cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.250749
title: Planktic foraminifera abundance of Hole 27-263

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.624057
title: Analyses of the recent components of sediment core PS1216-1

description: Values &lt;1 mark traces
DOI: 10.15468/qhahsp
title: Inventaire des individus de grande nacre de la digue du Port de Cannes

description: Réfection & Confortement de la digue Laubeuf et de la digue du Large du port départemental de Cannes : inventaire des individus de Grande nacre avant le début des travaux Observations réalisées par SEMANTIC TS pour le compte de : CCI Nice Cote d'Azur - Ville de Cannes (Marché N° N° 2017/57/PI/01/030)
DOI: 10.1594/pangaea.75430
title: Total foraminifera counts of multinet M10/2_MSN231
DOI: 10.15468/dl.8xgbnn
title: Occurrence Download

description: A dataset containing 32 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is (Table 1) Proportion of Toxoplasma gondii seropositive arctic foxes (Alopex lagopus) by age group and geographic area"
 ]
}

 The dataset includes 32 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004136-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.131468
title: Microzooplankton abundance and biomass at station NBP97-08-13-1
DOI: 10.1594/pangaea.604827
title: Planktic foraminifera counts at CTD station PS55/025
DOI: 10.1594/pangaea.692234
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station OCTOBER-1994-D4

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5 µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.15468/kehtee
title: Postia alni Niemelä & Vampola (Basidiomycota, Polyporales) – member of the problematic Postia caesia complex – has been found for the first time in Hungary

description: Due to their bluish basidiocarps the Postia caesia (syn. Oligoporus caesius) complex forms a distinctive morphological group within the polypore genus Postia Fr., 1874. Five species of this group occur in Europe: P. alni Niemelä & Vampola, P. caesia (Schrad.) P. Karst., P. luteocaesia (A. David) Jülich, P. mediterraneocaesia M. Pierre & B. Rivoire and P. subcaesia (A. David) Jülich. In this study P. alni is reported for the first time from Hungary. The dichotomous key of the species of the European Postia caesia complex was prepared as well.
DOI: 10.1594/pangaea.743959
title: (Appendix) Abundances of benthic foraminifera in ODP Hole 105-646B
DOI: 10.15468/st9brr
title: Scotland Island
DOI: 10.1594/pangaea.75979
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1386
DOI: 10.1594/pangaea.604821
title: Planktic foraminifera counts at CTD station M39/4_376CTD-29
DOI: 10.25345/c5862bp6t
title: MassIVE MSV000095433 - CCMR-UFRJ 2024 - Exploration runs
title: Exploration of the chemical space of the specimens from the cyanobacteria collection CCMR-UFRJ.
DOI: 10.1594/pangaea.82293
title: Distribution of planktic foraminifera (250-500 µm) of box sediment core PS1243-2
DOI: 10.15468/mwzwls
title: The Survey Data of Benthic Diatoms in Anping historical waterview park

description: The dataset provide the records of benthic diatoms attached on the diatom boards which were set on the artificial floating islands (AFIs) established on seawater in Anping Historical Waterview Park in Tainan, Taiwan. Diatoms were cultured with diatom boards and sampled four times from October to December of 2017. A total of 45 diatom species belonging to 22 genera were identified. Among them, the Navicula genus has the largest richness, and Achnanthes subsessilis and Nitzschia longissima were the dominant species in number.
DOI: 10.1594/pangaea.690958
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB01 in the euphotic zone of the Aegean Sea in March 1998. Part 3 - coccolithophores and other groups

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.788610
title: (Table 1) Planktonic foraminiferal abundance at DSDP Site 94-606

description: A "total fauna" curve (Ruddiman, 1971; doi:10.1130/0016-7606(1971)82[283:PSITEA]2.0.CO;2) shows that surface water overlying DSDP Site 606 (central North Atlantic Ocean) cooled suddenly at 3.1 Ma, within the Mammoth paleomagnetic reversed interval. At that time, Globorotalia puncticulata, Neogloboquadrina pachyderma, and Globorotalia crassaformis increased and Globorotalia hirsuta, Globigerinoides sacculifer, and Sphaeroidinellopsis decreased in abundance. Oxygen isotope results for Globigerina bulloides do not indicate a "stepwise" cooling, but probably reflect small changes in continental ice volume. It is hypothesized that as annual average temperatures decreased, G. bulloides delayed its bloom from spring to summer to follow a preferred temperature habitat.
description: Supplement to: Ehrmann, Lisa M; Keigwin, Lloyd D (1987): Middle Pliocene change in planktonic foraminiferal fauna at Site 606. In: Ruddiman, WF; Kidd, RB; Thomas, E; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 94, 921-924
DOI: 10.1594/pangaea.712654
title: (Table 2) Abundance of benthic foraminifers of sediment core PS2157-3
DOI: 10.1594/pangaea.249384
title: Nannofossil abundance of Hole 6-47

