cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.18712/nsd-nsd0959-1-v1
title: KEU Pre-survey 2003

description: Oxford Research conducts customer impact surveys for Innovation Norway (IN) in collaboration with Social and Business Research (SNF). The surveys include companies that have received services from Innovation Norway in the years from and including 2003. For each year, a pre-survey is conducted one year after the service was given and a follow-up survey four years later.

Innovation Norway offers products and services that will contribute to developing the districts, increasing innovation in business throughout the country and profiling Norwegian business and Norway as a destination.

The purpose of the customer impact surveys is twofold. First, there is an internal purpose that involves improving and further developing Innovation Norway’s activities. Second, there is an external purpose that answers the question “what have we got for our money?”.

The survey covers the following areas:

General about the project for which support is sought
Organization and implementation of establishment
Innovation Norway’s support’s importance for strategy, competence and network
Innovation Norway’s support’s results and effects
General about Innovation Norway
Background information

Innovation Norway was established on January 1, 2004, and is a merger of former SND, Norwegian Export Council, Norwegian Tourist Board and State Guidance Office for Inventors.
DOI: 10.6084/m9.figshare.23650860
title: A trophic metaweb of benthic ecosystems of South Korean streams and rivers

description: The metaweb is a dictionary of nodes and their potential interactions developed for a particular region focusing on particular kinds of ecosystem. Based on local biodiversity information, the metaweb can be easily decomposed to local webs to understand the local level ecological interactions. This data provides a metaweb developed for benthic ecosystem of South Korean streams and rivers. Maximum taxonomic resolution of the metaweb is set at genus level. GBIF backbone taxonomy was followed for classification and nomenclature. Then interactions for the nodes were searched from 624 different scientific literature. When same set of interactions for all members belongs to that taxonomic category, those nodes were merged into higher taxonomic level. Total 452 nodes and 25,645 interactions were included in the metaweb. Most of the nodes are represented by macroinvertebrates (63.7%) followed by fishes (22.3%) and microalgae (13%). Most of the interaction in this metaweb is originated from macroinvertebrates (83%), i.e., where macroinvertebrates are resource. This metaweb can be used to understand spatiotemporal change of food webs of South Korean streams and causal factors behind it. Apart from that, this metaweb will enrich the global understanding about ecological interaction.
DOI: 10.6084/m9.figshare.23650860.v2
title: A trophic metaweb of benthic ecosystems of South Korean streams and rivers

description: The metaweb is a dictionary of nodes and their potential interactions developed for a particular region focusing on particular kinds of ecosystem. Based on local biodiversity information, the metaweb can be easily decomposed to local webs to understand the local level ecological interactions. This data provides a metaweb developed for benthic ecosystem of South Korean streams and rivers. Maximum taxonomic resolution of the metaweb is set at genus level. GBIF backbone taxonomy was followed for classification and nomenclature. Then interactions for the nodes were searched from 624 different scientific literature. When same set of interactions for all members belongs to that taxonomic category, those nodes were merged into higher taxonomic level. Total 452 nodes and 25,645 interactions were included in the metaweb. Most of the nodes are represented by macroinvertebrates (63.7%) followed by fishes (22.3%) and microalgae (13%). Most of the interaction in this metaweb is originated from macroinvertebrates (83%), i.e., where macroinvertebrates are resource. This metaweb can be used to understand spatiotemporal change of food webs of South Korean streams and causal factors behind it. Apart from that, this metaweb will enrich the global understanding about ecological interaction.
DOI: 10.6084/m9.figshare.23650860.v1
title: A trophic metaweb of benthic ecosystems of South Korean streams and rivers

description: The metaweb is a dictionary of nodes and their potential interactions developed for a particular region focusing on particular kinds of ecosystem. Based on local biodiversity information, the metaweb can be easily decomposed to local webs to understand the local level ecological interactions. This data provides a metaweb developed for benthic ecosystem of South Korean streams and rivers. Maximum taxonomic resolution of the metaweb is set at genus level. GBIF backbone taxonomy was followed for classification and nomenclature. Then interactions for the nodes were searched from 624 different scientific literature. When same set of interactions for all members belongs to that taxonomic category, those nodes were merged into higher taxonomic level. Total 452 nodes and 25,645 interactions were included in the metaweb. Most of the nodes are represented by macroinvertebrates (63.7%) followed by fishes (22.3%) and microalgae (13%). Most of the interaction in this metaweb is originated from macroinvertebrates (83%), i.e., where macroinvertebrates are resource. This metaweb can be used to understand spatiotemporal change of food webs of South Korean streams and causal factors behind it. Apart from that, this metaweb will enrich the global understanding about ecological interaction.
DOI: 10.6084/m9.figshare.21714845
title: Neogene drainage reorganization of the Longzhong Basin driven by growth of the NE Tibetan Plateau: A Sr isotope hydrological perspective

