cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.n3d4rq
title: Occurrence Download

description: A dataset containing 4370823 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is one of (Algeria, Angola, Benin, Botswana, Burkina Faso, Burundi, Cabo Verde, Cameroon, Central African Republic, Chad, Comoros, Congo, Congo, Democratic Republic of the, Côte d’Ivoire, Djibouti, Egypt, Equatorial Guinea, Eritrea, Eswatini, Ethiopia, Gabon, Gambia, Ghana, Guinea, Guinea-Bissau, Kenya, Lesotho, Liberia, Libya, Madagascar, Malawi, Mali, Mauritania, Mauritius, Morocco, Mozambique, Namibia, Niger, Nigeria, Rwanda, Sao Tome and Principe, Senegal, Seychelles, Sierra Leone, Somalia, South Africa, South Sudan, Sudan, Tanzania, United Republic of, Togo, Tunisia, Uganda, Zambia, Zimbabwe, Western Sahara, Réunion, Mayotte, Saint Helena, Ascension and Tristan da Cunha, British Indian Ocean Territory, French Southern Territories)",
 "HasCoordinate is true",
 "Year is greater than or equal to 2018",
 "Year is less than or equal to 2018"
 ]
}

 The dataset includes 4370823 records from 633 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002174-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.577fdq
title: Occurrence Download

description: A dataset containing 3 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Selago canescens",
 "Country is Australia",
 "HasCoordinate is true"
 ]
}

 The dataset includes 3 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002210-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.60893/figshare.apl.29987443
title: Supplement Number 1

description: The four-step "photoemission model", details of ML algorithms and definitions of performance evaluation metrics of ML methods
DOI: 10.60893/figshare.apl.29987443.v1
title: Supplement Number 1

description: The four-step "photoemission model", details of ML algorithms and definitions of performance evaluation metrics of ML methods
DOI: 10.15468/dl.cu6tnu
title: Occurrence Download

description: A dataset containing 38 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is one of (Human Observation, Specimen, Occurrence evidence)",
 "TaxonKey is Argia westfalli"
 ]
}

 The dataset includes 38 records from 6 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002213-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.wp3r3s
title: Occurrence Download

description: A dataset containing 64 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Sophora tonkinensis"
 ]
}

 The dataset includes 64 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002214-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.4c2bfx
title: Occurrence Download

description: A dataset containing 26 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Selago corymbosa",
 "Country is Australia",
 "HasCoordinate is true"
 ]
}

 The dataset includes 26 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002216-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.cn44vb
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Pareuchiloglanis songdaensis)",
 "BasisOfRecord is one of (Specimen, Literature Occurrence, Human Observation, Observation)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 1991",
 "Year is less than or equal to 2025"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002217-250914085247600/datasets/export for details.
DOI: 10.15468/dl.jc6yef
title: Occurrence Download

description: A dataset containing 5562 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is one of (Human Observation, Specimen, Occurrence evidence)",
 "Continent is one of (North America, South America)",
 "TaxonKey is Brachymesia furcata"
 ]
}

 The dataset includes 5562 records from 50 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002218-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.w63dzu
title: Occurrence Download

description: A dataset containing 844 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is one of (Human Observation, Specimen, Occurrence evidence)",
 "TaxonKey is Brechmorhoga praecox"
 ]
}

 The dataset includes 844 records from 35 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002219-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25345/c5r78625k
title: MassIVE MSV000099160 - 20250914_Powers_eif4g2_lysates
title: A total of 4 cell lines were used: 3 independent murine PDA cell lines (ccmT1, ccmT2, ccmT4) and a cell line marked M1. For each cell line (4), there are 3 sample conditions: transduced with sgROSA, sgEIF4g2-2, or sgEIF4g2-4. For every sample condition (12) there are two technical replicates, totaling 24 samples.
DOI: 10.6084/m9.figshare.30123139.v3
title: BenchHub_database

description: This is used for loaded dataset for BenchHub
DOI: 10.15468/dl.4p4c6p
title: Occurrence Download

description: A dataset containing 561 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Verbascum blattaria",
 "Country is Canada",
 "HasCoordinate is true"
 ]
}

