cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/gba9dn
title: Abundances of dinoflagellate cysts in sediment trap MST-9 (Appendix 1)

description: To study the ecology of calcareous dinoflagellates we examined the impact of the SW and NE monsoons on cyst formation using sediment trap material, collected at 1032 m water depth, off Somalia from June 1992 to February 1993. The results do not confirm the relationship between cyst production and lower nutrient concentrations, as highest cyst fluxes were recorded during late SW monsoon under the relatively nutrient-rich and less agitated conditions of mature upwelled water. Lowest cyst fluxes were found under strongly stratified, nutrient-depleted surface waters during the inter-monsoon. Although all of the studied species seem to prefer a stratified water column, an elevated concentration of nutrients appears to be necessary to maintain high cyst production. Comparison of the mean cyst flux to the sediment trap with that into the underlying surface sediments reveals a loss of 81-96%, which can be attributed to calcite dissolution. The relatively small spheres of Thoracosphaera heimii are affected more than the cysts of the other species.
DOI: 10.15468/pnw2sj
title: Nannofossil abundance of Hole 1-3
DOI: 10.15468/qfefyc
title: Nannofossil abundance of Hole 6-55
DOI: 10.15468/vxy26w
title: Occurrence of mammalia relicts at site Raj Cave
DOI: 10.15468/n4wmzb
title: (Figure 5) Range chart of selected dinocysts and acritarchs of ODP Hole 104-642A
DOI: 10.15468/vcg9mv
title: Chironomid remains in the sediment sequence of Site PG1212
DOI: 10.15468/sudrwu
title: (Table 9) Relative abundance of calcareous nannofossil species across the Cretaceous/Paleocene boundary at ODP Hole 120-750A
DOI: 10.15468/833etv
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB03 in the euphotic zone of the Aegean Sea in March 1998. Part 2 - dinoflagellates
DOI: 10.15468/f5u5nq
title: (Table 2) Range chart for planktonic foraminifers from ODP Hole 111-677B
DOI: 10.15468/44btk7
title: Nannofossil abundance of Hole 31-299
DOI: 10.15468/6med4d
title: Occurence of marine palynomorphs of sediment core CRP-1 (Table 1)

description: The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section rather than the anticipated Palaeogene sediments. Initial palynologic study was conducted at the Crary Science and Engineering Laboratory, McMurdo Station, concurrent with drilling. Rapid and environmentally safe sample processing was made possible by the use of a focused microwave digestion unit that scrubbed acid fumes. In situ and/or reworked dinocysts (dinoflagellate cysts), acritarchs (leiospheres and acanthomorphs), and prasinophyte phycomata are present in the 35 samples studied. Overall, the CRP-1 assemblages are similar to Arctic marine palynomorph assemblages that are used there as ice margin indicators. Some of the acanthomorph acritarchs recovered from the CRP-1 core closely resemble cysts of extant Antarctic autotrophic sea-ice dinoflagellates. It is possible that some of these acanthomorphs are actually dinocysts, and could be used as indicators of sea-ice conditions similar to today. Most of the in situ marine palynomorphs are undescribed taxa and thus are presently of little biostratigraphic value. Dating of the core was based on diatom, palaeomagnetic and strontium isotope studies. The upper 43.55 mbsf of the core are Quaternary in age and the rest of the core, down to the bottom at 147.69 mbsf, is of early Miocene age. Although not biostratigraphically significant, the dinocysts are the first in situ Quaternary and Miocene dinocysts reported from East Antarctica, and constitute the most diverse assemblage recovered from any firmly dated Neogene section from Antarctica. In addition, they confirm that cyst-producing dinoflagellates were present in Antarctic waters during the Neogene and Quaternary. The core can be divided into three intervals based on their palynomorph assemblages (Quaternary, 0-43.55 mbsf; lower Miocene, 43.55-99.10 mbsf; and lower Miocene, 99.10- 147.69 mbsf). The distinctive palynomorph assemblages are interpreted to reflect changing climatic conditions that prevailed at the time of deposition. Overall, conditions appear to have deteriorated up-section.
