cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/gp3rc4
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V22-174
DOI: 10.15468/t6zdjv
title: Microplankton counts and carbon biomass at station TT007_10-CTD123
DOI: 10.15468/rf984k
title: The Brown University Foraminiferal Data Base (BFD)
DOI: 10.15468/zk88y8
title: Faunal distribution of the most important planktic foraminiferal species in the investigated surface sediment samples from the Chilean continental slope between 23°S and 44°S
DOI: 10.15468/kk3svp
title: Abundance of radiolaria at station UT99-5-1
DOI: 10.15468/r9tbrn
title: Foraminifera species abundances from tow TT011_5-MOC63
DOI: 10.15468/y6ns9r
title: Nannofossil abundance of Hole 4-25
DOI: 10.15468/hjgytm
title: Nannofossil abundance of Hole 94-610B
DOI: 10.15468/64fhsu
title: Total foraminifera counts of multinet M21/2_MSN644
DOI: 10.15468/myykst
title: Molluscs in surface sediments off Sylt collected during HEINCKE cruise HE233
DOI: 10.15468/jfet3p
title: (Table T5) Calcareous nannofossil abundance of ODP Hole 189-1172A sediments
DOI: 10.15468/s8pva2
title: (Table S2) Pliocene/Pleistocene benthic foraminiferal abundances from ODP Hole 161-975D
DOI: 10.15468/6anuj7
title: Planktic foraminifera abundance of Hole 73-524
DOI: 10.15468/xj86zx
title: Siliceous microfossil occurrence, Site 177-1091
DOI: 10.15468/kmcfcp
title: Range table from benthic foraminifers in ODP Hole 149-900A
DOI: 10.15468/gu7xkt
title: Nano and microzooplankton abundance and biomass at station NBP97-01-09-1
DOI: 10.15468/jfsh6z
title: Range table from benthic foraminifera in ODP Hole 199-1220A
DOI: 10.15468/x67u7y
title: Distribution of calcareous nannofossils from IODP Hole 313-M0027A
DOI: 10.15468/24faen
title: Benthic foraminifera abundance of Hole 84-567A, Part 1
DOI: 10.15468/ve57zg
title: Nannofossil abundance of Hole 58-442B
DOI: 10.15468/ekhvkf
title: Percentages of planktonic foraminifera species in sediment core V22-38
DOI: 10.15468/nkmtu7
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/061-3
DOI: 10.15468/drq8pt
title: Total foraminifera counts of multinet POS231/3_MSN1335
DOI: 10.15468/pdjwaw
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/090-2
DOI: 10.15468/bvfx22
title: Nannofossil abundance of Hole 74-526C
DOI: 10.15468/ndfsds
title: Range table from planktonic foraminifers in ODP Hole 170-1039A
DOI: 10.15468/f7m7ms
title: Plasm bearing foraminifera counts of multinet POS231/3_MSN1337
DOI: 10.15468/fb7gx3
title: (Table 2) Benthic foraminifers at DSDP Hole 72-518
DOI: 10.15468/h6pg82
title: Planktic foraminifera abundance of Hole 18-178
DOI: 10.15468/tf4xyq
title: Distribution of planktonic foraminifera of sediment core SH1972_16
DOI: 10.15468/j4kga9
title: Pollen profile from sediment core AV14_K2-3
DOI: 10.15468/p9apzj
title: (Table 1) Distribution of planktonic foraminifera in the upper Turonian-lower Campanian succession in ODP Hole 122-762C, Part II
DOI: 10.15468/bmmb3q
title: Nannofossil abundance of Hole 29-277
DOI: 10.15468/jq9344
title: Assemblage of living benthic foraminifera in sediment core SO118_MC-43, &gt;125 µm fraction
DOI: 10.15468/pmeeu4
title: Planktic foraminifera abundance of Hole 72-515A
DOI: 10.15468/2xyp37
title: Total foraminifera counts of multinet M10/2_MSN232
DOI: 10.15468/pqbw8t
title: Range table from benthic foraminifers in ODP Hole 159-959D
DOI: 10.15468/q8g6xx
title: Range table from benthic foraminifers in ODP Hole 141-861C
DOI: 10.15468/t4v6ez
title: Total foraminifera counts of multinet M21/2_MSN652
DOI: 10.15468/yadar3
title: Microplankton counts and carbon biomass at station TT007_3-CTD29
DOI: 10.15468/p7qhh3
title: Ostracoda abundance of Hole 42-372
DOI: 10.15468/wrgxrf
title: (Table 2) Ostracode distribution in ODP Hole 122-760B
DOI: 10.15468/tfx89m
title: Abundance of dead benthic foraminifera in sediment core CD86_08_BC5
DOI: 10.15468/ygnqwd
title: Plasm bearing foraminifera counts of multinet M21/2_MSN658
DOI: 10.15468/xa7php
title: Benthic foraminifera abundance of Hole 84-569A
DOI: 10.15468/9ax9n9
title: Microfossil abundance of Hole 18-173