 The dataset includes 561 records from 13 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002221-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.5vx3sp
title: Occurrence Download

description: A dataset containing 142 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Verbascum blattaria",
 "Country is Australia",
 "HasCoordinate is true"
 ]
}

 The dataset includes 142 records from 16 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002220-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.8223bj
title: Occurrence Download

description: A dataset containing 20 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Verbascum blattaria",
 "Country is Denmark",
 "HasCoordinate is true"
 ]
}

 The dataset includes 20 records from 6 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002222-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.21227/ag1c-1q46
title: "Model-based Incoherent Compact Polarimetric Decomposition Experimental Dataset"

description: "The three datasets used in \"Model-based Incoherent Compact Polarimetric Decomposition\".dataT(:,:,1) = T11; dataT(:,:,2) = T22; dataT(:,:,3) = T33;dataT(:,:,4) = real(T12); dataT(:,:,5) = real(T13); dataT(:,:,6) = real(T23);dataT(:,:,7) = imag(T12); dataT(:,:,8) = imag(T13); dataT(:,:,9) = imag(T23);Where Tij deones the element of a polarimetric coherency matrix. "
DOI: 10.15468/dl.nk465q
title: Occurrence Download

description: A dataset containing 64 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Sophora tonkinensis"
 ]
}

 The dataset includes 64 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0002223-250914085247600/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.6mtwrz
title: Occurrence Download

description: A dataset containing 382976 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Oryza sativa L."
 ]
}

 The dataset includes 382976 records from 498 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0032286-240626123714530/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.25027112
title: Exotic pollen in sediments from the high Arctic Lake Tenndammen, Svalbard archipelago: diversity, sources, and transport pathways

description: We analysed the pollen and spores extracted from 73 samples of lacustrine sediments from Colesdalen in Svalbard (Lake Tenndammen) as well as 10 soil samples collected from the lake’s shores. In total, 56 pollen taxa were recorded from the sediments spanning the last 800 years, whilst 35 pollen types were found in the soil samples. Pollen was categorised as (i) regional (from Svalbard); (ii) exotic to Svalbard today; or (iii) of mixed or unclear origin. Major changes in pollen assemblages after ca 1900 CE were associated with human impact. Around 1920 CE, the first signs of introduced plant taxa were identified, by the presence of Apiaceae and Fabaceae pollen. Additionally, large-sized pollen with a thick exine and annulus diameter of 10.6–13 μm, identified as Poaceae/Cerealia type, was constantly present after ca 1920 CE. Other exotic pollen, including <i>Ulmus</i>, <i>Juglans</i>, and tropical pollen of <i>Albizia/Mimosa</i> type, <i>Eucalyptus</i> type, <i>Acalypha</i> type, and <i>Passiflora</i> type, are found only during the 1930s to 1960s, which is the period associated with the most intensive mining activity and human migration to and from Colesdalen. Furthermore, the repeated occurrence of <i>Myrica</i> (<i>gale</i>) type and <i>Erica</i> type occurring both in the lake sediment and in the soil samples is best explained by the migration of geese from Scotland (UK). Our research demonstrates how precisely human history can be reflected in the lake sediments of the Arctic environment.
DOI: 10.6084/m9.figshare.25027112.v1
title: Exotic pollen in sediments from the high Arctic Lake Tenndammen, Svalbard archipelago: diversity, sources, and transport pathways