DOI: 10.15468/duna8f
title: Range table from planktonic foraminifers in ODP Hole 177-1089D
DOI: 10.15468/fsbxw7
title: Table 1. Species richness and abundance of the benthic infauna of the North Sea, 1980-1985
DOI: 10.15468/cmfeau
title: Phytoplankton abundance in surface water in September 1997, Chimbote, Peru
DOI: 10.15468/xphqqb
title: Appendicularia abundance of station M9_A near the Great Meteor Bank, Northeast Atlantic (Table 1)
DOI: 10.15468/fap55y
title: Range table from planktonic foraminifers in ODP Hole 183-1139A
DOI: 10.15468/7r4sc5
title: Abundance of radiolaria at station UT99-23-2
DOI: 10.15468/rh7yzk
title: (Appendix E) Stable carbon and oxygen isotope composition of Globigerinoides sacculifera of ODP Hole 121-758B
DOI: 10.15468/rbx5hm
title: Meiofauna abundance in sediment core 54301-010
DOI: 10.15468/zbmpp6
title: Ostracoda abundance of Hole 24-238
DOI: 10.15468/g5xb59
title: Phytoplankton abundance in surface water in November 1997, Pisco, Peru
DOI: 10.15468/ndwruj
title: Total foraminifera counts of multinet M21/5_MSN731
DOI: 10.15468/5svnpf
title: Planktic foraminifera abundance of Hole 72-516F
DOI: 10.15468/vvkm2b
title: (Appendix 4, Table 4) Relative abundances of benthic foraminifera in Late Quaternary sediments of core RC09-150 in the southeast Indian Ocean
DOI: 10.15468/z73yww
title: Benthic foraminifera abundance of Hole 96-624
DOI: 10.15468/xh3sz6
title: Range table from planktonic foraminifers in ODP Hole 183-1136A
DOI: 10.15468/8xdy5r
title: Living benthic foraminifera at station M33/1_MC-13 (WAST-T), size fraction 63-125 µm
DOI: 10.15468/sbk6as
title: Planktic foraminifera abundance of Hole 23-219
DOI: 10.15468/8zjjme
title: Assemblage of living benthic foraminifera in sediment core SO118_MC-51, 63-125 µm fraction
DOI: 10.15468/tnypkx
title: Total foraminifera counts of multinet M26/1_MSN845
DOI: 10.15468/jm3v4n
title: Percentages of planktonic foraminifera species in sediment core V15-168
DOI: 10.15468/gu3paa
title: Nannofossil abundance of Hole 20-200
DOI: 10.15468/ns6cy4
title: Phytoplankton abundance at station Casma_2003-03-27_2, Casma, Peru
DOI: 10.15468/nxs8f6
title: Assemblage of living benthic foraminifera in sediment core SO119_MC501, 30-63 µm fraction
DOI: 10.15468/g8dprd
title: Numbers and statistics of benthic foraminiferal Q-mode assemblages for the Lower Oligocene of section Poetschbichl in the Lower Inn Valley area
DOI: 10.15468/rd5wwc
title: Distribution of ostracoda in the Arctic Ocean (Table 1)
DOI: 10.15468/s4hgxk
title: (Table 2) Distribution of planktonic foraminifera in the upper Turonian-lower Campanian succession in ODP Hole 122-763B, Part III
DOI: 10.15468/4zydgg
title: Microzooplankton abundance and biomass at station NBP97-08-23-6
DOI: 10.15468/u3xyj5
title: Distribution of Quinqueloculina sp. in sediment core 13077-093
DOI: 10.15468/xgd23m
title: Range table from planktonic foraminifers in ODP Hole 157-954A
DOI: 10.15468/cfhcw3
title: Range table from benthic foraminifers in ODP Hole 189-1169A
DOI: 10.6084/m9.figshare.24498496.v1
title: Individual-Based Model use in Marine Policy

description: Individual-based models (IBMs) are increasingly used in marine conservation research, making this is an ideal time to assess IBM use in marine policy. IBMs can contribute important information to marine management and policy questions, as they offer complex methods of understanding ecosystems and animal behaviour, by allowing for heterogeneity in both individuals and environments. A review of 108 international peer-review publications utilizing marine IBMs was conducted using Web of Science (WoS). It was determined that 55% of the WoS articles claimed that the IBMs were relevant or important to marine conservation policy or management. A relevant English-language policy document was located for 83% of the IBMs, but only 32% were cited, while 85% of the same policy documents cited a different, non-IBM, modelling method. A separate survey of 175 policy documents from the Government of Canada was conducted. Of the 60 that contained citations, zero documents cited an IBM, while 75% cited a different modelling method. Of 407 webpages reviewed from the National Oceanic and Atmospheric Administration, the New Zealand Department of Conservation, and the UK Government website, only 4% referenced IBMs. This research demonstrates that, despite claims of usefulness by researchers, IBMs are not used to inform policy, while other model methods are commonly cited. Modellers should not assume that their model will inherently be useful for policy and should instead ensure that they are: 1) addressing a policy need; and 2) making the information accessible to policymakers by crafting a communication plan and/or joining a relevant boundary organization.