description: Table S1 Elemental and Sr isotopic compositions of carbonate and soluble salt in the YD section; Table S2 Elemental and Sr isotopic compositions of carbonate in the DHJ section; Table S3 Sr isotopic compositions of modern river water in Lanzhou and Xunhua basins
DOI: 10.6084/m9.figshare.21714845.v2
title: Neogene drainage reorganization of the Longzhong Basin driven by growth of the NE Tibetan Plateau: A Sr isotope hydrological perspective

description: Table S1 Elemental and Sr isotopic compositions of carbonate and soluble salt in the YD section; Table S2 Elemental and Sr isotopic compositions of carbonate in the DHJ section; Table S3 Sr isotopic compositions of modern river water in Lanzhou and Xunhua basins
DOI: 10.6084/m9.figshare.21714845.v1
title: Neogene drainage reorganization of the Longzhong Basin driven by growth of the NE Tibetan Plateau: A Sr isotope hydrological perspective

description: Table S1 Elemental and Sr isotopic compositions of carbonate and soluble salt in the YD section; Table S2 Elemental and Sr isotopic compositions of carbonate in the DHJ section; Table S3 Sr isotopic compositions of modern river water in Lanzhou and Xunhua basins
DOI: 10.15454/clyps4/99nxxb
title: Readme_EMMAH.txt

description: Description des informations sur l'origine et les responsables des données.
DOI: 10.15454/clyps4/t4vbsq
title: BDD_Phetec_EMMAH.tab

description: Données de phénologie et metadonnées associées. Phenology data and associated metadata
DOI: 10.15454/clyps4/cqfuo1
title: BDD_Phetec_EMMAH.tab

description: Données de phénologie et metadonnées associées. Phenology data and associated metadata
DOI: 10.57745/3t2mo1
title: Readme_EMMAH_EN.txt

description: "Read me" file
DOI: 10.57745/cq2jgr
title: BDD_Phetec_EMMAH_INRAE_TEMPO.xlsx

description: TEMPO file
DOI: 10.57745/ypujre
title: Lisez_moi_EMMAH_FR.txt

description: Fichier "Lisez moi"
DOI: 10.6084/m9.figshare.20308395
title: Höwenegg <i>Hippotherium primigenium</i>: geological context, cranial and postcranial morphology, palaeoecological and biogeographic importance

description: Höwenegg is an early Vallesian (MN9, 10.3 Ma) vertebrate locality in Hegau, Southwest Germany renowned for its preservation of complete mammalian skeletons, diverse invertebrate and plant fossils. We provide the first to be published photographic images of the Höwenegg <i>Hippotherium primigenium</i> skulls, mandibles and dentitions for describing critical character states used to define hipparion species. We compare these states to those for North American <i>Cormohipparion occidentale</i>, Turkish <i>Cormohipparion sinapensis</i> Algerian ‘<i>Cormohipparion</i>’ <i>africanum</i>, Austrian Pannonian C <i>Hippotherium</i> sp., Austrian locality Inzersdorf <i>Hippotherium primigenium</i>, the China type specimens of <i>Hippotherium weihoense</i> and ‘<i>Hipparion</i>’ <i>chiai</i>, and Moldovan <i>Cremohipparion moldavicum</i>. Also provided are univariate statistical comparisons of cranial-dental characters and Log10 ratio analyses of third metapodials dimensions to better evaluate taxonomic comparisons and define the genetic pool from which Old World hipparions are derived. We concur with previous authors that North American <i>Cormohipparion</i> is the likely source of first occurring Old World hipparions offering alternatives of <i>Cormohipparion occidentale</i> or <i>Cormohipparion quinni</i> as the most closely related species for the Old World <i>Cormohipparion</i> Datum. We find that the best evidence for the chronology of the <i>Cormohipparion</i> Datum suggests and age of 11.4–11.0 Ma, or 11.2–11.1 Ma rather than the 11.5 Ma datum recently alleged for China.
DOI: 10.6084/m9.figshare.20210733
title: Taphonomical and palaeoenvironmental analyses of the microvertebrate fossil material from the Late Pleistocene cave of Kalamakia (Mani peninsula), Greece

