cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.3535/5ba-ew7-qhl
title: Nassarius cadeei H. H. Kool, 2006

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/wtz-fr9-zfb
title: Hiatella arctica (Linnaeus, 1767)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/8pr-cql-c73
title: Atlanta lesueurii J. E. Gray, 1850

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/d3r-5ew-4zd
title: Tritia reticulata (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/4fm-zdk-fxv
title: Conus anemone Lamarck, 1810

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/a1a-m5f-leq
title: Volvulella acuminata (Bruguière, 1792)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/glh-fse-f8r
title: Conasprella puncticulata (Hwass, 1792)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/24z-3rs-85d
title: Vexillum subdivisum (Gmelin, 1791)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/abs-j4y-d7n
title: Rhinoclavis aspera (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/7cw-9zk-rd0
title: Cerithium egenum A. Gould, 1849

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/fqz-ys4-dpp
title: Latiaxis mawae (Gray, 1833)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/qen-enx-sbk
title: Setia H. Adams & A. Adams, 1852

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6sm-93b-1ze
title: Acmaea Eschscholtz, 1833

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/9cl-pkk-92g
title: Crepipatella dilatata (Lamarck, 1822)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/4s9-a3q-q7c
title: Phrontis luteostoma (Broderip & G. B. Sowerby I, 1829)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/vyn-r3v-nzk
title: Patella caerulea Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/7lm-vql-sjz
title: Drupella cornus (Röding, 1798)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6g6-fmp-89b
title: Penion sulcatus (Lamarck, 1816)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/yyq-as9-8vv
title: Caecum armoricum de Folin, 1869

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/kwy-sf9-ppe
title: Chondrina farinesii ascendens (Westerlund, 1878)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/lph-b61-fba
title: Filopaludina sumatrensis (Dunker, 1852)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/2cc-va8-zvt
title: Nassarius callospira (A. Adams, 1852)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/y2b-1yd-kzk
title: Prunum amygdalum (Kiener, 1841)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/5z7-ht8-p17
title: Harpa amouretta Röding, 1798

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6d4-j30-ke4
title: Oxymeris areolata (Link, 1807)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/nnj-2mx-8mb
title: Jujubinus montagui (W. Wood, 1828)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/78h-q6y-dlc
title: Conus omaria Hwass, 1792

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/le9-gsh-mde
title: Monacha syriaca (Ehrenberg, 1831)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/j02-1fj-rgy
title: Perrinia stellata (A. Adams, 1864)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/rb1-d58-pca
title: Conus austroviola Röckel & Korn, 1992

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6n5-tq2-smh
title: Clanculus pharaonius (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/lvj-wjv-vrs
title: Nassarius velatus (A. Gould, 1850)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/zbd-xmb-469
title: Carychium tridentatum (Risso, 1826)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/lpp-9bs-57l
title: Allopeas gracile (T. Hutton, 1834)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/wes-b7s-67p
title: Nerita albicilla Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/kjd-4kv-qfs
title: Neosubulina gloynii (J. S. Gibbons, 1879)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6r3-lx0-0d5
title: Solemya togata (Poli, 1791)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/sjq-x8g-tky
title: Helicella itala (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/3jf-p91-23d
title: Pseudorbis granulum (Brugnone, 1873)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/hqx-p1j-3pm
title: Filifusus filamentosus (Röding, 1798)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/qa6-rsd-zre
title: Pseudolilliconus boschorum (Moolenbeek & Coomans, 1993)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/w2k-fr6-fdq
title: Asaphis deflorata (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/99d-tsz-x0t
title: Cerithium atratum (Born, 1778)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/a9d-c8e-1bn
title: Mauritia arabica arabica (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/bzh-1h7-j56
title: Naria cernica (G. B. Sowerby II, 1870)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/7vv-9h9-lws
title: Acmella sutteri van Benthem Jutting, 1958

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/9rg-pan-jh5
title: Littorina striata P. P. King, 1832

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/cc4-ybp-mdc
title: Babelomurex lischkeanus (Dunker, 1882)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/lpw-e4b-3y1
title: Acteocina knockeri (E. A. Smith, 1872)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/ft1-k76-zxd
title: Conus jaspideus Gmelin, 1791

