cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.10073669
title: marsdenia_floribunda_decontaminated_FSCR.fasta.gz

description: marsdenia_floribunda_decontaminated_FSCR.fasta.gz
DOI: 10.5281/zenodo.10073677
title: microcambeva_barbata_decontaminated_FSCR.fasta.gz

description: microcambeva_barbata_decontaminated_FSCR.fasta.gz
DOI: 10.3886/e194923
title: Framing Welfare Expansion: Citizenship, Collective Memory, and Fiscal Dilemmas in Mexico (1997-1998) and Peru (2005-2006)

description: The present study is an analysis of the congressional debates that led to the implementation of the Conditional Cash Transfer programs in Mexico (1997) and Peru (2005), focusing on the narratives mobilized by legislators and members of the Executive branch in deliberation. Empirically, the analysis is primarily based on transcripts of all relevant congressional debates in the Senate and House of Representatives (in Mexico, both chambers, Peru has a unicameral legislature). To identify the periods of analysis, I used secondary sources, newspaper articles, and executive decrees and traced the process of the program conception, discussion, and implementation. The process of locating newspaper articles consisted of Factiva searches of the original-language editions of newspapers in Mexico and Peru. For the case of Mexico, I searched under “Progresa” from January 1997 to January 1998 and got 68 hits. For the case of Peru, I searched under “Juntos” from January 2005 to January 2006. As expected, since the word Juntos in Spanish means “together,” I got a larger number of hits: 389. The articles come from a diversity of newspapers, but a third of the hits come from the most important general interest newspapers in both countries: El Universal in Mexico and El Comercio in Peru. From this process, I selected hearings in two contentious periods in the initial stage of the program: the debates following the program’s official launch by the Executive to the Congress (September 1997 in Mexico; February-July 2005 in Peru) and the budget approval/modification (November-December 1997 in Mexico; June and November 2005 in Peru). The hearings lasted an average of four hours each. All the debates were conducted in Spanish.
DOI: 10.3886/e194923v1
title: Framing Welfare Expansion: Citizenship, Collective Memory, and Fiscal Dilemmas in Mexico (1997-1998) and Peru (2005-2006)

description: The present study is an analysis of the congressional debates that led to the implementation of the Conditional Cash Transfer programs in Mexico (1997) and Peru (2005), focusing on the narratives mobilized by legislators and members of the Executive branch in deliberation. Empirically, the analysis is primarily based on transcripts of all relevant congressional debates in the Senate and House of Representatives (in Mexico, both chambers, Peru has a unicameral legislature). To identify the periods of analysis, I used secondary sources, newspaper articles, and executive decrees and traced the process of the program conception, discussion, and implementation. The process of locating newspaper articles consisted of Factiva searches of the original-language editions of newspapers in Mexico and Peru. For the case of Mexico, I searched under “Progresa” from January 1997 to January 1998 and got 68 hits. For the case of Peru, I searched under “Juntos” from January 2005 to January 2006. As expected, since the word Juntos in Spanish means “together,” I got a larger number of hits: 389. The articles come from a diversity of newspapers, but a third of the hits come from the most important general interest newspapers in both countries: El Universal in Mexico and El Comercio in Peru. From this process, I selected hearings in two contentious periods in the initial stage of the program: the debates following the program’s official launch by the Executive to the Congress (September 1997 in Mexico; February-July 2005 in Peru) and the budget approval/modification (November-December 1997 in Mexico; June and November 2005 in Peru). The hearings lasted an average of four hours each. All the debates were conducted in Spanish.
DOI: 10.5281/zenodo.10073676
title: microcambeva_barbata_decontaminated_FSCR.fasta.gz

description: microcambeva_barbata_decontaminated_FSCR.fasta.gz
DOI: 10.5281/zenodo.10073628
title: Abiotic controls on warm-water carbonates through geological times