description: The present study focuses on the microvertebrate fossil material retrieved from the three fossiliferous units of Kalamakia cave dating from ca. 90–25 kya BP, to identify the accumulation agents of the assemblage and the processes that affected it post-depositionally. This was done through the quantification of specific indices described in the literature concerning breakage, digestion and other types of modifications observed upon the surface of the specimens. Furthermore, the Taxonomic Habitat Index was calculated to reconstruct the possible habitat types in the surrounding area. Regarding the results on taphonomy, significant amounts of post-depositional breakage were observed, possibly resulting from trampling and, secondarily, modifications from the occasionally naturally occurring high humidity within a cave. The main accumulators of the microvertebrate assemblage seem to have been barn owls either independently or jointly with long-eared owls and/or owlets. Concerning the habitats possibly present in the area, the existence of mixed habitats varying between relative expansions of shrublands, grasslands, rocky areas and (limited) deciduous forests was identified, while the occasional presence of water bodies was also revealed. Shifts between the percentages of different habitats were not great but could be correlated with climatic events within a geochronological context.
DOI: 10.6084/m9.figshare.20308395.v1
title: Höwenegg <i>Hippotherium primigenium</i>: geological context, cranial and postcranial morphology, palaeoecological and biogeographic importance

description: Höwenegg is an early Vallesian (MN9, 10.3 Ma) vertebrate locality in Hegau, Southwest Germany renowned for its preservation of complete mammalian skeletons, diverse invertebrate and plant fossils. We provide the first to be published photographic images of the Höwenegg <i>Hippotherium primigenium</i> skulls, mandibles and dentitions for describing critical character states used to define hipparion species. We compare these states to those for North American <i>Cormohipparion occidentale</i>, Turkish <i>Cormohipparion sinapensis</i> Algerian ‘<i>Cormohipparion</i>’ <i>africanum</i>, Austrian Pannonian C <i>Hippotherium</i> sp., Austrian locality Inzersdorf <i>Hippotherium primigenium</i>, the China type specimens of <i>Hippotherium weihoense</i> and ‘<i>Hipparion</i>’ <i>chiai</i>, and Moldovan <i>Cremohipparion moldavicum</i>. Also provided are univariate statistical comparisons of cranial-dental characters and Log10 ratio analyses of third metapodials dimensions to better evaluate taxonomic comparisons and define the genetic pool from which Old World hipparions are derived. We concur with previous authors that North American <i>Cormohipparion</i> is the likely source of first occurring Old World hipparions offering alternatives of <i>Cormohipparion occidentale</i> or <i>Cormohipparion quinni</i> as the most closely related species for the Old World <i>Cormohipparion</i> Datum. We find that the best evidence for the chronology of the <i>Cormohipparion</i> Datum suggests and age of 11.4–11.0 Ma, or 11.2–11.1 Ma rather than the 11.5 Ma datum recently alleged for China.
DOI: 10.6084/m9.figshare.20138827
title: New remains of <i>Eleutherocercus</i> (Xenarthra, Cingulata, Glyptodontidae) from the Pampean and Northwestern regions of Argentina: morphology and phylogeny of late Neogene Doedicurinae

description: The subfamily Doedicurinae is a monophyletic group of glyptodonts with their own anatomical features and is mostly known on the basis of the Pleistocene genus <i>Doedicurus</i>, one of the largest recorded taxa. The most distinctive character of the subfamily, unique within Cingulata, include the absence of ornamentation with large foramina, on the exposed surface of the carapace osteoderms. In terminal forms of the late Pleistocene, osteoderms have large foramina which tend to cross the entire thickness. The knowledge of the late Neogene diversity of the clade, as well as its evolutionary and geographical history, has increased in recent years, with important records in Argentina, where two late Miocene-Pliocene species are recognised: <i>Eleutherocercus solidus</i> from Catamarca and Tucumán provinces, and <i>Eleutherocercus antiquus</i> from Buenos Aires province. The most complete skull of <i>E. antiquus</i> from the early Pliocene Monte Hermoso Formation (ca. 5–4.2 Ma) is reported here. The specimen studied shows a conspicuous pathology on the parietal bones, first reported for fossil cingulates. In addition, the carapace of <i>E. solidus</i> is first described, on the basis of a partially complete specimen from the late Miocene-Pliocene (unknown stratigraphic level) from Tucumán province. Previous phylogenetic hypotheses of the relationships within the Doedicurinae, as well as their relationship with the remaining clades of Glyptodontidae, is tested in this study, adding new synapomorphies to the subfamily. The comparative study suggests that a third species previously proposed (<i>E. paranaensis</i>) from the ‘Mesopotamiense’ (late Miocene, Northeastern region of Argentina), must be considered as <i>Eleutherocercus</i> sp. Since their oldest record in the late Miocene, the latitudinal distribution of the Doedicurinae seems to have expanded rapidly reaching middle latitudes, particularly during the Pliocene, but during the Pleistocene (particularly the final lapse of this period), they began to retract latitudinally.
DOI: 10.6084/m9.figshare.20364413
title: Late Miocene rhinocerotids from the Balkan-Iranian province: ecological insights from dental microwear textures and enamel hypoplasia