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/jkt-lth-sa0
title: Neritopsis radula (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/cc7-eag-25c
title: Cerithium caeruleum G. B. Sowerby II, 1855

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6l7-dhn-y60
title: Cecilioides tumulorum (Bourguignat, 1856)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/em2-4jg-bpq
title: Conus planorbis Born, 1778

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/ce5-xp3-2ty
title: Pyrunculus hoernesi (Weinkauff, 1866)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/nrr-t9q-y3d
title: Varicorbula gibba (Olivi, 1792)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/31w-ffz-1fk
title: Subulina octona (Bruguière, 1789)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/zsw-gbl-571
title: Callista erycina (Linnaeus, 1758)

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.6084/m9.figshare.26861064
title: A Comprehensive Review of Hydrocarbon Contaminated Soil Behavior, Geotechnical Properties and Potential Remediation

description: Soil contamination due to urban and industrial activities has caused significant land degradation and changes in the geotechnical properties of soils. Among many contaminants, hydrocarbons pose severe threats not only from an engineering point of view but are also hazardous to the environment. This review article critically analyzes the essential aspects of different hydrocarbon types as a contamination source in various soil types and their implications in the geotechnical design. The modifications of geotechnical properties require an in-depth investigation, especially at the micro-scale, by assessing the soil particle interaction with hydrocarbons. The hydrocarbon compounds possess the ability to alter the morphological characteristics of soil particles, which, in turn, influences the shear mobilization in soils. Furthermore, several remediation techniques, such as biological, chemical, physical, or thermal treatment methods, are available to solidify, remove or immobilize hydrocarbons. However, limitations exist due to the applicability of some techniques. Taking these considerations into account, the primary purpose of this paper is to create a consensus about how hydrocarbons interact with different soils, what are the triggers of these interactions, which geotechnical properties are mostly affected, which remediation techniques will be more effective, and how quickly the method can be applied.
DOI: 10.6084/m9.figshare.26861064.v1
title: A Comprehensive Review of Hydrocarbon Contaminated Soil Behavior, Geotechnical Properties and Potential Remediation

description: Soil contamination due to urban and industrial activities has caused significant land degradation and changes in the geotechnical properties of soils. Among many contaminants, hydrocarbons pose severe threats not only from an engineering point of view but are also hazardous to the environment. This review article critically analyzes the essential aspects of different hydrocarbon types as a contamination source in various soil types and their implications in the geotechnical design. The modifications of geotechnical properties require an in-depth investigation, especially at the micro-scale, by assessing the soil particle interaction with hydrocarbons. The hydrocarbon compounds possess the ability to alter the morphological characteristics of soil particles, which, in turn, influences the shear mobilization in soils. Furthermore, several remediation techniques, such as biological, chemical, physical, or thermal treatment methods, are available to solidify, remove or immobilize hydrocarbons. However, limitations exist due to the applicability of some techniques. Taking these considerations into account, the primary purpose of this paper is to create a consensus about how hydrocarbons interact with different soils, what are the triggers of these interactions, which geotechnical properties are mostly affected, which remediation techniques will be more effective, and how quickly the method can be applied.
DOI: 10.15468/dl.th3pe5
title: Occurrence Download

description: A dataset containing 38 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Aedes unilineatus"
 ]
}

 The dataset includes 38 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0084994-250717081556266/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.29038888
title: Geochemistry characteristics and tectonic significance of the ‘ “mafic” S-type granites’

