av. La/Yb)<b><sub>N</sub></b> = 6.3) and Th enrichment, Ti, Nb and Ta depletion, and substantial within plate components (Nb/Yb; 0.65–5.16; <i>x</i> = 3.15). Rare occurrences of rocks with intra-oceanic island arc affinities and felsic volcanic rocks showing tectonic fabrics occur, indicating more distal sources contributed detritus. Most detritus in the turbidites has been derived from the calc-alkaline, continental rocks of the Keepit arc, some from the subduction–accretion sequences of the Tablelands Complex. CIA [Al<sub>2</sub>O<sub>3</sub>/(Al<sub>2</sub>O<sub>3</sub>+Na<sub>2</sub>O + K<sub>2</sub>O + CaO)×100] values (48–83; <i>x</i> = 68) indicate that erosion of these arc sequences occurred during glacial, temperate and humid conditions at different times. Further, index of chemical variability values (0.3–1.85; <i>x</i> = 0.85) reveal a compositional maturity and a high percentage of clays in the source rocks suggesting a passive tectonic setting in which minimal uplift and extensive weathering took place.KEY POINTSMetasediments in the Nambucca Block record geochemical signatures typical of calc-alkaline, continental, arc rocks.Detritus in metasediments was derived from the Keepit arc and Tablelands Complex, southern New England Orogen.Source rocks were subjected to glacial, temperate and humid conditions at different times. Metasediments in the Nambucca Block record geochemical signatures typical of calc-alkaline, continental, arc rocks. Detritus in metasediments was derived from the Keepit arc and Tablelands Complex, southern New England Orogen. Source rocks were subjected to glacial, temperate and humid conditions at different times.
DOI: 10.6084/m9.figshare.14452039.v1
title: Geochemistry and provenance of lower Permian sedimentary rocks, Nambucca Block, southern New England Orogen

description: It is well documented that sediments record geochemical signatures that reflect the composition and tectonic setting of the rocks providing the detritus for them. This is true of the turbidites in the Nambucca Block that record compositions that vary from basaltic to rhyodacitic but are dominantly andesitic to dacitic. They show chondrite and N-MORB patterns, characteristic of calc-alkaline, continental arc rocks, namely light REE (av. La/Yb)<b><sub>N</sub></b> = 6.3) and Th enrichment, Ti, Nb and Ta depletion, and substantial within plate components (Nb/Yb; 0.65–5.16; <i>x</i> = 3.15). Rare occurrences of rocks with intra-oceanic island arc affinities and felsic volcanic rocks showing tectonic fabrics occur, indicating more distal sources contributed detritus. Most detritus in the turbidites has been derived from the calc-alkaline, continental rocks of the Keepit arc, some from the subduction–accretion sequences of the Tablelands Complex. CIA [Al<sub>2</sub>O<sub>3</sub>/(Al<sub>2</sub>O<sub>3</sub>+Na<sub>2</sub>O + K<sub>2</sub>O + CaO)×100] values (48–83; <i>x</i> = 68) indicate that erosion of these arc sequences occurred during glacial, temperate and humid conditions at different times. Further, index of chemical variability values (0.3–1.85; <i>x</i> = 0.85) reveal a compositional maturity and a high percentage of clays in the source rocks suggesting a passive tectonic setting in which minimal uplift and extensive weathering took place.KEY POINTSMetasediments in the Nambucca Block record geochemical signatures typical of calc-alkaline, continental, arc rocks.Detritus in metasediments was derived from the Keepit arc and Tablelands Complex, southern New England Orogen.Source rocks were subjected to glacial, temperate and humid conditions at different times. Metasediments in the Nambucca Block record geochemical signatures typical of calc-alkaline, continental, arc rocks. Detritus in metasediments was derived from the Keepit arc and Tablelands Complex, southern New England Orogen. Source rocks were subjected to glacial, temperate and humid conditions at different times.
DOI: 10.6084/m9.figshare.13263092.v1
title: Review of life history parameters and preliminary age estimates of some New Zealand deep-sea fishes

