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764 results for “foraminifera”

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zenodo32/100

PLATE 5. 1 in Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf

PLATE 5. 1. Uvigerina spinulosa (core 2670, 178 cm); 2. Orthomorphina jedlitschkai (core 2670, 118 cm); 3a. Sphaeroidina bulloides; 3b. close-up of aperture of Sphaeroidina bulloides (core 2670, 118 cm); 4–6. Siphonina pulchra (core 2670, 98 cm); 6a–6b. oblique apertural views of Siphonina pulchra (core 2670, 98 cm); 7a. Cibicidoides crebbsi (oblique spiral view); 7b. Cibicidoides crebbsi (apertural view); 7c. Cibicidoides crebbsi (umbilical view) (core 2670, 118 cm); 8. Cibicidoides pseudoungerianus (spiral view) (core 2670, 85 cm); 9. Cibicidoides pseudoungerianus (umbilical view) (core 2670, 85 cm); 10a. Cibicidoides pseudoungerianus (spiral view); 10b. Cibicidoides pseudoungerianus (apertural view); 10c. Cibicidoides pseudoungerianus (umbilical view) (core 2670, 118 cm).

opennotspecifiedJan 2022View details →
zenodo32/100

PLATE 6. 1a in Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf

PLATE 6. 1a. Cibicidoides ungerianus (umbilical view); 1b. Cibicidoides ungerianus (apertural view); 1c. Cibicidoides ungerianus (spiral view) (core 2670, 178 cm); 2a. Heterolepa dutemplei (spiral view); 2b. Heterolepa dutemplei (oblique apertural view); 2c. Heterolepa dutemplei (oblique umbilical view) (core 2670, 128 cm); 3. Heterolepa broeckhiana (spiral view) (core 2670, 108 cm); 4a. Heterolepa broeckhiana (umbilical view); 4b. Heterolepa broeckhiana (apertural view); 4c. Heterolepa broeckhiana (spiral view) (core 2670, 88 cm); 5. Melonis affinis (core 2670, 178 cm); 6a. Anomalinoides helicinus (spiral view); 6b. Anomalinoides helicinus (oblique apertural-marginal view); 7. Anomalinoides helicinus (oblique umbilical view) (core 2670, 178 cm); 8a. Hansenisca soldanii (umbilical view); 8b. Hansenisca soldanii (apertural-marginal view) (core 2670, 115 cm).

opennotspecifiedJan 2022View details →
zenodo32/100

FIGURE 2. a and b in Presence of Foraminifera of Superfamily Komokioidea (Order Astrorhizida) in Colombian deep Caribbean waters

FIGURE 2. a and b. Specimens belonging to Lana neglecta (Family Komokiidae); c. Amplification of tubules from Lana neglecta.

opennotspecifiedOct 2017View details →
zenodo32/100

FIGURE 1 in Presence of Foraminifera of Superfamily Komokioidea (Order Astrorhizida) in Colombian deep Caribbean waters

FIGURE 1. Location of COL 4 and COL 5 blocks and differentiation of geoforms on the sea bed (Extracted and modified from Garrido-Linares et al. 2014).

opennotspecifiedOct 2017View details →
zenodo32/100

Laser ablation depth profile data for different IODP and ODP Sites and age intervals from Voigt et al. "Assessing the recrystallisation of planktonic foraminifera in Pelagic sediments and the reliability of Mg/Ca values with Laser Ablation (LA-) ICP-MS"

<p>These files contain the final processed laser ablation ICP-MS depth profiles of Mg/Ca and Sr/Ca through the shell walls of fossil planktonic foraminifera tests from specific time intervals from International Ocean Discovery Program (IODP) Sites U1334, U1335, U1336, U1337, U1338 and Ocean Drilling Program (ODP) SIte 1218 in the eastern equatorial Pacific.</p> <p>These data are from Voigt et al. "Assessing the recrystallisation of planktonic foraminifera in Pelagic sediments and the reliability of Mg/Ca values with Laser Ablation (LA-) ICP-MS",&nbsp;a manuscript submitted&nbsp; to the journal <em>Paleoceanography and Paleoclimatology</em></p>

opencc-by-4.0Jun 2024View details →
zenodo32/100

FIGURE 2. Reticulammina novaezelandica Tendal, 1972 in First record of a Xenophyophore (Rhizaria: Foraminifera) on the Chilean margin

FIGURE 2. Reticulammina novaezelandica Tendal, 1972 (MNHNCL PRO-15000). Details of the specimen: a, SEM view of lamellae and open spaces forming the reticulated structure. b, overview of agglutinated material. c, detail of agglutinated material showing foraminiferan and radiolarian tests and sponge spicule fragments. d, foraminiferan test. e–f, radiolarian tests; some scattered stercomata are visible in e.

opennotspecifiedAug 2018View details →
zenodo32/100

FIGURE 1. Reticulammina novaezelandica Tendal, 1972 in First record of a Xenophyophore (Rhizaria: Foraminifera) on the Chilean margin