description: Taking account of their importance in inferring continental geodynamic processes, S-type granites have been the subject of considerable research since their discovery and identification. With their high A/CNK (Mol. Al<sub>2</sub>O<sub>3</sub>/(Na<sub>2</sub>O + K<sub>2</sub>O + CaO) &gt; 1.1) and low Na<sub>2</sub>O (&lt;3.2 wt.%) and MgO + FeO<sup>T</sup> contents (generally with maficity &lt; 4 wt.%), S-type granites were originally considered to be largely derived from partial melting of metasedimentary sources in orogeny zone settings. However, it is hotly debated why many S-type granites show significantly higher maficity [here defined as the weight percent of MgO + FeO<sup>T</sup> up to 12 wt.% and lower silica (SiO<sub>2</sub> &lt;65 wt.%), known as low- to medium-silica ‘mafic’ S-type granites (L-MSMST granites). Hence, the interpretation of these distinctive S-type granites has provided valuable insights into anatectic and metamorphic processes, tectonic thermal events, and the evolutionary dynamics of the crust along convergent margins. Nevertheless, with the increasing number of reported ‘special S-type granites ’,the absence of standardized terminology has become increasingly evident. In light of this, the present study critically examines advancements in defining maficity S-type granites and formally introduces widely accepted classifications and genetic models associated with them. A comprehensive compilation of published articles on maficity S-type granites was utilized to construct a robust database. This database facilitated the screening of 404 samples, applying various geochemical definitions to refine the selection process. We recognize that (1) the L-MSMST granites are inconsistent with originally defined S-type granite (ST granite); (2) the schematic models of the addition of mantle derived materials can explain the formation of high silica ‘non-mafic’ S-type granites (HSNMST granites) and L-MSMST granites; and (3) L-MSMST granites were may be formed in a typical extensional tectonic background. 404 reference ST granite samples were obtained after screening. L-MSMST granites are inconsistent with the originally defined ST granite. Schematic models may explain the formation of HSNMST and L-MSMST granites. L-MSMST granites may form in a typical extensional tectonic setting.
DOI: 10.6084/m9.figshare.29038888.v1
title: Geochemistry characteristics and tectonic significance of the ‘ “mafic” S-type granites’

description: Taking account of their importance in inferring continental geodynamic processes, S-type granites have been the subject of considerable research since their discovery and identification. With their high A/CNK (Mol. Al<sub>2</sub>O<sub>3</sub>/(Na<sub>2</sub>O + K<sub>2</sub>O + CaO) &gt; 1.1) and low Na<sub>2</sub>O (&lt;3.2 wt.%) and MgO + FeO<sup>T</sup> contents (generally with maficity &lt; 4 wt.%), S-type granites were originally considered to be largely derived from partial melting of metasedimentary sources in orogeny zone settings. However, it is hotly debated why many S-type granites show significantly higher maficity [here defined as the weight percent of MgO + FeO<sup>T</sup> up to 12 wt.% and lower silica (SiO<sub>2</sub> &lt;65 wt.%), known as low- to medium-silica ‘mafic’ S-type granites (L-MSMST granites). Hence, the interpretation of these distinctive S-type granites has provided valuable insights into anatectic and metamorphic processes, tectonic thermal events, and the evolutionary dynamics of the crust along convergent margins. Nevertheless, with the increasing number of reported ‘special S-type granites ’,the absence of standardized terminology has become increasingly evident. In light of this, the present study critically examines advancements in defining maficity S-type granites and formally introduces widely accepted classifications and genetic models associated with them. A comprehensive compilation of published articles on maficity S-type granites was utilized to construct a robust database. This database facilitated the screening of 404 samples, applying various geochemical definitions to refine the selection process. We recognize that (1) the L-MSMST granites are inconsistent with originally defined S-type granite (ST granite); (2) the schematic models of the addition of mantle derived materials can explain the formation of high silica ‘non-mafic’ S-type granites (HSNMST granites) and L-MSMST granites; and (3) L-MSMST granites were may be formed in a typical extensional tectonic background. 404 reference ST granite samples were obtained after screening. L-MSMST granites are inconsistent with the originally defined ST granite. Schematic models may explain the formation of HSNMST and L-MSMST granites. L-MSMST granites may form in a typical extensional tectonic setting.
DOI: 10.15468/dl.ruh45j
title: Occurrence Download

description: A dataset containing 975 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Senna didymobotrya",
 "Country is South Africa",
 "HasCoordinate is true"
 ]
}