DOI: 10.15468/gusmkc
title: (Table T2) Paleocene calcareous nannofossil abundance of ODP Hole 173-1068A
DOI: 10.15468/va49kn
title: (Table 3) Distribution of calcareous nannofossils at DSDP Site 82-563 in the North Atlantic
DOI: 10.15468/3a4g29
title: Abundance and carbon biomass of phytoplankton at station TT007_7-CTD88
DOI: 10.15468/97xpj8
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1391
DOI: 10.15468/chjn7y
title: Microzooplankton abundance measured on water bottle samples at station PS65/545-1
DOI: 10.15468/9qbnst
title: Coccoliths in sediment core PS1532-9
DOI: 10.15468/pe69br
title: Abundance and carbon biomass of phytoplankton at station TT007_15-CTD162
DOI: 10.15468/szd68r
title: Planktic foraminifera abundance of Hole 6-47
DOI: 10.15468/d7npbf
title: Nannofossil abundance of Hole 20-199
DOI: 10.15468/hk37vr
title: Counts of the living benthic foraminifera assemblage in surface sediments of the North Atlantic
DOI: 10.15468/z2gfuc
title: Nannofossil abundance of Hole 74-528A
DOI: 10.15468/d32jnr
title: Benthic foraminifera abundance of Hole 84-567A
DOI: 10.15468/jqfebv
title: Total foraminifera counts of multinet POS247/2_MSN1380
DOI: 10.15468/zbent6
title: Phytoplankton abundance at station Casma_2003-02-27_2, Casma, Peru
DOI: 10.15468/dc8thu
title: Planktic foraminifera abundance of Hole 9-78
DOI: 10.15468/kgjeye
title: Plasm bearing foraminifera counts of multinet M26/1_MSN844
DOI: 10.15468/999cbr
title: Nematode genera abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/363-1a
DOI: 10.15468/a2rsp2
title: (Table 4) Abundance of Pulleniatina obliquiloculata in sediment core ERDC-129BX
DOI: 10.15468/3dg9bv
title: Nannofossil abundance of Hole 9-84
DOI: 10.15468/gh5gfr
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/046-3
DOI: 10.15468/bee3ud
title: Size of planktic foraminifera at CTD station PS55/084-1
DOI: 10.15468/m8rtg4
title: Microplankton abundance at Station SEPT-1997-GN36199704605MSB03 in the euphotic zone of the Aegean Sea in September 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/q4mhg9
title: Total foraminifera counts of multinet M21/4_MSN718
DOI: 10.15468/rsqsjw
title: Nannofossil abundance of Hole 37-332B
DOI: 10.15468/gpne72
title: Living benthic foraminifera at station M33/1_MC-30 (SAST), size fraction 63-125 µm
DOI: 10.15468/6bb2j8
title: Radiolaria assemblage in sediment core GIK17722
DOI: 10.15468/b27x59
title: Occurrence of the most important taxa of macrofauna on Voering Plateau, Tab.10b,11b,14b
DOI: 10.15468/gp6p99
title: Phytoplankton abundance at station Rigel_3_2005-02 in Febraury 2005, Chipana, Chile
DOI: 10.15468/m3ezm7
title: Microplankton counts and carbon biomass at station TT008_5-CTD42
DOI: 10.15468/s89uwd
title: Total foraminifera counts from multinet M31/3_MSN914
DOI: 10.15468/7y5uar
title: Assemblage of living benthic foraminifera in sediment core CD145_55802#4, &gt;150 µm
DOI: 10.15468/ema799
title: Gandaca butterfly specimens at Museum Zoologi Bogor, Indonesia

description: Dataset of Gandaca butterfly specimens deposited at Museum Zoologi Bogor, Indonesia
DOI: 10.15468/tdy5c9
title: Physical properties, geochemistry and ostracoda abundance of sediment core Lz1080
DOI: 10.15468/htsvas
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1387
DOI: 10.15468/6r429q
title: (Table T2) Dinoflagellate stratigraphy of ODP Hole 184-1148A
DOI: 10.15468/wja9as
title: (Appendix B Table 2) Abundance of organic-walled dinoflagellate cysts of sediment core GeoB2204-2