description: Evaluation of global carbonate distribution and accumulation over the past 265 Myr accounting for changes in paleogeography, plate tectonics, and paleo-climatic conditions.
description: The approach relies on (1) paleo-environmental ocean variables from the HadCM3 (BRIDGE) coupled atmosphere-ocean-vegetation Hadley Centre climate models, (2) the observed modern photozoan-T factory defined after Michel et al., (3) the updated continental margins and paleocoastlines dataset available on Zenodo based on the paleogeography maps from the PALEOMAP project, and (4) sediment flux derived from global scale landscape evolution model for the Phanerozoic HydroShare. In addition, sensitivity tests are making use of the fossil records from the Paleo Reefs PARED database.
description: All provided data are available as geotiff files.
The dataset contains the environmental variables for each time slice (approximately every 5 Myr) and for 2 CO2 scenarios (Foster & Smooth curves - Foster_ensemble.zip and Smooth_ensemble.zip):

currents
ocean stream
SSS max
SSS min
SST max
SST min
sediment influx
Then the results from the species distribution model (BIOMOD2) ensemble models are provided for each CO2 scenarios and contains four variables (FosterCO2.zip and Smooth_CO2.zip): 

median of probabilities (median),
mean of probabilities (mean),
weighted mean of probabilities according to single evaluation scores (wmean) and
committee averaging score (ca):
Additional information are provided in the companion GitHub repository.
DOI: 10.6084/m9.figshare.21938306
title: Exporting, investing, and productivity dynamics in African manufacturing

description: Supplemental file documents in Stata .dta and .do format for: Exporting, investing, and productivity dynamics in African manufacturing
DOI: 10.6084/m9.figshare.21938306.v2
title: Exporting, investing, and productivity dynamics in African manufacturing

description: Supplemental file documents in Stata .dta and .do format for: Exporting, investing, and productivity dynamics in African manufacturing
DOI: 10.48329/cfh2-kf80
title: CPRD GOLD November 2023

description: The CPRD GOLD database contains longitudinal routinely-collected electronic health records (EHR data) from UK primary care practices using Vision® general practice patient management software. The database captures information on demographic characteristics; diagnoses and symptoms; drug exposures; vaccination history; laboratory tests; and referrals to hospital and specialist care. Access to anonymised data from CPRD is subject to a full licence agreement containing detailed terms and conditions of use. Anonymised patient datasets can be extracted for researchers against specific study specifications, following protocol approval. Further information is available at https://www.cprd.com/data-access.
DOI: 10.6084/m9.figshare.22134842
title: Tectonic control on travertine and silica sinter deposition in oceanic transform-fault setting: the case of the Lýsuskarð volcano-geothermal area, Snæfellsnes Peninsula, Iceland

description: Deposition of terrestrial carbonate (i.e. travertine) and silica sinter in geothermal areas is always closely linked to the presence of relevant crustal structures which enhance the permeability in the upper crust favouring the upflow of fluids to the surface. Most travertine deposits are originated by geothermal fluids stored within carbonate reservoirs in continental crust, and their morphology and areal distribution provide useful information on geometry, kinematics, and age of faults which control the fluid flow. In this paper, we focus on the tectonic control on a travertine depositional system, associated with silica sinter, developing in oceanic crust, in the Lýsuskarð volcano-geothermal area on the Snæfellsnes Peninsula, West Iceland. The presence of HCO<sub>3</sub> and Ca in the geothermal fluids is related to chemical-physical processes linked to fluid–rock interaction that occurs in the geothermal reservoir made up of tholeiitic basalt, by fluids enriched in CO<sub>2</sub> of deep origin (i.e. magmatic). Travertine deposits consist of mounds and slopes, which are still in formation and overlie the silica sinter deposits. Both sinter and travertine deposits derive from thermal springs aligned according to two trends: NNE-SSW and WNW-ESE. This evidence suggests the occurrence of buried, permeable, and thus active faults, which control the circulation of fluids containing HCO<sub>3</sub> and Ca. Faults are near parallel to those which define the rift systems and transform zones in Iceland, and probably comprise the still active sector of the abandoned transform zone that, starting with the Snæfellsnes Peninsula, interrupts eastward the northern continuation of the western and eastern rift-zones in the south-central Iceland. In this setting, we refer, for the first time, travertine and silica sinter deposition to an oceanic active crustal structure.
DOI: 10.6084/m9.figshare.22274782
title: Middle Permian basic and acidic volcanism in the Istanbul zone (NW Turkey): evidence for post-variscan extensional magmatism

