Find research datasets worth reusing
Search datasets from major research repositories and use ShareScore to quickly assess how well each record supports discovery, access, and reuse.
13
datasets available to search
ShareScore release 0.9.0
Dataset results
13 results for “planktic foraminifera”
caseysaenger/ForamMgCa_PSM: files and scripts for revised version of manuscript "Calibration and validation of environmental controls on planktic foraminifera Mg/Ca using global core-top data".
<p>files and scripts for revised version of manuscript "Calibration and validation of environmental controls on planktic foraminifera Mg/Ca using global core-top data". Saenger, C. and M. N. Evans. Resubmitted to Paleoceanography and Paleoclimatology, May 3, 2019.</p>
Fig. 1 in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 1. Study area bathymetry (Liu and Dittert 2010), surface circulation patterns (Koutsikopoulos et al. 1996), and location of the study Site WH (44°33′N, 2°45′W; 2,000 m water depth). The position of Site KS10b (Mojtahid et al. 2013) is marked by a white square. IPC – Iberian Poleward Current, ENACW – Eastern North Atlantic Central Waters.
Fig. 5. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 5. a – oxygen stable isotope ratios (δ18O) performed on G. bulloides and G. inflata; b – Δδ 18O between δ18O and δ18O; G. inflata G. bulloides c – carbon stable isotope ratios (δ13C) performed on G. bulloides and G. inflata; d – Δδ 13C between δ13C and δ13C. The grey G. inflata G. bulloides lines represent FC WH and the black colour represents CADIAC WH. The horizontal dotted lines delimitate the major changes (see text for all the details).
Fig. 4. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 4. a – time records in Cores CADIAC WH (black color) and FC WH (grey color) of benthic foraminiferal abundances (ind. g–1 of dry sediment), benthic foraminiferal accumulation rates (ind. cm–2 ka–1), relative abundances of the main benthic species present with ≥ 5% in at least one sample (after removing the non-fossilizing taxa), and species richness; b – time records in Cores CADIAC WH (black color) and FC WH (grey color) of planktic foraminiferal abundances (ind. g–1 of dry sediment), same indications as for benthic faunas. The horizontal dotted lines delimitate the major foraminiferal changes (see text for all the details).
Data From: Forabot: Automated Planktic Foraminifera Isolation and Imaging
<p>Physical inspection and sorting of foraminifera is a necessity in many research labs, as foraminifera serve as paleoenvironmental and chronostratigraphic indicators.</p> <p>In order to gain counts of species from samples, analyze chemical compositions, or extract morphological properties of foraminifera, research labs require human effort and time handling and sorting these microscopic fossils.</p> <p>The presented information supports Forabot, an open-source system that can physically manipulate individual foraminifera for imaging and isolation with minimal human interaction.</p> <p>The associated data, codebase, and documentation support building a Forabot and confirming results related to processing raw image data, error detection results, and proof of concept deep classification network.</p>
Benthic and Planktic Foraminifera Counts from Concession 20D on the Orange Shelf, South Africa.
<p>Benthic and planktic foraminifera counts from three vibracores within Concession 20D on the Orange Shelf of western South Africa. The vibracores from which foraminifera were subsampled include inner shelf core 12820D, outer shelf core 14820D, and outer shelf core 14620D. Counts are presented as absolute abundances and were counted to a 300-300 benthic-planktic threshold. Where this threshold could not be met, the total amount of benthic and planktic foraminifera for all sampled sediment was noted. </p>
Data From: Forabot: Automated Planktic Foraminifera Isolation and Imaging
Open the record for dataset details and reuse information.
Data : Planktic-benthic foraminifera ratio (%P) as a tool for the reconstruction of paleobathymetry and geohazard: A case study from Taiwan
<p>Details of the core sites used in this study, gear used for recovery, sediment horizon analyzed, coordinates, water depth and foraminiferal data for the size fractions of >125 µm and >63 µm (only a subset of all the sites). Study sites are divided into East Taiwan that comprises the Southern Okinawa Trough (1), Nanao-Hoping-Hateruma Basins (2), and Taitung-Hualien (3). The area of West Taiwan is consisted of the Gaoping (4), Changchun sand Ridge (5), and Henghun Ridge (6) sectors. Gear for recovery are Box core (BC); Gravity core (GC) and Grab (G). Italic numbers in TOC column (in red) are average values, italic numbers in the Laboratory column show the laboratory where the TOC and C/N were analysed, namely Geosciences-NTU (1) , Institute of Oceanography-NTU (2) and National Sun-yat sen University (3). NaN= no available data. </p>
DATA: Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth
<p>Dataset from "Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth". Three files that represent: all data (stable isotope, weight, size) for T. sacculifer; all data (stable isotope, weight, size) for G. ruber and N.dutertrei and individual final chamber and remaining shell for T. sacculifer.</p>
Data from: Blooms of aberrant planktic foraminifera across the K/Pg boundary in the Western Tethys: causes and evolutionary implications
Open the record for dataset details and reuse information.
FIGURE 11. Planktic foraminifera from the Namibian outer shelf with primary apertural views visible. 1 in Quaternary foraminifera and mollusc assemblages on the southwestern African shelf
FIGURE 11. Planktic foraminifera from the Namibian outer shelf with primary apertural views visible. 1. Globorotalia (Globoconella) inflata (d'Orbigny, 1839b) (core 2670, 98 cm); 2. Globorotalia menardii (Parker, Jones and Brady, 1865) (core 2670, 23 cm); 3. Globorotalia truncatulinoides (d'Orbigny, 1839b) (core 2670, 23 cm); 4. Neogloboquadrina dutertrei (d'Orbigny, 1839a) (core 2670, 43 cm); 5. Neogloboquadrina incompta (Cifelli, 1961) (core 2670, 85 cm); 6 Globigerina bulloides d'Orbigny, 1826 (core 2670, 85 cm); 7. Globigerinella siphonifera (d'Orbigny, 1839b) (core 2670, 33 cm); 8. Globigerinoides ruber white (d'Orbigny, 1839a) (core 2670, 13 cm); 9. Trilobatus sacculifer (Brady, 1877) (core 2670, 63 cm); 10. Orbulina bilobata (d'Orbigny, 1846) (core 2670, 3 cm); 11. Orbulina universa d'Orbigny, 1839a (core 2670, 33 cm).
Fig. 2. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 2. a – age model and AMS radiocarbon ages for Cores FC WH and CADIAC WH; b – X-Ray photograph of Core CADIAC WH and grain-size parameters.
Fig. 3 in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 3. Benthic foraminiferal fauna characteristics of Core FC WH: a – densities of the main (> 5% in at least one sample) living benthic foraminifera (ind. 50 cm–3 of wet sediment); b – species richness of the living benthic fauna; c – densities of the main (> 5% in at least one sample) dead benthic foraminiferal species (ind. 50 cm–3 of wet sediment); d – species richness of the dead benthic fauna.
ScienceDex guides
Understand access before you commit
These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.