description: A literature review on longevity of New Zealand deep-sea fishes provided life history parameter estimates for 17 bony and five cartilaginous species. Preliminary age estimates for a further nine deep-sea bony fishes were made from otolith zone counts and included results from a pilot analysis of radiocarbon age estimates from the otoliths of three of the species. Radiocarbon age estimates corroborated the otolith zone count age estimates made for white rattail (<i>Trachyrincus aphyodes</i>) and smallhead cod (<i>Lepidion microcephalus</i>) but were substantially lower for the third species, smallscale brown slickhead (<i>Alepocephalus antipodianus</i>) which suggested that it was not exposed to elevated (near-surface) levels of <sup>14</sup>C in early life. Validation of otolith zone age estimates is difficult for deep-sea species but the radiocarbon analysis provided a practical method to corroborate age estimates for some bony fishes. Of the 31 fish in this study (known and new age estimates), five of the fishery target species and 10 of the bycatch were long-lived (50 years or more). The hypothesis that all New Zealand deep-sea species are long-lived was not supported, but the chance of a species being long-lived seem to be higher in deeper water.
DOI: 10.6084/m9.figshare.13263092
title: Review of life history parameters and preliminary age estimates of some New Zealand deep-sea fishes

description: A literature review on longevity of New Zealand deep-sea fishes provided life history parameter estimates for 17 bony and five cartilaginous species. Preliminary age estimates for a further nine deep-sea bony fishes were made from otolith zone counts and included results from a pilot analysis of radiocarbon age estimates from the otoliths of three of the species. Radiocarbon age estimates corroborated the otolith zone count age estimates made for white rattail (<i>Trachyrincus aphyodes</i>) and smallhead cod (<i>Lepidion microcephalus</i>) but were substantially lower for the third species, smallscale brown slickhead (<i>Alepocephalus antipodianus</i>) which suggested that it was not exposed to elevated (near-surface) levels of <sup>14</sup>C in early life. Validation of otolith zone age estimates is difficult for deep-sea species but the radiocarbon analysis provided a practical method to corroborate age estimates for some bony fishes. Of the 31 fish in this study (known and new age estimates), five of the fishery target species and 10 of the bycatch were long-lived (50 years or more). The hypothesis that all New Zealand deep-sea species are long-lived was not supported, but the chance of a species being long-lived seem to be higher in deeper water.
DOI: 10.5281/zenodo.5279799
title: Dataset of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars

description: This dataset contains the original data and crater counting data of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars.
DOI: 10.5281/zenodo.5031312
title: Dataset of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars

description: This dataset contains the original data and crater counting data of the paper titled Geological characteristics and high scientific interest targets of the Zhurong landing region on Mars.
DOI: 10.25345/c5b256
title: MassIVE MSV000088027 - GNPS Indonesian Marine Sponge Genus Aaptos
title: Secondary metabolites from the marine sponge of the genus Aaptos. The specimens were collected during 2017-2019 around Sabang and Aceh islands, Indonesia. The extracts and standards were provided in this study.
DOI: 10.6084/m9.figshare.15127988
title: Negative interaction of fatty liver and hypertension on cardiovascular mortality in non-diabetic men: 34 years of follow-up

description: Fatty liver disease (FLD) and hypertension are separately associated with cardiovascular (CV) mortality. The two conditions are related in multiple ways. This work aimed to study the joint effect and interaction of FLD and hypertension in respect to overall and CV mortality. The population-based cohort, Kuopio Ischaemic Disease Risk Factor Study, followed 1569 middle-aged non-diabetic Finnish men for 34 years. Considering adjustment for age, body mass index, smoking and alcohol consumption, separate and combined effects of FLD and hypertension and their interaction at the multiplicative and additive scales regarding all-cause and CV death were assessed using Cox proportional hazards models. FLD and hypertension coexisted in 8.54% of the men (<i>n</i> = 134). FLD and hypertension associated, independently and combined, with an increased hazard of all-cause and CV deaths. Non-CV mortality associated with FLD, but not with hypertension. We found a negative interaction between FLD and hypertension regarding the hazard of all-cause (relative excess risk due to interaction (RERI), −0.97; 95% confidence interval (CI), −1.65 to −0.28) and CV mortality (RERI, −1.74; 95% CI, −2.98 to −0.5). The interaction was also found on a multiplicative scale. We found evidence of a negative interaction between FLD and hypertension in respect to CV mortality. We thus recommend adjusting for FLD or hypertension when studying the effect of the other condition on mortality or CV diseases in middle-aged men.
DOI: 10.6084/m9.figshare.15127988.v1
title: Negative interaction of fatty liver and hypertension on cardiovascular mortality in non-diabetic men: 34 years of follow-up