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.75674
title: Total foraminifera counts of multinet M21/4_MSN722
DOI: 10.1594/pangaea.605393
title: Abundance of nematoda in sediment profile M3/1_031 from the Iberian deep sea basin (Table 5)

description: Counts per core, core surface 25 cm**2
DOI: 10.1594/pangaea.249745
title: Nannofossil abundance of Hole 60-457

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.724678
title: (Table DR1) Abundance of benthonic foraminifera in sediments from ODP Hole 113-690

description: A mass extinction of deep-sea benthic foraminifera has been documented globally, coeval with the negative carbon isotope excursion (CIE) at the Paleocene-Eocene boundary, which was probably caused by dissociation of methane hydrate. A detailed record of benthic foraminiferal faunal change over ~30 k.y. across the carbon isotopic excursion at the Ocean Drilling Program Site 690 (Southern Ocean) shows that shortly before the CIE absolute benthic foraminiferal abundance at that site started to increase. 'Doomed species' began to decrease in abundance at the CIE by a few thousand years. After the extinction faunas were dominated by small species, which resemble opportunistic taxa under high-productivity regions in the present oceans. Calcareous nannofossils (primary producers), however, show a transition to more oligotrophic nannofloras exactly where the benthic faunas show the opposite. Plankton and benthos is thus decoupled. Possibly, a larger fraction of food particles reached the seafloor after the CIE, so that food for benthos increased although productivity declined. Enhanced organic preservation might have resulted from low-oxygen conditions caused by oxidation of methane. Alternatively, and speculatively, there was a food-source at the ocean floor. Benthic foraminifera dominating the post-extinction fauna resemble living species that symbiotically use chemosynthetic bacteria at cold seeps. During increased, diffuse methane escape from hydrates, sulfate-reducing bacteria could have produced sulfide used by chemosynthetic bacteria, which in turn were used by the benthic foraminifera, causing extinction by a change in food supply.
description: Supplement to: Thomas, Ellen (2003): Extinction and food at the seafloor: A high-resolution benthic foraminiferal record across the initial Eocene thermal maximum, Southern Ocean site 690. GSA Special Paper: Causes and consequences of globally warm climates in the Early Paleogene, 319-332
DOI: 10.1594/pangaea.358350
title: Assemblage of living benthic foraminifera in sediment core SO117_MC468, &gt;125 µm fraction
DOI: 10.1594/pangaea.810696
title: (Table 14) Benthic foraminifera in late Miocene sediments of DSDP Hole 90-592

description: Abundances: X = present, A = very abundant, - = absent.
DOI: 10.1594/pangaea.225572
title: Planktic foraminifera of sediment core GeoB1406-4

description: Half Moon 07.04.1991
DOI: 10.1594/pangaea.71254
title: Total foraminifera counts from multinet M31/3_MSN917
DOI: 10.1594/pangaea.690960
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB03 in the euphotic zone of the Aegean Sea in March 1998. Part 3 - coccolithophores and other groups

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.623649
title: Analyses of the recent components in the sand fraction of sediment core PS1011-1
DOI: 10.15468/gwietr
title: Suivi de l'expansion du Frelon asiatique (Vespa velutina)-Inventaire hivernal des nids de frelon asiatique

description: Objectif :
L’objectif de cet inventaire est de rassembler un jeu exhaustif de données de nidification concernant Vespa velutina dans des espaces restreints géographiquement. Ceci dans le but de réaliser des études d'impact, des évaluations de méthodes de lutte ou modélisation fine de sa répartition.

