cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.28630430.v1
title: Revision of <i>Dinosorex</i> (Heterosoricidae, Eulipotyphla), with special reference to Slovak and Swiss material

description: <i>Dinosorex</i> is an emblematic representative of the European Miocene small mammal community. Despite a relatively well-known fossil record, previous works pointed out the ambiguous definition of several species, accentuating the need for a taxonomic revision. The present work provides a comprehensive study of the highly specialised heterosoricid genus <i>Dinosorex</i>, including the description of well-preserved Slovak material from Devínska Nová Ves – Bonanza (MN6), Borský Svätý Jur (MN9), Studienka A (MN9), and Pezinok (MN10). The use of micro-computed tomography has shed light on the peculiarities of the basal <i>Dinosorex zapfei</i>, and material from numerous localities have been compared and restudied. As a result, we provide here an updated morphological comparison of all <i>Dinosorex</i> species and discuss the variability and resolving power of all morphological and morphometrical features used in the taxonomy of the genus. Our phylogenetic reconstruction confirms the strong role of geological basins in the evolutionary history of <i>Dinosorex</i>. The detailed study of European and Anatolian <i>Dinosorex</i> material led to the identification of a new species, <i>Dinosorex kaelini</i> sp. nov. from the Swiss locality of Nebelbergweg (MN9). The history of <i>Dinosorex</i> is driven by local evolution and dietary specialisation, which led to a trophic dead end in the earliest Turolian.
DOI: 10.6084/m9.figshare.27179377
title: Post-cranial remains of Rhinocerotidae from the Neogene of central Myanmar: morphological descriptions and comparisons with ratios

description: New post-cranial remains from the early Late Miocene have been discovered in the lowermost part of the Irrawaddy Formation, Tebingan area, central Myanmar. Three genera and one indeterminate taxon were identified: <i>Rhinoceros</i> sp. <i>Rhinoceros</i> cf. <i>R. sondaicus</i>, <i>Dicerorhinus</i> sp., <i>Brachypotherium perimense</i>, and Rhinocerotidae indet. The evolutionary history of the Rhinocerotidae is still poorly known in Southeast Asia. Few <i>Rhinoceros</i> species, <i>Rhinoceros</i> sp. ‘<i>B</i>’. <i>fatehjangense</i>, and <i>B. perimense</i>, has already been identified in the Tebingan area by dental remains. The present discovery of the post-cranial remains of <i>Rhinoceros</i> cf. <i>R. sondaicus</i> and <i>Dicerorhinus</i> sp. that complements previous studies based on dental remains. The early Late Miocene Tebingan record is the oldest fossil record of <i>Dicerorhinus</i> in Southeast Asia, indicating a continental origin of the genus. Furthermore, the possible presence of <i>R. sondaicus</i> in the Tebingan area suggests that it may have appeared in Southeast Asia as early as the early Late Miocene.
DOI: 10.6084/m9.figshare.27179377.v1
title: Post-cranial remains of Rhinocerotidae from the Neogene of central Myanmar: morphological descriptions and comparisons with ratios

description: New post-cranial remains from the early Late Miocene have been discovered in the lowermost part of the Irrawaddy Formation, Tebingan area, central Myanmar. Three genera and one indeterminate taxon were identified: <i>Rhinoceros</i> sp. <i>Rhinoceros</i> cf. <i>R. sondaicus</i>, <i>Dicerorhinus</i> sp., <i>Brachypotherium perimense</i>, and Rhinocerotidae indet. The evolutionary history of the Rhinocerotidae is still poorly known in Southeast Asia. Few <i>Rhinoceros</i> species, <i>Rhinoceros</i> sp. ‘<i>B</i>’. <i>fatehjangense</i>, and <i>B. perimense</i>, has already been identified in the Tebingan area by dental remains. The present discovery of the post-cranial remains of <i>Rhinoceros</i> cf. <i>R. sondaicus</i> and <i>Dicerorhinus</i> sp. that complements previous studies based on dental remains. The early Late Miocene Tebingan record is the oldest fossil record of <i>Dicerorhinus</i> in Southeast Asia, indicating a continental origin of the genus. Furthermore, the possible presence of <i>R. sondaicus</i> in the Tebingan area suggests that it may have appeared in Southeast Asia as early as the early Late Miocene.
DOI: 10.6084/m9.figshare.26616137
title: They all floated in the cretaceous: new rebbachisaurid (Sauropoda, Diplodocoidea) with a highly pneumatized skeleton from the Upper Cretaceous (lower Cenomanian) of Patagonia, Argentina