description: Fatty liver disease (FLD) and hypertension are separately associated with cardiovascular (CV) mortality. The two conditions are related in multiple ways. This work aimed to study the joint effect and interaction of FLD and hypertension in respect to overall and CV mortality. The population-based cohort, Kuopio Ischaemic Disease Risk Factor Study, followed 1569 middle-aged non-diabetic Finnish men for 34 years. Considering adjustment for age, body mass index, smoking and alcohol consumption, separate and combined effects of FLD and hypertension and their interaction at the multiplicative and additive scales regarding all-cause and CV death were assessed using Cox proportional hazards models. FLD and hypertension coexisted in 8.54% of the men (<i>n</i> = 134). FLD and hypertension associated, independently and combined, with an increased hazard of all-cause and CV deaths. Non-CV mortality associated with FLD, but not with hypertension. We found a negative interaction between FLD and hypertension regarding the hazard of all-cause (relative excess risk due to interaction (RERI), −0.97; 95% confidence interval (CI), −1.65 to −0.28) and CV mortality (RERI, −1.74; 95% CI, −2.98 to −0.5). The interaction was also found on a multiplicative scale. We found evidence of a negative interaction between FLD and hypertension in respect to CV mortality. We thus recommend adjusting for FLD or hypertension when studying the effect of the other condition on mortality or CV diseases in middle-aged men.
DOI: 10.6084/m9.figshare.16435581
title: List of CAZy annotations in Genomes from Earth’s Microbiomes

description: List of all annotated CAZymes in MAGs from global study Genomes from Earth’s Microbiomes.<br>
DOI: 10.6084/m9.figshare.16457595
title: Anonymizedfile.xls

description: <b>This is the XLS file used to statistical analysis of the our work" Social isolation but not deprivation involved in employment status after bariatric surgery." published in PLOSONE journal </b><br>
DOI: 10.6084/m9.figshare.16457595.v1
title: Anonymizedfile.xls

description: <b>This is the XLS file used to statistical analysis of the our work" Social isolation but not deprivation involved in employment status after bariatric surgery." published in PLOSONE journal </b><br>
DOI: 10.5517/ccdc.csd.cc1j9mv9
title: CCDC 1409441: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1j9mwb
title: CCDC 1409442: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1j9mxc
title: CCDC 1409443: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1j9mzf
title: CCDC 1409445: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1nhyqt
title: CCDC 1534677: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1nhyrv
title: CCDC 1534678: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1q4xxp
title: CCDC 1583663: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1q4xyq
title: CCDC 1583664: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1q4xzr
title: CCDC 1583665: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1q4y0t
title: CCDC 1583666: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc1q4y1v
title: CCDC 1583667: Experimental Crystal Structure Determination

description: Related Article: Chayma Ben Maamer, Pierre C. Mpawenayo, Baptiste Lecachey, Nacira Alouane, Pierre Mangeney, Arie van der Lee, Jérôme Marrot, Samira Bouaouli, Maya Guillaumont, Rafâa Besbes, Hélène Gerard, Emmanuel Vrancken, Jean-Marc Campagne|2021|Org.Lett.|23|6305|doi:10.1021/acs.orglett.1c02095
DOI: 10.5517/ccdc.csd.cc2281zd
title: CCDC 1914373: Experimental Crystal Structure Determination

description: Related Article: Dominic Bara, Claire Wilson, Max Mörtel, Marat M. Khusniyarov, Sanliang Ling, Ben Slater, Stephen Sproules, and Ross S. Forgan|2019|J.Am.Chem.Soc.|141|8346|doi:10.1021/jacs.9b03269
DOI: 10.5517/ccdc.csd.cc22820g
title: CCDC 1914374: Experimental Crystal Structure Determination

description: Related Article: Dominic Bara, Claire Wilson, Max Mörtel, Marat M. Khusniyarov, Sanliang Ling, Ben Slater, Stephen Sproules, and Ross S. Forgan|2019|J.Am.Chem.Soc.|141|8346|doi:10.1021/jacs.9b03269
DOI: 10.5517/ccdc.csd.cc2507gx
title: CCDC 1996228: Experimental Crystal Structure Determination

description: Related Article: Bartłomiej Pigulski, Kazutaka Shoyama, Frank Würthner|2020|Angew.Chem.,Int.Ed.|59|15908|doi:10.1002/anie.202005376
DOI: 10.5517/ccdc.csd.cc253k73
title: CCDC 1999414: Experimental Crystal Structure Determination

description: Related Article: Isabelle Georg, Markus Bursch, Julius B. Stückrath, Edith Alig, Michael Bolte, Hans-Wolfram Lerner, Stefan Grimme, Matthias Wagner|2020|Angew.Chem.,Int.Ed.|59|16181|doi:10.1002/anie.202006463