description: A palaeoceanographic reconstruction of the Late Quaternary tropical Atlantic Ocean has been made on the basis of dinoflagellate cyst associations of two sediment cores: the first core was recovered from below the highly productive waters of the equatorial divergence and the second from the oligotrophic western tropical Atlantic Ocean. Palaeoenvironmental indicators for productivity, sea surface temperature (SST) and salinity (SSS) based on selected organic-walled dinoflagellate cyst species have been established. On the basis of these palaeoenvironmental indicators, a strengthened intensity of the equatorial divergence in the eastern region during glacials and cold periods of interglacials has been reconstructed. The highest SST probably occurred around substage 5.5 and might refer to weakest upwelling intensity. In comparison, SST and SSS appear to have been generally higher in the western tropical Atlantic Ocean, with probably enhanced values during glacial intervals. Pronounced differences in accumulation rates and relative abundances of cysts formed by congruentidiacean dinoflagellates and relative abundances of oligotrophic cyst species between the eastern and the western region can be related to differences in palaeoproductivity, suggesting much higher values in the eastern area. The coherence between variation in frequency of the indicators for productivity and the boreal summer insolation and monsoon intensity in the eastern tropical Atlantic Ocean suggests an oceanographic reflection of regional intertropical, rather than boreal, dynamics.
DOI: 10.15468/ngd63b
title: Relative abundance of dead benthic foraminifera of sediment core M5/2_100MC
DOI: 10.15468/c8udvs
title: Macrofauna abundance in surface sediment sampled during cruise DI226
DOI: 10.15468/bgpm4y
title: (Figure 2) Stratigraphic distribution of planktonic foraminifera in the Neogene of ODP Hole 122-762B
DOI: 10.15468/snfae2
title: Total foraminifera counts of multinet M6/7_MSN100
DOI: 10.15468/ugj5gg
title: Nannofossil abundance of Hole 78-542
DOI: 10.15468/ngajxy
title: Abundance of planktic foraminifera at CTD station PS55/077-1
DOI: 10.15468/8g93hk
title: Range table from ostracoda in ODP Hole 151-910A
DOI: 10.15468/ev5zad
title: (Fig. 4) Assemblage of benthic foraminifera in sediment core GeoB6725-1
DOI: 10.15468/3j9h3u
title: Live benthic foraminifera in South Atlantic surface sediments
DOI: 10.15468/puwz8z
title: Phytoplankton abundance in surface water in October 1997, Callao, Peru
DOI: 10.6084/m9.figshare.24498376
title: 230827 PIM-1_Literature survey.xlsx

description: Membranes
DOI: 10.6084/m9.figshare.24498376.v1
title: 230827 PIM-1_Literature survey.xlsx

description: Membranes
DOI: 10.15468/weyqer
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
DOI: 10.15468/8t6ftg
title: Meiofaunal abundance, biomass, taxon richness and indices of nematode diversity of samples from the Santa Maria di Leuca Bank (southern Adriatic margin)

description: Deep-water coral ecosystems are hot spots of biodiversity and provide habitats and refuges for several deep-sea species. However, their role in shaping the biodiversity of the surrounding open slopes is still poorly known. We investigated how meiofaunal biodiversity varies with and is related to the occurrence of deep-water living scleractinian corals and coral rubble in two deep-sea areas (the Rockall Bank, northeastern Atlantic) and the Santa Maria di Leuca (central Mediterranean). In both areas, replicated sampling on alive and dead coral areas and from the adjacent slope sediments without corals (at the same and increasing depths) allowed us to demonstrate that sediments surrounding the living corals and coral rubble were characterised by higher meiofaunal biodiversity (as number of higher taxa, and nematode species richness) than the slope sediments. Despite the soft sediments surrounding the living coral having a higher nutritional value than those not associated with corals, with the opposite seen for coral rubble, the presence of both alive and dead corals had a significant effect on nematode assemblages. Our data suggest that, due particularly to the effects on habitat heterogeneity/complexity, both living coral and coral rubble promoted higher biodiversity levels than in surrounding slope sediments. We conclude that the protection of deep-water corals can be crucial to preserve the biodiversity of surrounding open slopes, and that the protection of dead corals, a so-far almost neglected habitat in terms of biological conservation, can further contribute to the maintenance of a high deep-sea biodiversity along continental margins.