Collecte :
Les données sont collectées par Q. Rome (MNHN) et divers organismes partenaires.
DOI: 10.1594/pangaea.810697
title: (Table 15) Benthic foraminifera in Pliocene sediments of DSDP Hole 90-592

description: Abundances: X = present, A = very abundant, - = absent.
DOI: 10.1594/pangaea.688479
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB03 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.66507
title: (Table 2b) Downcore distribution of live benthic foraminifera of sediment core PS1394-3, Weddell Sea
DOI: 10.15468/dl.y99nwh
title: Occurrence Download

description: A dataset containing 1310925 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is Paleobiology Database"
 ]
}

 The dataset includes 1310925 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004137-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.752214
title: (Table 1) Distribution of planktonic foraminifera in ODP Hole 183-1135A, Part I

description: Abundances: AA = very abundant (&gt;40%), A = abundant (26-39%), C = common (16-25%), F = few (6-15%), R = rare (2-5%), VR = very rare (&lt;2%), cf. = uncertain identification, transitional forms, ? = questionable identification, - = absent.
DOI: 10.1594/pangaea.655281
title: Phytoplankton abundance during ARGOS cruise Argos91/5
DOI: 10.1594/pangaea.688482
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB05 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.250115
title: Planktic foraminifera abundance of Hole 29-281

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.785117
title: (Table 4) Characteristics of the Donax trunculus population on the beach of the Anapa Bay Bar in October 2010
DOI: 10.1594/pangaea.128657
title: Coccolith counts of multinet SO119_MSN1295
DOI: 10.1594/pangaea.87309
title: Abundance of coccosphere-units of sediment core GIK23411-5

description: Age given in calendar years. Coccosphere-unit: Conversion of coccoliths to hypothetical coccospheres by taking an average number of coccoliths per coccosphere. Data were corrected after publication due to a systematical error (conversion factor 1.44).
DOI: 10.1594/pangaea.198817
title: Phytoplankton abundance at station CD47_1206C#7

description: Plymouth Marine Laboratory. Authorship was originally taken from the JGOFS CDs (Lowry et al.) and was changed by request of the BODC.
DOI: 10.1594/pangaea.251338
title: Nannofossil abundance of Hole 94-609C

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.249740
title: Nannofossil abundance of Hole 60-454

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.399102
title: Relative abundance of planktonic foraminifera in sediment core L-198
DOI: 10.1594/pangaea.250663
title: (Figure 4) Stratigraphic distribution of planktonic foraminifera in DSDP Hole 93-604

description: During Deep Sea Drilling Project Leg 93, upper Miocene through Quaternary sediments were continuously cored in Hole 604, located on the upper continental rise of the New Jersey transect (western North Atlantic). A detailed biostratigraphic study of these strata has been made using the vertical distribution of planktonic foraminifers. The Quaternary climatic zonation of Ericson and Wollin (1968) has been tentatively delineated and all the Pliocene zones and subzones (sensu Berggren, 1977) have been recognized. The rate of sedimentation was slow during most of the Pliocene but underwent a significant acceleration in the early Pleistocene. Quantitative variations in the distribution of planktonic foraminifers appear to be influenced by various factors, such as hydrodynamic winnowing resulting from the action of bottom currents and surficial thermal conditions caused by climatic changes. Both dissolution intervals and brief increases in the coarser detrital input seem, most of the time, to be correlated with indications of climatic cooling and may correspond to glacial events or cycles. This chapter delineates a precursor stage in the inception of Northern Hemisphere glaciation at 3 Ma and wide-scale Quaternary glacial-interglacial cycles.Data from a detailed study of Hole 604 are briefly compared with the main sedimentary and microfaunal features of contemporaneous series previously drilled along the east American margin in the northwestern Atlantic. One of the striking observations appears to be the intense redistribution of sediments that affected this region in Neogene-Quaternary times.
description: Species abundance: A = abundant, C = common, F = few, R = rare, VR = very rare, - = absent.
description: Supplement to: Moullade, Michel (1987): Distribution of Neogene and Quaternary planktonic foraminifers from the upper continental rise of the New Jersey Margin (western North Atlantic), Deep Sea Drilling Project Leg 93, Site 604: Sedimentary and paleoceanographic implications of the biostratigraphy. In: van Hinte, JE; Wise, SW Jr; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 93, 493-509
DOI: 10.15468/dl.zo5b6s
title: Occurrence Download

description: A dataset containing 36019 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Elaeagnus L."
 ]
}