description: Rebbachisaurids are a group of basal diplodocoid sauropods that diversified primarily in Gondwana between the early Lower Cretaceous and the early Upper Cretaceous. Their phylogenetic relationships are still under debate given the fragmentary and incomplete nature of its remains. Here, we provide a detailed description of the postcranial remains of <i>Campananeyen fragilissimus</i> gen. et sp. nov. from the Candeleros Formation (lower Cenomanian) of Neuquén Province, Argentina. <i>Campananeyen</i> presents notable features that allow it to be recognised as a new species by the presence of an underdeveloped crista prootica, paraoccipital process internally hollow and a fuse dorsal alar arm of the ilium. The phylogenetic analysis recovered this taxon as a basal rebbachisaurid closely related to <i>Zapalasaurus</i>, <i>Sidersaura</i> and the specimen from La Amarga Formation MACN-Pv-N 35. The new rebbachisaurid is recovered as the sister taxon of <i>Sidersaura</i> due the presence of procoelous posterior caudal vertebrae and dorsoventrally flattened posterior caudal centra. <i>C.</i> <i>fragilissimus</i> presents an extreme pneumatization of the sacral region with an autapomorphic dorsal alar arm of the sacral transverse processes. Finally, the phylogenetic analysis supports a South American origin for Rebbachisauridae and an early diversification to Africa and Europe by the Barremian-Aptian as previously suggested.
DOI: 10.6084/m9.figshare.26616137.v1
title: They all floated in the cretaceous: new rebbachisaurid (Sauropoda, Diplodocoidea) with a highly pneumatized skeleton from the Upper Cretaceous (lower Cenomanian) of Patagonia, Argentina

description: Rebbachisaurids are a group of basal diplodocoid sauropods that diversified primarily in Gondwana between the early Lower Cretaceous and the early Upper Cretaceous. Their phylogenetic relationships are still under debate given the fragmentary and incomplete nature of its remains. Here, we provide a detailed description of the postcranial remains of <i>Campananeyen fragilissimus</i> gen. et sp. nov. from the Candeleros Formation (lower Cenomanian) of Neuquén Province, Argentina. <i>Campananeyen</i> presents notable features that allow it to be recognised as a new species by the presence of an underdeveloped crista prootica, paraoccipital process internally hollow and a fuse dorsal alar arm of the ilium. The phylogenetic analysis recovered this taxon as a basal rebbachisaurid closely related to <i>Zapalasaurus</i>, <i>Sidersaura</i> and the specimen from La Amarga Formation MACN-Pv-N 35. The new rebbachisaurid is recovered as the sister taxon of <i>Sidersaura</i> due the presence of procoelous posterior caudal vertebrae and dorsoventrally flattened posterior caudal centra. <i>C.</i> <i>fragilissimus</i> presents an extreme pneumatization of the sacral region with an autapomorphic dorsal alar arm of the sacral transverse processes. Finally, the phylogenetic analysis supports a South American origin for Rebbachisauridae and an early diversification to Africa and Europe by the Barremian-Aptian as previously suggested.
DOI: 10.6084/m9.figshare.27179380
title: Dental morphology evolution in early peratheriines, including a new morphologically cryptic species and findings on the largest early Eocene European metatherian

description: The initial stages of the evolutionary history of peratheriines, the European herpetotheriid metatherians, are largely unknown, primarily due to their limited morphological dental disparity throughout the Palaeogene, coupled with significant intraspecific variation. Based on eleven molars, we document a new early peratheriine species, <i><b>Peratherium musivum</b></i> <b>sp. nov</b>. which is larger than and morphologically similar to the earliest peratheriine, <i>Peratherium constans</i> (MP7). Subtle molar characters are shared with the largest early Eocene peratheriine, <i><b>Peratherium</b></i> <b><i>maximum</i> comb. nov</b>. We illustrate the importance of studying possible changes in molar cusp – basin proportions and correlated characters that occured during peratheriine evolution. <i>Peratherium musivum</i> sp. nov. which spanned only part of the MP7-MP8 + 9 time interval, and the ~MP8 + 9 <i>Peratherium maximum</i> comb. nov. were probably widespread in Western Europe. The description of a well-preserved mandible of the latter, from La Borie (~MP8 + 9), reveals original features concerning relative size and shape of dental alveoli, partly corroborated using isolated molars. These traits are absent in the younger, most representative species of both peratheriine genera, <i>Peratherium</i> and <i>Amphiperatherium</i>. Based on the aforementioned data and a critical review, it is demonstrated that peratheriine genera lack consistent definitions, so that the <i>Peratherium</i>/<i>Amphiperatherium</i> dichotomy is plausibly inapplicable to early Eocene representatives. This article is registered in ZooBank under urn:lsid:zoobank.org:pub:A2B4DE58-855C-4CB8-BC1D-C9677E6DF97D
DOI: 10.6084/m9.figshare.27179380.v2
title: Dental morphology evolution in early peratheriines, including a new morphologically cryptic species and findings on the largest early Eocene European metatherian