description: We analysed the pollen and spores extracted from 73 samples of lacustrine sediments from Colesdalen in Svalbard (Lake Tenndammen) as well as 10 soil samples collected from the lake’s shores. In total, 56 pollen taxa were recorded from the sediments spanning the last 800 years, whilst 35 pollen types were found in the soil samples. Pollen was categorised as (i) regional (from Svalbard); (ii) exotic to Svalbard today; or (iii) of mixed or unclear origin. Major changes in pollen assemblages after ca 1900 CE were associated with human impact. Around 1920 CE, the first signs of introduced plant taxa were identified, by the presence of Apiaceae and Fabaceae pollen. Additionally, large-sized pollen with a thick exine and annulus diameter of 10.6–13 μm, identified as Poaceae/Cerealia type, was constantly present after ca 1920 CE. Other exotic pollen, including <i>Ulmus</i>, <i>Juglans</i>, and tropical pollen of <i>Albizia/Mimosa</i> type, <i>Eucalyptus</i> type, <i>Acalypha</i> type, and <i>Passiflora</i> type, are found only during the 1930s to 1960s, which is the period associated with the most intensive mining activity and human migration to and from Colesdalen. Furthermore, the repeated occurrence of <i>Myrica</i> (<i>gale</i>) type and <i>Erica</i> type occurring both in the lake sediment and in the soil samples is best explained by the migration of geese from Scotland (UK). Our research demonstrates how precisely human history can be reflected in the lake sediments of the Arctic environment.
DOI: 10.6084/m9.figshare.25129973
title: Upper Cretaceous (Cenomanian) palynostratigraphy and palynofacies of the Shushan Basin, North Egypt

description: This study provides an updated quantitative analysis and prospective paleoenvironment reconstruction of the Tut oilfield, Shushan Basin, North Egypt to evaluate the hydrocarbon reservoirs in space and times for further development plans and modeling in the Tethyan region. Two sporomorph interval zones (<i>Classopollis brasiliensis</i> and <i>Afropollis jardinus</i>), and one total foraminiferal Range Zone (<i>Thomasinella punica</i>) are proposed. Three palynofacies assemblages are differentiated using cluster analysis of the different palynofacies parameters. The paleoenvironmental conditions during the Cenomanian were reconstructed. Palynofacies assemblage I of the Baharyia Formation suggests a marginally dysoxic-oxic basin environment with a common occurrence of ostracods and terrestrial organic matter, while palynofacies assemblage II reflects the high abundance of dinoflagellate cysts, suggesting a suboxic-anoxic middle neritic environment. Palynofacies assemblage III of the upper part of the Abu Roash G Member represents a relatively deep water inner-middle neritic environment. Three 3<sup>rd</sup> order significant sequences separated by two hiatus surfaces (Ce3 and Ce4) are described and correlated with the global eustatic sea-level. The hydrocarbon evaluation results show that the samples from the Abu Roash G Member contain oil-prone material of kerogen type II, while the samples of the Baharyia Formation are characterized by kerogen type III (gas-prone). Spore coloration analysis reveals that the samples from the studied units are too immature to produce gas or oil and are ineffective as sources of hydrocarbons.
DOI: 10.6084/m9.figshare.25375081
title: Biostratigraphic analysis of a Late Pleistocene to Holocene section from Punta Pescador, eastern Venezuela