DOI: 10.15468/masgeg
title: (Table 1) Distribution of planktonic foraminifera species in Core ML2_66
DOI: 10.15468/fpdthx
title: Total foraminifera counts of trap L2_92_A42
DOI: 10.6084/m9.figshare.24498496
title: Individual-Based Model use in Marine Policy

description: Individual-based models (IBMs) are increasingly used in marine conservation research, making this is an ideal time to assess IBM use in marine policy. IBMs can contribute important information to marine management and policy questions, as they offer complex methods of understanding ecosystems and animal behaviour, by allowing for heterogeneity in both individuals and environments. A review of 108 international peer-review publications utilizing marine IBMs was conducted using Web of Science (WoS). It was determined that 55% of the WoS articles claimed that the IBMs were relevant or important to marine conservation policy or management. A relevant English-language policy document was located for 83% of the IBMs, but only 32% were cited, while 85% of the same policy documents cited a different, non-IBM, modelling method. A separate survey of 175 policy documents from the Government of Canada was conducted. Of the 60 that contained citations, zero documents cited an IBM, while 75% cited a different modelling method. Of 407 webpages reviewed from the National Oceanic and Atmospheric Administration, the New Zealand Department of Conservation, and the UK Government website, only 4% referenced IBMs. This research demonstrates that, despite claims of usefulness by researchers, IBMs are not used to inform policy, while other model methods are commonly cited. Modellers should not assume that their model will inherently be useful for policy and should instead ensure that they are: 1) addressing a policy need; and 2) making the information accessible to policymakers by crafting a communication plan and/or joining a relevant boundary organization.
DOI: 10.15468/ja9w3n
title: (Appendix A) Sea surface temperture reconstruction for ODP Hole 117-723A
DOI: 10.15468/ragjhv
title: (Table 1) Distribution and numerical abundance of foraminifera of sediment core CRP-3

description: A foraminiferal fauna comprising c. 33 genera and c. 53 species was recovered from a suite of 156 Lower Oligocene sediment samples, mostly muddy sandstone and siltstone, selected over the 2.80 - 823.11 mbsf depth range in the CRP-3 drillhole. All foraminifers, except for 2 isolated specimens, occurred above 340 mbsf, with 54 of 103 samples from above this depth being fossiliferous. At a generic and even a specific level, the fauna contains many components for the present-day Antarctic foraminiferal biota, indicating that its origin is at least as old as early Oligocene. Foraminiferal assemblages represent a single biofacies which is characterised by low diversity, and by dominant and persistent occurrences of Cassidulinoides chapmani, other Cassidulinoides and Globocassidulina species, and Stainforthia sp. These taxa and commonly accompanied by Cibicides lobatulus, Epistominella exigna, Fissurina spp. Nonionella spp., and Oolina spp. Large miliolids occur as isolated specimens at various levels. Planktic species are absent, and agglutinated taxa occur only rarely and sporadically. Preservation generally is fair good, while absolute abundance is very low, with a maximum of c. 6 specimens/gram, and most samples containing &lt;1 specimen/gram. These assemblages probably represent mid to outer shelf depth (50-200 m) in glacially influenced environments with a high sedimentation rate and poor oceanic connections. Although the CRP-3 fauna closely resembles the one from Foraminiferal Unit III as defined in CRP-2/2A (CRP-2/2A Science Team, 1999; Strong & Webb, 2000, hdl:10013/epic.28260.d001), absence of some species, and the first records of others in the uppermost CRP-3 section, is consistent with an interpretation of minimal overlap between the CRP-2/2A and CRP-3 sediments. The fauna also appears correlative with the Globocassidulina-Cassidulinoides-Trochoeiphidiella Assemblage Zone from lower DSDP-270, and with faunas from the lower but not lowermost, section at CIROS-1.