DOI: 10.15468/4jcjha
title: Range table from benthic foraminifers in ODP Hole 172-1055C
DOI: 10.15468/pz83xb
title: (Table T1) Census counts of planktic foraminifers at ODP Hole 175-1087A
DOI: 10.15468/akqadd
title: (Table 2a) Species of planktonic foraminifera found in sediment traps at Station Vy20-3217TR
DOI: 10.15468/vabphr
title: (Table 5) Distribution of foraminifera in the Miocene section of ODP Hole 133-826A
DOI: 10.15468/vyqbgw
title: Stratigraphic occurrence of selected marine palynomorph species recorder in the Paleogene of ODP Hole 105-647A (Table 3)

description: Dinoflagellate cysts were recovered throughout the Paleogene succession of Hole 647A, which contains an almost complete deep-water record of early Eocene through early late Oligocene sedimentation in the Labrador Sea. Dinoflagellate cyst biostratigraphy is in general accord with that provided by other microfossil groups and is consistent with a lower Eocene age, as determined by nannofossils, for basal sediments in Hole 647A. These sediments overlie oceanic crust of Chron 24 age. Dinocyst assemblages indicate outer neritic to oceanic conditions throughout, although the persistent occurrence of Wetzeliellaceae specimens in the lower Eocene suggests a greater influence from shelf environments during this time. Lower Eocene dinocyst assemblages are similar to coeval assemblages from the Rockall Plateau, but those from the middle to upper Eocene have mixed affinities and may be related to the intensification of the proto-Gulf Stream from middle Eocene time. Oligocene dinocyst assemblages suggest the influence of both arctic and North Atlantic wate rmasses at this site. The presence of protoperidineacean species in the upper Eocene and Oligocene may indicate increased availability of nutrients, perhaps related to increased upwelling or the effects of water-mass mixing. Productive samples are dominated by dinocysts and acritarchs, while sporomorphs are represented mainly by bisaccate pollen. Preservational differences within samples may reflect mixing of penecontemporaneous dinocyst populations during the Eocene, and all samples examined may have a considerable allochthonous component. Variability in relative abundance of many species during the Eocene may be related to fluctuating water-mass properties. A total 175 dinocyst and acritarch taxa were recorded from 53 productive samples from the Paleogene. Only one Paleogene sample was barren of palynomorphs. Of three Miocene samples processed, all were barren.