description: The Istanbul Zone (NW Turkey) forms the eastward extension of Avalonia and was subjected to deformation, uplift and erosion for a time period of 40–50 Ma following the collision with the Sakarya Zone during Early to Late Carboniferous. This paper deals with the petrology and age of the volumetrically minor basic and acidic volcanism at the lowermost horizons of Middle Permian continental red beds, which are overlain by Lower Triassic marine sedimentary rocks in the Kocaeli Peninsula. The volcanic activity is represented mainly by amygdaloidal basalt, rhyolite and minor trachydacite. The amygdaloidal basalt was derived from near-primary middle-K calc-alkaline mantle melts with negligible crystal fractionation. On the other hand, the rhyolite and trachydacite compositionally resemble A<sub>2</sub>-type rhyolites and underwent low-pressure crystal fractionation as indicated by the presence of a significant Eu anomaly. Initial ɛNd values of amygdaloidal basalt range from 0.0 to 1.5 and those of rhyolite-trachydacite are between −0.4 and −3.4. Amygdaloidal basalt and rhyolite-trachydacite are not directly related to each other by crystal fractionation. Amygdaloidal basalt probably represents the product of the near-primary mantle melts from low-degree melting of a spinel peridotitic source, and the rhyolite-trachydacite originated from highly-fractionated products of basic magmas that are slightly more alkaline than amygdaloidal basalt. However, basic and intermediate products of alkaline basic magmas are unknown in this region to date. U-Pb dating of zircons from a rhyolite sample yielded an igneous crystallization age of 261 ± 3 Ma (2σ), suggesting that the date of deposition of the continental red beds goes back to the latest Middle Permian. Based on the transgressive nature of the Permian-Triassic sequence that starts from the Middle Permian continental red beds and grades into Lower Triassic marine deposits, we suggest that the volcanism likely occurred in an extensional setting. This extension was concurrent with the northward subduction of the Palaeo-Tethys beneath the Sakarya and Istanbul zones after the Variscan orogeny. Therefore, the latest Middle to Late Permian volcanism might have occurred during the initial stage of a back-arc extensional setting
DOI: 10.6084/m9.figshare.22274792
title: Petrological and geochemical evidence for partial melting and melt-rock interaction in mantle rocks from the eastern part of the Sabzevar ophiolite, NE Iran

description: The Sabzevar ophiolite is the most extensive and best-exposed section of oceanic lithosphere in NE Iran. In this study, we examined the mantle section of the eastern part of the Sabzevar ophiolite, where mantle peridotites are the most widespread rock type and are crosscut by pyroxenite veins and mafic dykes. Major and trace element compositions (minerals and whole-rock) of lherzolites are akin to those of abyssal peridotites from mid-ocean ridges (MOR), whereas those of harzburgites evidence formation in a supra-subduction zone (SSZ) setting. Rare-earth element (REE) patterns of whole-rock and clinopyroxene of lherzolites and harzburgites suggest polybaric melting, with initial melting in the garnet peridotite field (~5–6%), followed by ~5–15% melting for lherzolites and ~10–20% for harzburgites in the spinel peridotite field. Harzburgites show LREE enrichment incompatible with partial melting models, indicating significant interaction with SSZ-related melts, whereas analysed lherzolites experienced limited melt-rock interaction. Pyroxene dissolution and olivine precipitation in residual peridotites resulting from reaction with island arc tholeiite and/or boninite melts led to the formation of dunites. These melts eventually intruded as dykes and veins in the mantle and crustal sections of the ophiolite. In addition, boninite melts are inferred to be responsible for forming olivine pyroxenite veins within the harzburgites. We conclude that the mantle section of the Sabzevar ophiolite formed in an intra-oceanic arc setting and experienced a geochemical evolution from a MOR-like to SSZ setting. The intra-oceanic subduction of the Neotethys oceanic lithosphere and shifting conditions of melting during the development of subduction beneath the incipient island arc were responsible for the geochemical heterogeneity of mantle peridotites and the generation of SSZ-related magmas within the Sabzevar oceanic lithosphere.
DOI: 10.6084/m9.figshare.22134842.v1
title: Tectonic control on travertine and silica sinter deposition in oceanic transform-fault setting: the case of the Lýsuskarð volcano-geothermal area, Snæfellsnes Peninsula, Iceland