description: The initial stages of the evolutionary history of peratheriines, the European herpetotheriid metatherians, are largely unknown, primarily due to their limited morphological dental disparity throughout the Palaeogene, coupled with significant intraspecific variation. Based on eleven molars, we document a new early peratheriine species, <i><b>Peratherium musivum</b></i> <b>sp. nov</b>. which is larger than and morphologically similar to the earliest peratheriine, <i>Peratherium constans</i> (MP7). Subtle molar characters are shared with the largest early Eocene peratheriine, <i><b>Peratherium</b></i> <b><i>maximum</i> comb. nov</b>. We illustrate the importance of studying possible changes in molar cusp – basin proportions and correlated characters that occured during peratheriine evolution. <i>Peratherium musivum</i> sp. nov. which spanned only part of the MP7-MP8 + 9 time interval, and the ~MP8 + 9 <i>Peratherium maximum</i> comb. nov. were probably widespread in Western Europe. The description of a well-preserved mandible of the latter, from La Borie (~MP8 + 9), reveals original features concerning relative size and shape of dental alveoli, partly corroborated using isolated molars. These traits are absent in the younger, most representative species of both peratheriine genera, <i>Peratherium</i> and <i>Amphiperatherium</i>. Based on the aforementioned data and a critical review, it is demonstrated that peratheriine genera lack consistent definitions, so that the <i>Peratherium</i>/<i>Amphiperatherium</i> dichotomy is plausibly inapplicable to early Eocene representatives. This article is registered in ZooBank under urn:lsid:zoobank.org:pub:A2B4DE58-855C-4CB8-BC1D-C9677E6DF97D
DOI: 10.6084/m9.figshare.27179380.v1
title: Dental morphology evolution in early peratheriines, including a new morphologically cryptic species and findings on the largest early Eocene European metatherian

description: The initial stages of the evolutionary history of peratheriines, the European herpetotheriid metatherians, are largely unknown, primarily due to their limited morphological dental disparity throughout the Palaeogene, coupled with significant intraspecific variation. Based on eleven molars, we document a new early peratheriine species, <i><b>Peratherium musivum</b></i> <b>sp. nov</b>. which is larger than and morphologically similar to the earliest peratheriine, <i>Peratherium constans</i> (MP7). Subtle molar characters are shared with the largest early Eocene peratheriine, <i><b>Peratherium</b></i> <b><i>maximum</i> comb. nov</b>. We illustrate the importance of studying possible changes in molar cusp – basin proportions and correlated characters that occured during peratheriine evolution. <i>Peratherium musivum</i> sp. nov. which spanned only part of the MP7-MP8 + 9 time interval, and the ~MP8 + 9 <i>Peratherium maximum</i> comb. nov. were probably widespread in Western Europe. The description of a well-preserved mandible of the latter, from La Borie (~MP8 + 9), reveals original features concerning relative size and shape of dental alveoli, partly corroborated using isolated molars. These traits are absent in the younger, most representative species of both peratheriine genera, <i>Peratherium</i> and <i>Amphiperatherium</i>. Based on the aforementioned data and a critical review, it is demonstrated that peratheriine genera lack consistent definitions, so that the <i>Peratherium</i>/<i>Amphiperatherium</i> dichotomy is plausibly inapplicable to early Eocene representatives. This article is registered in ZooBank under urn:lsid:zoobank.org:pub:A2B4DE58-855C-4CB8-BC1D-C9677E6DF97D
DOI: 10.15468/dl.8wnx8z
title: Occurrence Download

description: A dataset containing 291335 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Centropus sinensis (Stephens, 1815), Chrysococcyx maculatus (Gmelin, 1788), Chrysococcyx xanthorhynchus (Horsfield, 1821), Clamator coromandus (Linnaeus, 1766), Clamator jacobinus (Boddaert, 1783), Cuculus canorus Linnaeus, 1758, Cuculus micropterus Gould, 1838, Cuculus optatus Gould, 1845, Cuculus poliocephalus Latham, 1790, Cuculus saturatus Blyth, 1843, Eudynamys scolopaceus (Linnaeus, 1758), Cuculus hyperythrus Gould, 1856, Cuculus nisicolor Blyth, 1843, Cuculus sparverioides Vigors, 1832, Cuculus varius Vahl, 1797, Rhopodytes tristis (Lesson, 1830), Surniculus lugubris (Horsfield, 1821), Falco amurensis Radde, 1863, Falco cherrug J.E.Gray, 1834, Falco columbarius Linnaeus, 1758, Falco naumanni J.G.Fleischer, 1818, Falco peregrinus Tunstall, 1771, Falco rusticolus Linnaeus, 1758, Falco severus Horsfield, 1821, Falco subbuteo Linnaeus, 1758, Falco tinnunculus Linnaeus, 1758, Falco vespertinus Linnaeus, 1766, Microhierax caerulescens (Linnaeus, 1758), Microhierax melanoleucos (Blyth, 1843), Alectoris chukar (J.E.Gray, 1830), Alectoris magna (Przewalski, 1876), Arborophila ardens (Styan, 1892), Arborophila atrogularis (Blyth, 1849), Arborophila brunneopectus (Blyth, 1855), Arborophila crudigularis (Swinhoe, 1864), Arborophila gingica (J.F.Gmelin, 1789), Arborophila mandellii Hume, 1874, Arborophila rufipectus Boulton, 1932, Arborophila rufogularis (Blyth, 1849), Arborophila torqueola (Valenciennes, 1825))",
 "Geometry POLYGON((73.5208333 16.6625,135.0791667 16.6625,135.0791667 53.5541667,73.5208333 53.5541667,73.5208333 16.6625))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "BasisOfRecord is one of (Human Observation, Specimen)",
 "Country is one of (China, Hong Kong, Macao, Chinese Taipei)"
 ]
}