DOI: 10.15468/8rtaqz
title: Foraminifera species abundances from tow TT011_9-MOC69
DOI: 10.15468/vnwmpj
title: (Table T5) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole 171B-1052E
DOI: 10.15468/9epcbt
title: Distribution of dinoflagellate cysts in Eocene-Oligocene sediments of ODP Hole 151-913B
DOI: 10.15468/pq8aat
title: Range table from planktonic foraminifers in ODP Hole 175-1083A
DOI: 10.15468/zf5ey3
title: (Table SD1, Fig. 2) Benthic foraminiferal abundances, preservation states and thickness to diameter ratios from IODP Hole 310-M0005D
DOI: 10.15468/gq22hr
title: Total foraminifera counts of multinet M21/4_MSN722
DOI: 10.15468/ch7b45
title: Planktic foraminifera abundance of Hole 23-219
DOI: 10.15468/9bwwmc
title: Planktic foraminifera abundance of Hole 4-30
DOI: 10.15468/7x2vf5
title: Abundance of epibenthic echinoderms at seafloor photography station M21/4_250
DOI: 10.15468/wct3t7
title: Crustacea in surface sediments off Sylt collected during HEINCKE cruise HE272
DOI: 10.15468/yw4sfa
title: Analyses of the recent components of sediment core PS1400-4
DOI: 10.15468/ewacc5
title: Pollen analysis of sediment profile KR0 from Kreutzsee
DOI: 10.15468/asn9sd
title: Benthic foraminifera assemblage in sediment core BBLL3_MC1
DOI: 10.15468/z7ft55
title: (Table C a) Relative contributions of planktic foraminiferal species in sediment trap series L1/K276-23 at 3000 m water depth
DOI: 10.15468/jc5btf
title: Distribution of planktic foraminifers of core Y71-09-101
DOI: 10.15468/uv4rc8
title: Phytoplankton abundance during Akademik Vernadsky cruise AV22
DOI: 10.15468/z5nmyh
title: Foraminifera, sedimentological parameters and sea surface temperature and salinity calculated on core SO82_5-2
DOI: 10.15468/8ykqsb
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station JUNE-94-GN3619940280200590
DOI: 10.15468/aznftk
title: Nannofossil abundance of Hole 59-448
DOI: 10.15468/aqmma8
title: Calcareous dinoflagellates nominated in grain fraction &lt; 20 µm
DOI: 10.15468/tqexaa
title: Planktic foraminifera abundance of Hole 54-423
DOI: 10.15468/rres3h
title: (Table 2) Miocene biostratigraphy of the Vierlandian stage in Schleswig-Holstein
DOI: 10.15468/ssqtvq
title: Nannofossil abundance of Hole 7-63A
DOI: 10.15468/nssbxn
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1380
DOI: 10.15468/bxkx9b
title: Trap data WR2, 599 m
DOI: 10.15468/ss7k4k
title: Phytoplankton abundance measured on water samples from rivers of the Lena Delta in 2009

description: During the 2009 cruise in the Lena delta a first comprehensive set of phytoplankton samples was collected from several areas of the Lena Delta. The aim was to establish a first checklist of phytoplankton and microzooplankton species in the Delta for form the basis for future assessments and to aid in the selection of sites to be used as fixed annual monitoring sites in future.
DOI: 10.15468/8a673b
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
DOI: 10.15468/uqgvm4
title: Abundance of the benthic infauna of the North Sea sampled during Victor Hensen cruise VH1486
DOI: 10.15468/apa8e9
title: Phytoplankton abundance at station CD47_1206C#7
DOI: 10.15468/6tpp6c
title: Nannofossil abundance of Hole 94-609C
DOI: 10.15468/a4zab7
title: (Table T1) Calcareous nannofossil stratigraphy of ODP Hole 182-1127B
DOI: 10.15468/7racpa
title: Abundance of broken diatom frustules measured on water bottle samples at station PS58/011-3
DOI: 10.15468/gbthsa
title: Nannofossil abundance of Hole 14-142
DOI: 10.15468/jrds3s
title: Percentages of planktonic foraminifera species in sediment core V25-60
DOI: 10.15468/ab5jfm
title: Phytoplankton abundance at station Rigel_6_2005-03 in March 2005, Chipana, Chile
DOI: 10.15468/q8q5z3
title: Assemblage of living benthic foraminifera in sediment core GeoB3725-1
DOI: 10.15468/hc75cm
title: Planktic foraminifera abundance of Hole 16-158
DOI: 10.15468/7c7nd6
title: Assemblage of living benthic foraminifera in sediment core SO129_MC-03, &gt;125 µm fraction