FIGURE 1. Reticulammina novaezelandica Tendal, 1972 (MNHNCL PRO-15000). a–d, four views of entire specimen. e, detail showing the abraded surfaces of the lamellae separated by open spaces. f, specimen attached to rock. Scale is 10 mm for a–d and f, and 2 mm for e.

opennotspecifiedAug 2018View details →
zenodo32/100

Paired X-ray Micro CT Scanning and individual foraminifera isotopic analysis reveal (de)coupled changes in carbonate preservation and temperature

<p>To assess the coupling between drivers of isotopic variability and carbonate dissolution in foraminifera, we combine individual foraminiferal carbon and oxygen isotopic analyses (IFA) and X-ray MicroCT Scanning (XMCT)-based measurements of test densities (a proxy for the extent of post-depositional dissolution). As a proof-of-concept application of this approach, we analyze Globigerina bulloides tests from both coretop and downcore (latest Miocene/earliest Pliocene-aged) sediment from Ocean Drilling Project (ODP) Site 1088 (Agulhas Ridge).<br>Sediments from both the core intervals were wet-sieved over a 150 &mu;m sieve and oven-dried at 55&deg;C overnight. Individual tests of G. bulloides were picked from the &gt;150 &mu;m size fraction and gently brushed with the wet tip of a paintbrush to remove any adhering clay. Broken or partially fragmented tests were avoided. 25-50 individuals were mounted on a 1.2cm x 1 cm cardboard sample holder using double-sided carbon and imaged at a time on a Bruker Skyscan 1272 Micro-CT Scanner. In total, 123 individuals from the coretop sample and 88 individuals from the downcore sample were scanned.<br>Stable carbon (&delta;&sup1;&sup3;C) and oxygen (&delta;&sup1;⁸O) isotopic compositions of individual foraminifera were measured using a Kiel Carbonate Device IV coupled to a Thermo Fisher MAT 253 Plus Isotope Ratio Mass Spectrometer (IRMS). All individuals were weighed on a Sartorius ultramicrobalance before analysis, and only samples with mass &gt;10 &micro;g were analyzed as per the long-term precision setup of analyzing small quantities of carbonates on this machine. The XMCT-IFA dataset in this study consists of &delta;&sup1;&sup3;C and &delta;&sup1;⁸O values of 90 foraminifera (67 coretop and 23 downcore individuals). We compare population averages of XMCT parameters and isotopic compositions from both the coretop and downcore sediments.</p>

opencc-by-4.0Sep 2024View details →
zenodo32/100

SW Gulf of Mexico planktonic foraminifera, oxygen isotopes and Mg/Ca data from core RC10-265PC spanning MIS 6 to MIS 1

<p>In the sediment Core RC10-265PC collected in the oligotrophic region of the SW Gulf of Mexico, it was reconstructed the surface ocean conditions, including water masses, the mixed layer depth and the sea surface temperatures over the Late Pleistocene to Holocene (last 180 cal ka BP). This database includes (Table S1) the counting and distribution of planktonic foraminifera assemblages, and (Table S2) stable oxygen isotopes (&delta;<sup>18</sup>O-PDB) (&permil;) of <em>Globigerinoides ruber</em> (white) and elemental ratios of Mg/Ca (mmol/mol), Mn/Ca (mmol/mol), Fe/Ca (mmol/mol), Sr/Ca (mmol/mol), Mn/Fe (mmol/mol).</p>

opencc-by-4.0Aug 2024View details →
zenodo32/100

Supporting data for: Decadal trend of plankton community change and habitat shoaling in the Arctic gateway recorded by planktonic foraminifera

<p><strong>Table S1:&nbsp;</strong>Metadata of the samples included in the study complete with the relative source of CTD and foraminifera census data.</p> <p><strong>Table S2</strong>:&nbsp;Environmental and biological data used for the analyses in the study. Abbreviations: dh= depth habitat, sst= sea surface temperature, aw = Atlantic water layer.</p>

opencc-by-4.0Dec 2020View details →
zenodo32/100

FIGURE 1. A in A checklist of Foraminifera of the Eastern Shelf of the Adriatic Sea

FIGURE 1. A. Adriatic Sea regions after Giorgetti and Mosetti (1969) (a–e) and after Artegiani et al. (1997) (I–III). B. Sediments distribution in the Adriatic Sea (modified after Pigorini 1967 and Colantoni &amp; Mencucci 2010), with Adriatic Sea regions modified for this study after Artegiani et al. (1997); lines define the Northern Adriatic (1), Central Adriatic (2), South Adriatic (3) with Otranto (4) sub-basins.

opennotspecifiedSep 2011View details →
zenodo32/100

FIGURE 2 in A checklist of Foraminifera of the Eastern Shelf of the Adriatic Sea

FIGURE 2. Geographic positions of investigated areas. Authors are presented by numbers explained in Table 2.

opennotspecifiedSep 2011View details →
zenodo32/100

FIGURE 2 in New species of Leptohalysis (Rhizaria, Foraminifera) from an extreme hadal site in the western Pacific Ocean