description: The late Miocene is a period of increasing aridity and habitat openness in the south-eastern Mediterranean region. The impact of these changes has not been fully explored regarding rhinocerotids’ ecology, although rhinoceroses were a major and diverse component of the Miocene mammalian faunas. Here, we investigate the palaeoecology of rhinocerotid specimens coming from 12 localities throughout the Balkan-Iranian zoogeographic province, and covering a large part of the late Miocene (MN9 to MN13). Microwear textures confirmed the hypothesised niche partitioning between the two main rhinocerotid species – <i>Ceratotherium</i> [<i>Ce</i>.] <i>neumayri</i> (mixed-feeder including grasses) and <i>Dihoplus pikermiensis</i> (browser) – but highlighted dietary overlap between <i>Ce. neumayri</i> and the co-occurring chilothere species at Maragheh, Samos and Pentalophos-1. Although microwear did not reveal clear spatiotemporal differences, we found obvious discrepancies regarding hypoplasia prevalence: Vallesian rhinocerotid teeth displayed more defects (Xirochori and Pentalophos-1: 16.26% of teeth affected) than Turolian specimens (all other localities: 9.72%). Similarly, rhinocerotid teeth from eastern localities (Samos and Maragheh; supposedly more arid), had a higher hypoplasia prevalence (13.52%) than their western counterparts (6.90%). Insights from rhinocerotids’ ecology thus challenged space and time homogeneity within Balkan-Iranian province, and the associated savanna habitat, at least regarding the sample studied here.
DOI: 10.6084/m9.figshare.20364413.v1
title: Late Miocene rhinocerotids from the Balkan-Iranian province: ecological insights from dental microwear textures and enamel hypoplasia

description: The late Miocene is a period of increasing aridity and habitat openness in the south-eastern Mediterranean region. The impact of these changes has not been fully explored regarding rhinocerotids’ ecology, although rhinoceroses were a major and diverse component of the Miocene mammalian faunas. Here, we investigate the palaeoecology of rhinocerotid specimens coming from 12 localities throughout the Balkan-Iranian zoogeographic province, and covering a large part of the late Miocene (MN9 to MN13). Microwear textures confirmed the hypothesised niche partitioning between the two main rhinocerotid species – <i>Ceratotherium</i> [<i>Ce</i>.] <i>neumayri</i> (mixed-feeder including grasses) and <i>Dihoplus pikermiensis</i> (browser) – but highlighted dietary overlap between <i>Ce. neumayri</i> and the co-occurring chilothere species at Maragheh, Samos and Pentalophos-1. Although microwear did not reveal clear spatiotemporal differences, we found obvious discrepancies regarding hypoplasia prevalence: Vallesian rhinocerotid teeth displayed more defects (Xirochori and Pentalophos-1: 16.26% of teeth affected) than Turolian specimens (all other localities: 9.72%). Similarly, rhinocerotid teeth from eastern localities (Samos and Maragheh; supposedly more arid), had a higher hypoplasia prevalence (13.52%) than their western counterparts (6.90%). Insights from rhinocerotids’ ecology thus challenged space and time homogeneity within Balkan-Iranian province, and the associated savanna habitat, at least regarding the sample studied here.
DOI: 10.6084/m9.figshare.20138827.v1
title: New remains of <i>Eleutherocercus</i> (Xenarthra, Cingulata, Glyptodontidae) from the Pampean and Northwestern regions of Argentina: morphology and phylogeny of late Neogene Doedicurinae