 The dataset includes 975 records from 9 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0084996-250717081556266/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.28595574
title: Revisiting gabbroic rocks in the Egyptian-Nubian Shield: new perspectives on the tectonic evolution and classification

description: This contribution reconceives the classification and tectonic evolution of gabbroic rocks in the Egyptian segment of the Arabian-Nubian Shield (ANS), where gabbroic intrusions of diverse ages and geodynamic settings offer an opportunity to give new insights into the tectonomagmatic evolution of the shield’s crust. Early classifications were mainly based on field criteria and mineral compositions. Four distinct gabbro types have been identified: ophiolitic metagabbros, arc-related metagabbros, collision-related gabbros, and anorogenic alkaline gabbros; each reflects a unique petrogenesis and tectonic setting. This new refined classification elucidates the petrogenesis of Egyptian gabbros and emphasizes their formation in peculiar tectonic processes, including mid-ocean ridge spreading, subduction, continental collision, post-collisional extension, and within continental plate up-arching and rifting. Ophiolitic and arc-related gabbros are affiliated with the early pre-collision stages, while collision-related gabbros are associated with the ANS’s collisional phases. The latter Phanerozoic within-plate extension facilitated the formation of anorogenic alkaline gabbros as the least evolved members in some alkaline ring complexes. This review provides a deeper overview and fills gaps in the interpretation of the complex magmatic and tectonic processes that influenced the Arabian-Nubian Shield from the Early Neoproterozoic to the Late Cretaceous period.
DOI: 10.6084/m9.figshare.28595574.v1
title: Revisiting gabbroic rocks in the Egyptian-Nubian Shield: new perspectives on the tectonic evolution and classification

description: This contribution reconceives the classification and tectonic evolution of gabbroic rocks in the Egyptian segment of the Arabian-Nubian Shield (ANS), where gabbroic intrusions of diverse ages and geodynamic settings offer an opportunity to give new insights into the tectonomagmatic evolution of the shield’s crust. Early classifications were mainly based on field criteria and mineral compositions. Four distinct gabbro types have been identified: ophiolitic metagabbros, arc-related metagabbros, collision-related gabbros, and anorogenic alkaline gabbros; each reflects a unique petrogenesis and tectonic setting. This new refined classification elucidates the petrogenesis of Egyptian gabbros and emphasizes their formation in peculiar tectonic processes, including mid-ocean ridge spreading, subduction, continental collision, post-collisional extension, and within continental plate up-arching and rifting. Ophiolitic and arc-related gabbros are affiliated with the early pre-collision stages, while collision-related gabbros are associated with the ANS’s collisional phases. The latter Phanerozoic within-plate extension facilitated the formation of anorogenic alkaline gabbros as the least evolved members in some alkaline ring complexes. This review provides a deeper overview and fills gaps in the interpretation of the complex magmatic and tectonic processes that influenced the Arabian-Nubian Shield from the Early Neoproterozoic to the Late Cretaceous period.
DOI: 10.6084/m9.figshare.28738741
title: Pre-Alpine illitization ages from the Palaeozoic sequences of the Tauride Belt, Southern Türkiye: new data for a Late Palaeozoic event in northern Gondwana

description: Due to the effects of the Alpine orogeny, it is extremely difficult to obtain age data for pre-Alpine geological events for northern Gondwana. This study aims to study the metamorphism in Precambrian (Ediacaran) metaclastic rocks of the Geyik Dağı unit and re-evaluate the geodynamic models of the northern Gondwana-margin based on the geochronology of illite diagenesis in the Late Silurian to Carboniferous shales of the Aladağ and Geyik Dağı units of the Taurides, in southern Türkiye. The average illitization (diagenesis) ages of ~ 275 Ma and ~ 165 Ma correspond to the periods of main unconformities between the Middle Carboniferous and the Late Permian and the Triassic and the Late Jurassic. The fossil records from below and above the unconformity plane between the Middle Carboniferous and the Late Permian indicate a gap of &gt; 70 Ma. Mineralogical and organic matter reflectance data indicate a temperature difference of ~ 50°C between Permian and Carboniferous units indicating different thermal gradients below and above the hiatus. This thermal event coincides with the maximum burial depth resulting from the Palaeozoic subsidence curve of the Geyik Dağı Unit. Mineral and organic petrography-based thermal indicators indicate a pre-Alpine (Variscan) regional tectonic event, confirmed here for the first time by combined mineralogical, organic-petrographic, and isotopic age data. The new data may have the potential to re-evaluate geodynamic models of the northern Gondwana-margin during the Late Palaeozoic. The illitization ages associated with the Alpine metamorphism are ascribed to ophiolite emplacement during the Cretaceous and to tectonic events during the Eocene compressional period, which led to the present nappe structure of the Taurides.