description: Deposition of terrestrial carbonate (i.e. travertine) and silica sinter in geothermal areas is always closely linked to the presence of relevant crustal structures which enhance the permeability in the upper crust favouring the upflow of fluids to the surface. Most travertine deposits are originated by geothermal fluids stored within carbonate reservoirs in continental crust, and their morphology and areal distribution provide useful information on geometry, kinematics, and age of faults which control the fluid flow. In this paper, we focus on the tectonic control on a travertine depositional system, associated with silica sinter, developing in oceanic crust, in the Lýsuskarð volcano-geothermal area on the Snæfellsnes Peninsula, West Iceland. The presence of HCO<sub>3</sub> and Ca in the geothermal fluids is related to chemical-physical processes linked to fluid–rock interaction that occurs in the geothermal reservoir made up of tholeiitic basalt, by fluids enriched in CO<sub>2</sub> of deep origin (i.e. magmatic). Travertine deposits consist of mounds and slopes, which are still in formation and overlie the silica sinter deposits. Both sinter and travertine deposits derive from thermal springs aligned according to two trends: NNE-SSW and WNW-ESE. This evidence suggests the occurrence of buried, permeable, and thus active faults, which control the circulation of fluids containing HCO<sub>3</sub> and Ca. Faults are near parallel to those which define the rift systems and transform zones in Iceland, and probably comprise the still active sector of the abandoned transform zone that, starting with the Snæfellsnes Peninsula, interrupts eastward the northern continuation of the western and eastern rift-zones in the south-central Iceland. In this setting, we refer, for the first time, travertine and silica sinter deposition to an oceanic active crustal structure.
DOI: 10.6084/m9.figshare.22134842.v2
title: Tectonic control on travertine and silica sinter deposition in oceanic transform-fault setting: the case of the Lýsuskarð volcano-geothermal area, Snæfellsnes Peninsula, Iceland

description: Deposition of terrestrial carbonate (i.e. travertine) and silica sinter in geothermal areas is always closely linked to the presence of relevant crustal structures which enhance the permeability in the upper crust favouring the upflow of fluids to the surface. Most travertine deposits are originated by geothermal fluids stored within carbonate reservoirs in continental crust, and their morphology and areal distribution provide useful information on geometry, kinematics, and age of faults which control the fluid flow. In this paper, we focus on the tectonic control on a travertine depositional system, associated with silica sinter, developing in oceanic crust, in the Lýsuskarð volcano-geothermal area on the Snæfellsnes Peninsula, West Iceland. The presence of HCO<sub>3</sub> and Ca in the geothermal fluids is related to chemical-physical processes linked to fluid–rock interaction that occurs in the geothermal reservoir made up of tholeiitic basalt, by fluids enriched in CO<sub>2</sub> of deep origin (i.e. magmatic). Travertine deposits consist of mounds and slopes, which are still in formation and overlie the silica sinter deposits. Both sinter and travertine deposits derive from thermal springs aligned according to two trends: NNE-SSW and WNW-ESE. This evidence suggests the occurrence of buried, permeable, and thus active faults, which control the circulation of fluids containing HCO<sub>3</sub> and Ca. Faults are near parallel to those which define the rift systems and transform zones in Iceland, and probably comprise the still active sector of the abandoned transform zone that, starting with the Snæfellsnes Peninsula, interrupts eastward the northern continuation of the western and eastern rift-zones in the south-central Iceland. In this setting, we refer, for the first time, travertine and silica sinter deposition to an oceanic active crustal structure.
DOI: 10.6084/m9.figshare.22274792.v1
title: Petrological and geochemical evidence for partial melting and melt-rock interaction in mantle rocks from the eastern part of the Sabzevar ophiolite, NE Iran