description: The subfamily Doedicurinae is a monophyletic group of glyptodonts with their own anatomical features and is mostly known on the basis of the Pleistocene genus <i>Doedicurus</i>, one of the largest recorded taxa. The most distinctive character of the subfamily, unique within Cingulata, include the absence of ornamentation with large foramina, on the exposed surface of the carapace osteoderms. In terminal forms of the late Pleistocene, osteoderms have large foramina which tend to cross the entire thickness. The knowledge of the late Neogene diversity of the clade, as well as its evolutionary and geographical history, has increased in recent years, with important records in Argentina, where two late Miocene-Pliocene species are recognised: <i>Eleutherocercus solidus</i> from Catamarca and Tucumán provinces, and <i>Eleutherocercus antiquus</i> from Buenos Aires province. The most complete skull of <i>E. antiquus</i> from the early Pliocene Monte Hermoso Formation (ca. 5–4.2 Ma) is reported here. The specimen studied shows a conspicuous pathology on the parietal bones, first reported for fossil cingulates. In addition, the carapace of <i>E. solidus</i> is first described, on the basis of a partially complete specimen from the late Miocene-Pliocene (unknown stratigraphic level) from Tucumán province. Previous phylogenetic hypotheses of the relationships within the Doedicurinae, as well as their relationship with the remaining clades of Glyptodontidae, is tested in this study, adding new synapomorphies to the subfamily. The comparative study suggests that a third species previously proposed (<i>E. paranaensis</i>) from the ‘Mesopotamiense’ (late Miocene, Northeastern region of Argentina), must be considered as <i>Eleutherocercus</i> sp. Since their oldest record in the late Miocene, the latitudinal distribution of the Doedicurinae seems to have expanded rapidly reaching middle latitudes, particularly during the Pliocene, but during the Pleistocene (particularly the final lapse of this period), they began to retract latitudinally.
DOI: 10.6084/m9.figshare.20210733.v1
title: Taphonomical and palaeoenvironmental analyses of the microvertebrate fossil material from the Late Pleistocene cave of Kalamakia (Mani peninsula), Greece

description: The present study focuses on the microvertebrate fossil material retrieved from the three fossiliferous units of Kalamakia cave dating from ca. 90–25 kya BP, to identify the accumulation agents of the assemblage and the processes that affected it post-depositionally. This was done through the quantification of specific indices described in the literature concerning breakage, digestion and other types of modifications observed upon the surface of the specimens. Furthermore, the Taxonomic Habitat Index was calculated to reconstruct the possible habitat types in the surrounding area. Regarding the results on taphonomy, significant amounts of post-depositional breakage were observed, possibly resulting from trampling and, secondarily, modifications from the occasionally naturally occurring high humidity within a cave. The main accumulators of the microvertebrate assemblage seem to have been barn owls either independently or jointly with long-eared owls and/or owlets. Concerning the habitats possibly present in the area, the existence of mixed habitats varying between relative expansions of shrublands, grasslands, rocky areas and (limited) deciduous forests was identified, while the occasional presence of water bodies was also revealed. Shifts between the percentages of different habitats were not great but could be correlated with climatic events within a geochronological context.
DOI: 10.6084/m9.figshare.22807238.v2
title: SelfTargeting h5ad data encoded into 912 classes

description: filename is formated as : CellType_Repeat_Coding.h5ad <br> h5ad with event frequency stored in adata.X event description saved in adata.var meta data for each Guide-Target pair saved in adata.obs <br> To download and unzip the file copy the link address within terminal : wget --no-check-certificate LINK within terminal : mv 2 2.zip unzip 2.zip
DOI: 10.15454/jfvdnx/0rwmxf
title: Readme_Ferlus.txt

description: Description des informations sur l'origine et les responsables des données
DOI: 10.5281/zenodo.7758529
title: Laboratory investigation of hydrodynamic and sand dune morphology changes under wave overwash (Version 1)

description: Lab datasets of the experiment
DOI: 10.15454/jfvdnx/q2jz7q
title: BDD_Phetec_Ferlus.tab

description: Données de phénologie et metadonnées associées. Phenology data and associated metadata
DOI: 10.5281/zenodo.7758528
title: Laboratory investigation of hydrodynamic and sand dune morphology changes under wave overwash (Version 1)

description: Lab datasets of the experiment
DOI: 10.57745/9qns5o
title: Readme_Ferlus_EN.txt

description: "Read me" file
DOI: 10.57745/au9qhy
title: Lisezmoi_Ferlus_FR.txt

description: Fichier " Lisez moi"
DOI: 10.57745/tu8kpm
title: BDD_Phetec_Ferlus_INRAE_TEMPO.xlsx

description: TEMPO file