description: A biostratigraphic study was undertaken on a shallow borehole drilled to 90 meters in the easternmost Orinoco Delta, Venezuela. Twenty-eight samples were analyzed for palynomorphs and foraminifera. Palynomorphs were recovered in all except one sample consisting of 178 entities. Foraminifera assemblages of low diversity were recovered in 17 of the 28 samples. The analysis provides some insight into the vegetation, climate, and depositional history allowing comparisons with other Late Pleistocene to Holocene studies in the northern South America region. The Late Pleistocene to Early Holocene transition is marked by an unconformity, where the vegetation changes from a diverse flora of <i>Mauritia flexuosa</i>, grasses (Poaceae), ferns, and mangroves (<i>Rhizophora</i>, <i>Avicennia</i>) to one dominated by <i>Rhizophora</i> around 10,000 years BP. This transition also contains reworked palynomorphs and abundant black wood (inertinite), indicative of erosion and oxidation. The absence of foraminifera suggests an exposed continental shelf and lowering of sea level. The Early Holocene mangrove flora is replaced by vegetation dominated by <i>Mauritia flexuosa</i>, with <i>Symphonia globuliflora</i>, grasses, and ferns. The palynological signature for the upper 42 m of the section compares favorably with a previous study of the Holocene in the Orinoco Delta. Radiocarbon dating indicates there is an unconformity or condensed section at the vegetation change, representing as much as 5500 ± years. Foraminifera indicate an open shelf environment immediately above this horizon followed by a significant shallowing to nearshore transitional environments near the top of the section. Local climate and/or human influence may have been a factor in the abundance of <i>Mauritia flexuosa</i> as suggested by other studies.
DOI: 10.6084/m9.figshare.25375081.v1
title: Biostratigraphic Analysis of a Late Pleistocene to Holocene section from Punta Pescador, Eastern Venezuela

description: A biostratigraphic study was undertaken on a shallow borehole drilled to <b>90 meters</b> in the easternmost Orinoco Delta, Venezuela. Twenty-eight samples were analyzed for palynomorphs and foraminifera. Palynomorphs were recovered in all except one sample consisting of 178 entities. Foraminifera assemblages of low diversity were recovered in 17 of the 28 samples. The analysis provides some insight into the vegetation, climate, and depositional history allowing comparisons with other Late Pleistocene to Holocene studies in the northern South America region. The Late Pleistocene to Early Holocene transition is marked by an unconformity, where the vegetation changes from a diverse flora of <i>Mauritia flexuosa,</i> grasses (Poaceae), ferns, and mangroves (<i>Rhizophora</i>, <i>Avicennia</i>) to one dominated by <i>Rhizophora</i> around 10,000 years BP. This transition also contains reworked palynomorphs and abundant black wood (inertinite), indicative of erosion and oxidation. The absence of foraminifera suggests an exposed continental shelf and lowering of sea level. The Early Holocene mangrove flora is replaced by vegetation dominated by <i>Mauritia flexuosa,</i> with <i>Symphonia globuliflora,</i> grasses, and ferns. The palynological signature for the upper <b>42 meter</b> of the section compares favorably with a previous study of the Holocene in the Orinoco Delta. Radiocarbon dating indicates there is an unconformity or condensed section at the vegetation change, representing as much as 5,500 +/- years. Foraminifera indicate an open shelf environment immediately above this horizon followed by a significant shallowing to nearshore transitional environments near the top of the section. Local climate and/or human influence may have been a factor in the abundance of <i>Mauritia flexuosa</i> as suggested by other studies.
DOI: 10.6084/m9.figshare.25375081.v2
title: Biostratigraphic analysis of a Late Pleistocene to Holocene section from Punta Pescador, eastern Venezuela

description: A biostratigraphic study was undertaken on a shallow borehole drilled to 90 meters in the easternmost Orinoco Delta, Venezuela. Twenty-eight samples were analyzed for palynomorphs and foraminifera. Palynomorphs were recovered in all except one sample consisting of 178 entities. Foraminifera assemblages of low diversity were recovered in 17 of the 28 samples. The analysis provides some insight into the vegetation, climate, and depositional history allowing comparisons with other Late Pleistocene to Holocene studies in the northern South America region. The Late Pleistocene to Early Holocene transition is marked by an unconformity, where the vegetation changes from a diverse flora of <i>Mauritia flexuosa</i>, grasses (Poaceae), ferns, and mangroves (<i>Rhizophora</i>, <i>Avicennia</i>) to one dominated by <i>Rhizophora</i> around 10,000 years BP. This transition also contains reworked palynomorphs and abundant black wood (inertinite), indicative of erosion and oxidation. The absence of foraminifera suggests an exposed continental shelf and lowering of sea level. The Early Holocene mangrove flora is replaced by vegetation dominated by <i>Mauritia flexuosa</i>, with <i>Symphonia globuliflora</i>, grasses, and ferns. The palynological signature for the upper 42 m of the section compares favorably with a previous study of the Holocene in the Orinoco Delta. Radiocarbon dating indicates there is an unconformity or condensed section at the vegetation change, representing as much as 5500 ± years. Foraminifera indicate an open shelf environment immediately above this horizon followed by a significant shallowing to nearshore transitional environments near the top of the section. Local climate and/or human influence may have been a factor in the abundance of <i>Mauritia flexuosa</i> as suggested by other studies.
DOI: 10.6084/m9.figshare.25129973.v1
title: Upper Cretaceous (Cenomanian) Palynostratigraphy and Palynofacies of the Shushan Basin, North Egypt