DOI: 10.15468/ryhmg7
title: Phytoplankton abundance and species composition in the Gulf of Naples in June 1999 at station MCSSII-phyto102-110
DOI: 10.15468/by3j2m
title: Planktic foraminifera counts of sediment core ELT48.027-PC
DOI: 10.15468/q94bkd
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station APRIL-1995-D2
DOI: 10.15468/9dfvsa
title: Range table from planktonic foraminifers in ODP Hole 151-909C
DOI: 10.15468/ygsa6g
title: Range table from planktonic foraminifers in ODP Hole 177-1088B
DOI: 10.15468/8yy6eu
title: (Appendix 2) Abundances of benthic forminifera in ODP Hole 113-690B
DOI: 10.15468/ah6yvy
title: Distribution of planktic foraminifera of sediment core GIK23352-3 at stadium 5.5
DOI: 10.15468/s6rxva
title: Abundance of benthos infauna at station GIK23006-3
DOI: 10.15468/vxr274
title: Pollen analysis of sediment profile MU01 from Muggesfelder See
DOI: 10.15468/5a2tzu
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station JUNE-1998-IR72
DOI: 10.15468/yt3epd
title: Total foraminifera counts of multinet FCA97C_MSN1343
DOI: 10.15468/6bvw6p
title: Range table from benthic foraminifers in ODP Hole 159-960C
DOI: 10.15468/b5jf4d
title: (Table 2) Abundance of benthic foraminifers of sediment core PS2157-3
DOI: 10.15468/xazas4
title: Benthic macrofauna abundance of sediment core 12930-017
DOI: 10.5281/zenodo.10070388
title: Chronological Molecular Fingerprint of Wetland Soil by Sensitivity-Enhanced Solid-State NMR

description: The unprocessed ssNMR data files generated in this study "Chronological Molecular Fingerprint of Wetland Soil by Sensitivity-Enhanced Solid-State NMR".
DOI: 10.15468/9xwndh
title: Relativ abundances of total live fauna of benthic foraminifera in surface sediments (Table C1.1)
DOI: 10.5281/zenodo.10070387
title: Chronological Molecular Fingerprint of Wetland Soil by Sensitivity-Enhanced Solid-State NMR

description: The unprocessed ssNMR data files generated in this study "Chronological Molecular Fingerprint of Wetland Soil by Sensitivity-Enhanced Solid-State NMR".
DOI: 10.15468/npgqs6
title: (Table 7) Planktonic foraminifer abundance of ODP Hole 162-983A
DOI: 10.15468/jay8ap
title: Planktic foraminifera of sediment core GeoB1406-4
DOI: 10.15468/3zf8r8
title: Abundance of radiolaria at station LV28-64-2
DOI: 10.15468/d4y6af
title: (Table 7) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-684A
DOI: 10.15468/b574w8
title: (Table 1) Distribution of planktonic foraminifera in ODP Hole 183-1135A, Part I
DOI: 10.15468/rc3wsn
title: Range table from ostracoda in ODP Hole 151-911A
DOI: 10.15468/5jrh8x
title: Distribution of late Neogene age calcareous nannofossils in ODP Hole 111-677A (Table 2)

description: The calcareous nannofossil assemblages recovered from Site 677A range in age from latest Miocene (NN11) to latest Pleistocene. The consistently high sediment-accumulation rate (mean of 48 m/m.y.) coupled with little dissolution of carbonate has ensured that generally rich, well-preserved coccolith assemblages occur at this site. Exceptions are the Pliocene/Pleistocene boundary sediments, which show evidence of dissolution, and upper Miocene basement sediments, which show evidence of diagenetic overgrowths. The apparent paradox of the occurrence of large numbers of the cool-water species Coccolithus pelagicus together with subtropical and tropical nannofossil species is thought to represent increased seasonality in the degree of upwelling in the Panama Basin. Seasonal upwelling was particularly intense during the late Miocene, when common C. pelagicus occurred with Thalassionema diatoms. Populations of C. pelagicus probably bloomed during a winter period of upwelling that was associated with a shallow thermocline and depressed surface-water temperatures.
DOI: 10.15468/x9a2j7
title: Total foraminifera counts of multinet SO117_MSN1243
DOI: 10.15468/pxs7rm
title: Coccolith counts of multinet SO119_MSN1295