 The dataset includes 291335 records from 55 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0007916-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.bnfbdt
title: Occurrence Download

description: A dataset containing 33 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-76.9855 4.50455,-63.3442 4.43073,-66.23252 12.52598,-70.36514 13.16605,-78.22113 12.32805,-76.9855 4.50455))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Triplaris purdiei Meisn."
 ]
}

 The dataset includes 33 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0001637-250426092105405/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25549/inscriptifact-ouc110806564
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes
DOI: 10.25549/inscriptifact-ouc110807293
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes
DOI: 10.25549/inscriptifact-ouc110806552
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes
DOI: 10.25549/inscriptifact-ouc110807301
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes
DOI: 10.25549/inscriptifact-ouc110806537
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes
DOI: 10.17632/79hfr2sc6s
title: Remote Sensing Ecological Index (RSEI) raster data for the ecological restoration belt in the southeastern karst region of Southwest China

description: This dataset comprises annual Remote Sensing Ecological Index (RSEI) raster data for the ecological restoration belt in the southeastern karst region of Southwest China, spanning the period from 2000 to 2022. The dataset has a spatial resolution of 500 meters and is designed to provide a comprehensive assessment of the spatiotemporal dynamics of the Ecological Environment Quality (EEQ) in the study area.
The RSEI is a composite index that integrates four key remote sensing indicators through Principal Component Analysis (PCA):
Greenness Indicator: Normalized Difference Vegetation Index (NDVI), reflecting vegetation cover.
Wetness Indicator: The wetness component (WET) from the Tasseled Cap Transformation, representing the moisture content of soil and vegetation.
Dryness Indicator: Normalized Difference Built-up and Soil Index (NDBSI), indicating the degree of surface dryness influenced by built-up areas and bare soil.
Heat Indicator: Land Surface Temperature (LST), reflecting the surface thermal environment.
All original remote sensing imagery (MOD09A1, MOD13A1, MOD11A2, MOD17A3HGF) was sourced from the National Aeronautics and Space Administration's (NASA) Earth Observing System Data and Information System (EOSDIS). This study utilized the Google Earth Engine (GEE) platform for the systematic processing of these multi-source remote sensing data. The process included image mosaicking, cloud removal, gap-filling, atmospheric correction, and topographic correction to ultimately compute the 23-year annual RSEI time-series data covering the entire study area.
This dataset is a core output of the paper titled "Diagnostic Adaptive Assessment Framework (DAAF-Karst): Revealing the Heterogeneous Mechanisms of Ecological Evolution in the Karst Region of Southwest China." It provides a critical data foundation for an in-depth analysis of the ecological restoration and degradation processes, decoupling their complex driving mechanisms, and formulating precise adaptive management strategies for this ecologically fragile region.
DOI: 10.25549/inscriptifact-ouc110649989
title: Persepolis Fortification Elamite Tablet 0576.101, Fort 0576.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 0576.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on left edge. ❧ [Physical Object Note:] Wear on right side of obverse, right edge broken off.
DOI: 10.25549/inscriptifact-ouc110806540
title: Mesha Inscription, KAI 181, Mesha' Inscription, Mesha'-Inschrift, Mesha Stela, Mesha' Stela

description: [Text Description:] Commemoration of military actions and building projects of Mesha, King of Moab ❧ [Text or Publication Number Note:] KAI 181 ❧ [Excavation Description:] Discovered in 1868 by a German missionary in Diban (Dhiban) ❧ [Medium:] Stone ❧ [Script Note:] Moabite ❧ [Physical Object Description:] Basalt Stone, 1.1 meters high, 60-68 cm wide (or 1.15 m x 60 cm), rounded at the top ❧ [Physical Object Note:] Present stele has been restored from fragments, and missing text reconstructed based on paper squeezes