description: The current work can produce an updated quantitative analysis and prospective paleoenvironment reconstruction from Tut oil Field, Shushan Basin to evaluate the hydrocarbon reservoirs in space and times for further development plans and modelling in the Tethyan regime. Two sporomorph interval zones (<i>Classopollis brasiliensis</i> and <i>Afropollis jardinus</i>), and one total foraminiferal Range Zone (<i>Thomasinella punica</i>) are proposed. Three palynofacies assemblages are differentiated using cluster analysis of the different palynofacies parameters. The paleoenvironmental conditions during the Cenomanian age were reconstructed. Palynofacies assemblage I of the Baharyia Formation suggests a marginally dysoxic-oxic basin environment with a common occurrence of ostracods and terrestrial organic matter, while palynofacies assemblage II reflects the high abundance of dinoflagellate cysts, suggesting a suboxic-anoxic middle neritic environment. Palynofacies assemblage III of the upper part of Abu Roash G Member represents a relatively deep water inner-middle neritic environment. Three 3<sup>rd</sup> order significant sequences separated by two hiatus surfaces (Ce3 and Ce4) are described and correlated with the global eustatic sea-level. The hydrocarbon evaluation results show that the samples from the Abu Roash G Member contain oil-prone material of kerogen type II, while the samples of the Baharyia Formation are characterized by kerogen type III (gas-prone). Spore coloration analysis reveals that the samples from the studied formations are too immature to produce gas or oil and are ineffective as sources of hydrocarbon.
DOI: 10.6084/m9.figshare.25129973.v2
title: Upper Cretaceous (Cenomanian) palynostratigraphy and palynofacies of the Shushan Basin, North Egypt

description: This study provides an updated quantitative analysis and prospective paleoenvironment reconstruction of the Tut oilfield, Shushan Basin, North Egypt to evaluate the hydrocarbon reservoirs in space and times for further development plans and modeling in the Tethyan region. Two sporomorph interval zones (<i>Classopollis brasiliensis</i> and <i>Afropollis jardinus</i>), and one total foraminiferal Range Zone (<i>Thomasinella punica</i>) are proposed. Three palynofacies assemblages are differentiated using cluster analysis of the different palynofacies parameters. The paleoenvironmental conditions during the Cenomanian were reconstructed. Palynofacies assemblage I of the Baharyia Formation suggests a marginally dysoxic-oxic basin environment with a common occurrence of ostracods and terrestrial organic matter, while palynofacies assemblage II reflects the high abundance of dinoflagellate cysts, suggesting a suboxic-anoxic middle neritic environment. Palynofacies assemblage III of the upper part of the Abu Roash G Member represents a relatively deep water inner-middle neritic environment. Three 3<sup>rd</sup> order significant sequences separated by two hiatus surfaces (Ce3 and Ce4) are described and correlated with the global eustatic sea-level. The hydrocarbon evaluation results show that the samples from the Abu Roash G Member contain oil-prone material of kerogen type II, while the samples of the Baharyia Formation are characterized by kerogen type III (gas-prone). Spore coloration analysis reveals that the samples from the studied units are too immature to produce gas or oil and are ineffective as sources of hydrocarbons.