description: The Sabzevar ophiolite is the most extensive and best-exposed section of oceanic lithosphere in NE Iran. In this study, we examined the mantle section of the eastern part of the Sabzevar ophiolite, where mantle peridotites are the most widespread rock type and are crosscut by pyroxenite veins and mafic dykes. Major and trace element compositions (minerals and whole-rock) of lherzolites are akin to those of abyssal peridotites from mid-ocean ridges (MOR), whereas those of harzburgites evidence formation in a supra-subduction zone (SSZ) setting. Rare-earth element (REE) patterns of whole-rock and clinopyroxene of lherzolites and harzburgites suggest polybaric melting, with initial melting in the garnet peridotite field (~5–6%), followed by ~5–15% melting for lherzolites and ~10–20% for harzburgites in the spinel peridotite field. Harzburgites show LREE enrichment incompatible with partial melting models, indicating significant interaction with SSZ-related melts, whereas analysed lherzolites experienced limited melt-rock interaction. Pyroxene dissolution and olivine precipitation in residual peridotites resulting from reaction with island arc tholeiite and/or boninite melts led to the formation of dunites. These melts eventually intruded as dykes and veins in the mantle and crustal sections of the ophiolite. In addition, boninite melts are inferred to be responsible for forming olivine pyroxenite veins within the harzburgites. We conclude that the mantle section of the Sabzevar ophiolite formed in an intra-oceanic arc setting and experienced a geochemical evolution from a MOR-like to SSZ setting. The intra-oceanic subduction of the Neotethys oceanic lithosphere and shifting conditions of melting during the development of subduction beneath the incipient island arc were responsible for the geochemical heterogeneity of mantle peridotites and the generation of SSZ-related magmas within the Sabzevar oceanic lithosphere.
DOI: 10.6084/m9.figshare.22283696
title: Neogene uplift and deformation in the northeastern Bird’s Head Peninsula, West Papua, Indonesia: consequences of oblique plate convergence

description: Since ~ 25 Ma ago the plate margin between the Australian plate and the Philippine Sea and Pacific-Caroline plates in northwestern New Guinea has been undergoing oblique convergence and resulted in various uplifts and compressional deformation in the Bird’s Head Peninsula. These reflect partitioning into north-northeast compression and east-west sinistral strike-slip faulting analogous to that in the Sumatran active margin. We present new data on the provenance of the upper Miocene to lower Pliocene succession in the northeastern Bird’s Head Peninsula and its structure that has enabled a new tectonic synthesis. Initiation of oblique convergence resulted in development of the sinistral strike-slip Sorong Fault and docking of the Oligocene Arfak Volcanics from the southern Philippine Sea Plate. At ~ 15–12 Ma the compressional component initiated 40 km of dextral offset of the Sorong Fault along the northwest-trending Ransiki Fault. Subsequently, sinistral movement along the Sorong Fault was impeded by formation of a restraining bend at the Ransiki Fault, with uplift shown by the provenance of the local upper Miocene to lower Pliocene conglomerates. Further compressional deformation in the late Pliocene to Pleistocene caused widespread uplift and folding in the adjacent upper Miocene to lower Pliocene succession.
DOI: 10.6084/m9.figshare.22268429
title: Depositional response to the Emeishan mantle plume: evidence from the eastern Sichuan Basin, South China

description: The Emeishan large igneous province (ELIP) is among the prominent large igneous provinces in the world and has been associated with mantle plume activity. In this study we investigated the impact of the Emeishan mantle plume on generating the sedimentary rock suites of the eastern Sichuan Basin. We present petrology, detrital zircon U – Pb ages, trace elements, and Hf isotopic compositions of the Middle-Late Permian sedimentary sequences in the Huayingshan region to constrain the provenance and characterize the depositional response to the Emeishan mantle plume activity. The detrital zircon U – Pb ages of the Middle Permian Maokou Formation indicate that terrigenous detritus was mainly sourced from the Kangdian paleoland in the southwestern margin of South China. Detrital zircon grains from the bottom of the Late Permian Longtan Formation yield a lower intercept age of 257 ± 28 Ma, interpreted as the contemporaneous metamorphism related to the ELIP magma. The detrital zircon U – Pb ages of the middle part of the Longtan Formation are characterized by unimodal age spectra with a peak at 259 Ma. Provenance analysis indicates that the Longtan Formation was mainly sourced from the Emeishan volcanic rocks in the Huayingshan region. We propose that the Kangdian paleohigh may have been regionally uplifted as the result of the pre-eruption rise of the Emeishan mantle plume in the late Middle Permian. Moreover, this paleohigh was translated into a denuded zone and provided voluminous detritus into the eastern Sichuan Basin. In the early Late Permian, the ELIP magmas upwelled and outpoured from the Huayingshan fault, and flowed past the peripheral rocks to the low terrain in the Huayingshan region. The ELIP volcanic rocks in the Huayingshan region underwent intense post-eruption erosion, resulting in the deposition of voluminous volcanic detritus in the eastern Sichuan Basin.