FIGURE 2: Leptohalysis kaikoi sp. nov., scanning electron micrographs. A: Complete specimen. B; Proximal end showing organic-walled proloculus. C: Central part of test showing grains with flat exposed surfaces. D: Aperture. E: Patches of organic cement on grain surfaces. F–G: Outer surface showing agglutinated grains embedded in copious amounts of organic cement.

opennotspecifiedMar 2009View details →
zenodo32/100

FIGURE 1 in New species of Leptohalysis (Rhizaria, Foraminifera) from an extreme hadal site in the western Pacific Ocean

FIGURE 1: Leptohalysis kaikoi sp. nov., photographs taken using transmitted light. A: Holotype, reg. no. MPC-02690. B–G: Paratypes, reg. nos MPC-02691-02696. H–P: Additional unregistered specimens. Scale bars = 50 µm.

opennotspecifiedMar 2009View details →
zenodo32/100

FIGURE 3 in New species of Leptohalysis (Rhizaria, Foraminifera) from an extreme hadal site in the western Pacific Ocean

FIGURE 3: Leptohalysis sp. 1, scanning electron micrographs. A: Complete specimen. B: Proximal end showing organic-walled proloculus with some plate-like grains. C: Final chamber. D–E: Progressively closer views of final chamber showing mesh-like masses of organic cement and flake-like mineral grains. F: Central part of test. G: Close view showing cement and agglutinated grains.

opennotspecifiedMar 2009View details →
zenodo32/100

Organic geochemical proxies, foraminieral assemblages and isotopic geochemistry of benthic foraminifera from core NYA17-154

<p>The dataset contains all the data from cor NYA17-154 presented in Tesi et al. 2021 Science Advances</p> <p><strong>Rapid Atlantification along the Fram Strait at the beginning of the 20<sup>th</sup> century </strong></p> <p>Tesi. Tommaso<sup>1*</sup>, Francesco &nbsp;Muschitiello<sup>2,3*</sup>, Gesine Mollenhauer<sup>4</sup>, Stefano Miserocchi<sup>1</sup>, Leonardo Langone<sup>1</sup>, Chiara Ceccarelli<sup>5</sup>, Giuliana Panieri<sup>6</sup>, Jacopo Chiggiato<sup>7</sup>, Alessio &nbsp;Nogarotto<sup>1,8</sup>, Jens Hefter<sup>4</sup>, Gianmarco Ingrosso<sup>1</sup>, Federico Giglio<sup>1</sup>, Patrizia Giordano<sup>1</sup>, Lucilla Capotondi<sup>7</sup></p> <p>(1) Istituto di Scienze Polari - Consiglio Nazionale delle Ricerche ISP-CNR,&nbsp; 40129 Bologna, Italy</p> <p>(2) Department of Geography - University of Cambridge, Cambridge, CB2 3EN, UK</p> <p>(3) NORCE Norwegian Research Centre, 5007 Bergen, Norway</p> <p>&nbsp;(4) Alfred Wegener Institute - Helmholtz Center for Polar and Marine Sciences, 27570 Bremerhaven, Germany</p> <p>(5) Dipartimento di Scienze Biologiche, Geologiche ed Ambientali &ndash; BiGeA, 40126 Bologna, Italy</p> <p>(6) CAGE ‐ Center of Arctic Gas Hydrate, Environment and Climate, Department of Geolosciences, UiT The Arctic University of Norway, Troms&oslash;, Norway</p> <p>&nbsp;(7) Istituto di Scienze Marine - Consiglio Nazionale delle Ricerche ISMAR-CNR,&nbsp; 40129 Bologna, Italy</p> <p>(8) Campus Scientifico, Universit&agrave; Ca&rsquo; Foscari Venezia, 30172 Venezia Mestre, Italy</p> <p>&nbsp;</p> <p>The data encompasses:</p> <p>- age-depth model</p> <p>- alkenone derived sea surface temperature</p> <p>- TEX86-L derived water temperature</p> <p>- stable oxygen isotope data of N. labradorica</p> <p>- benthic foraminifera assemblages</p> <p>- retene content</p>

opencc-by-4.0Oct 2021View details →
zenodo32/100

DATA: Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth

<p>Dataset from &quot;Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth&quot;. Three files that represent: all data (stable isotope, weight, size) for T. sacculifer;&nbsp;all data (stable isotope, weight, size) for G. ruber and N.dutertrei and&nbsp;&nbsp;individual final chamber and remaining shell for T. sacculifer.</p>

opencc-by-4.0Dec 2018View details →
dryad32/100

Data from: Abyssal benthic foraminifera in the eastern equatorial Pacific (IODP Exp 320) during the middle Eocene

Open the record for dataset details and reuse information.

publicJul 2013View details →
dryad32/100

Data from: Within- and among-genus components of size evolution during mass extinction, recovery, and background intervals: a case study of Late Permian through Late Triassic foraminifera

Open the record for dataset details and reuse information.

publicMay 2012View details →
dryad32/100

Data from: Environmental monitoring through protist NGS metabarcoding: assessing the impact of fish farming on benthic foraminifera communities

Open the record for dataset details and reuse information.

publicApr 2014View details →

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