 The dataset includes 36019 records from 407 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004139-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.788605
title: (Table T5) Calcareous nannofossil stratigraphy of ODP Hole 198-1212B

description: Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (&gt;10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1 specimen per 2-10 FOV); R = rare (1 specimen per 11-100 FOV), 1-2 = 1 or 2 specimens, ? = questionable occurrence, - = not found. Biostratigraphy is described with reference to the lowermost Cretaceous NK zones of Bralower et al. (1989, doi:10.1016/0377-8398(89)90035-2), Lower Cretaceous NC zones of Roth (1978, doi:10.2973/dsdp.proc.44.134.1978; 1983, doi:10.2973/dsdp.proc.76.125.1983) with subzones after Bralower (1987, doi:10.1016/0377-8398(87)90003-X) and Bralower et al. (1993), and Upper Cretaceous zones of Burnett (1998). The biostratigraphic zones, chronostratigraphy, and timescale correlations are after Shipboard Scientific Party (2002a, doi:10.2973/odp.proc.ir.198.102.2002).
DOI: 10.1594/pangaea.690947
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB02 in the euphotic zone of the Aegean Sea in March 1998. Part 1 - diatoms

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.819425
title: (Figure 7) Relative abundance of nannoliths at DSDP Hole 62-463

description: 0 = species that were not observed in the particular sample during counting.
DOI: 10.15468/x8rcse
title: Observations of the emergence of Fijian cicadas in September 2017

description: A "nanai" campaign was run on the month of September of 2017, increasing awareness about our unique and endemic cicada, Raiateana knowlesi; a species that is known to emerge once every 8 years. This species is known from only a handful of locations within the Namosi and Navosa Province. A competition was developed through the NatureFiji-MareqetiViti (NFMV) campaign and website to help collect any additional information of emergence from the public with the hopes that we could confirm original distributional information as well as include any possible new credible information of their distribution/emergence. The competition required that certain information was recorded and that a picture was uploaded to help confirm the species and presence.
DOI: 10.1594/pangaea.604871
title: Abundance of planktic foraminifera at CTD station PS55/078-1
DOI: 10.1594/pangaea.787035
title: (Appendix) Abundance of Discoaster brouweri and Coccolithus pelagicus in ODP Site 180-1115 sediments
DOI: 10.1594/pangaea.75435
title: Total foraminifera counts of multinet M10/2_MSN261
DOI: 10.1594/pangaea.231614
title: Planktic foraminifera abundance of Hole 23-223

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.623668
title: Analyses of the recent components in the sand fraction of sediment core PS1402-2
DOI: 10.1594/pangaea.75849
title: Total foraminifera counts of multinet M21/2_MSN624
DOI: 10.1594/pangaea.250131
title: Planktic foraminifera abundance of Hole 9-80A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.75725
title: Total foraminifera counts of multinet M21/5_MSN734
DOI: 10.1594/pangaea.59073
title: Assemblage of living benthic foraminifera in sediment core SO129_MC-09, 30-63 µm fraction
DOI: 10.1594/pangaea.250738
title: Ostracoda abundance of Hole 11-105

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.692233
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station OCTOBER-1994-D2

description: Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (&gt;5 µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.
DOI: 10.1594/pangaea.75950
title: Total foraminifera counts of multinet POS247/2_MSN1378
DOI: 10.15468/dl.g0omxy
title: Occurrence Download

description: A dataset containing 32 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is (Table 1) Proportion of Toxoplasma gondii seropositive arctic foxes (Alopex lagopus) by age group and geographic area"
 ]
}

 The dataset includes 32 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004146-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.hlnj1y
title: Occurrence Download

description: A dataset containing 30 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((160.16161 -53.29769,199.33364 -53.29769,199.33364 -32.13146,160.16161 -32.13146,160.16161 -53.29769))",
 "HasCoordinate is true",
 "TaxonKey is Ricciocarpos natans (L.) Corda",
 "HasGeospatialIssue is false"
 ]
}

 The dataset includes 30 records from 6 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004140-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.761995
title: (Table 2) Macrobenthos on the floor of the West Bay of the Furugelm Island, Sea of Japan
DOI: 10.15468/dl.5qa4f7
title: Occurrence Download

description: A dataset containing 162 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Mexico",
 "TaxonKey is Scyphophorus acupunctatus Gyllenhal, 1838"
 ]
}

 The dataset includes 162 records from 9 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0004141-190621201848488/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.