DOI: 10.15468/z76jkm
title: Distribution of planktic foraminifera (250-500 µm) of sediment core PS1244-2
DOI: 10.15468/dvystg
title: (Table 2) Distribution of benthic foraminifera on sediment core PS2138-1
DOI: 10.15468/wpuaa8
title: Relative abundance of dead benthic foraminifera in the large size fraction of surface sediment off NW Africa (Table 4)
DOI: 10.15468/ty9xbw
title: (App 2) Relative contents of benthic foraminifera species in Holocene sediments from Core ASV11-858-3
DOI: 10.15468/yrvhg5
title: (Table 1) Percentage of Coccolithus pelagicus vs. Reticulofenestra spp. of ODP Hole 120-747A
DOI: 10.15468/vd3fu2
title: Planktic foraminifera abundance of Hole 42-372
DOI: 10.15468/7qd2nr
title: (Table 6) Ostracod assemblages of sediment core 9409
DOI: 10.15468/fmje3w
title: (Figure 7) Distribution chart of benthic foraminifers in ODP Site 126-793
DOI: 10.15468/4yccqb
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/009-2
DOI: 10.15468/aphg6r
title: Planktic foraminifera counts of sediment core V04-8
DOI: 10.15468/b4pqpc
title: Distribution of major planktic foraminifer at Site 177-1090
DOI: 10.15468/bhvufw
title: (Table 9) Dinoflagellate cyst species distribution in ODP Hole 112-684B
DOI: 10.15468/xfha94
title: Microplankton abundance at Station MARCH-1997-GN36199704601MSB02 in the euphotic zone of the Aegean Sea in spring 1997. Part 1 - diatoms
DOI: 10.15468/96yp8a
title: Dead benthic foraminifera of surface sediments from the East Atlantic continental margin off Portugal (Table 5 & 7)
DOI: 10.15468/j46kyt
title: (Table 2) Distribution of Cretaceous nannofossils at DSDP Hole 79-545
DOI: 10.15468/d5naja
title: Pollen data of trap CB4
DOI: 10.15468/tx7rxc
title: Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0004C
DOI: 10.15468/war4t4
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-11-5
DOI: 10.15468/dcaspu
title: Large protozoan and small metazoan abundance measured on concentrated water bottle samples at station PS65/593-14
DOI: 10.15468/y6vr4c
title: Phytoplankton abundance at station Rigel_5_2005-02 in Febraury 2005, Chipana, Chile
DOI: 10.15468/kghbkr
title: Abundance of planktic foraminifera at CTD station PS55/080-1
DOI: 10.15468/rv4yy6
title: Distribution of planktic foraminifera of sediment core M35003-4
DOI: 10.15468/p2h5z9
title: (Table 3) Relative abundance of benthic foraminifera in sediment profile HUD84-030-04
DOI: 10.15468/6hgc9b
title: Nannofossil abundance of Hole 3-15
DOI: 10.15468/bu5jbm
title: Pollen analysis of sediment profile KAI2 from Kaiserwinkel
DOI: 10.15468/qddcy5
title: (Table 3) Stratigraphic ranges of selected Oligocene planktonic foraminifers in ODP Hole 115-707A
DOI: 10.15468/hg7q5j
title: Microplankton abundance at Station SEPT-1997-GN36199704605MSB02 in the euphotic zone of the Aegean Sea in September 1997. Part 2 - dinoflagellates
DOI: 10.15468/szahse
title: Sea surface temperature and salinity reconstructions for sediment core LaPAS-KF02
DOI: 10.15468/ftv79h
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V28-127
DOI: 10.15468/mk5wwy
title: Total foraminifera counts of multinet M21/1_MSN606
DOI: 10.15468/p3pp52
title: (Table 2) Abundance of benthic foraminifers of sediment core PS2445-2
DOI: 10.15468/6g4dj9
title: Planktic foraminifera abundance of Hole 18-173
DOI: 10.15468/yv7uuu
title: Table A3. Benthic foraminifera assemblage of sediment core GeoB1710-3
DOI: 10.15468/3pkk8a
title: Distribution of planktic foraminifera (250-500 µm) of sediment core GIK23059-3
DOI: 10.15468/r3tpvf
title: Relative abundance of dead benthic foraminifera of sediment core M5/2_93MC
DOI: 10.15468/bjkeez
title: Analyses of the recent components in the sand fraction of sediment core PS1278-1
DOI: 10.15468/gt7kqj
title: Microplankton counts and carbon biomass at station TT011_4-CTD46
DOI: 10.15468/sndtjw
title: (Table 14) Calcareous nannofossil occurrences in ODP Hole 130-806B
DOI: 10.15468/qa84gf
title: (Figure 10) Range chart of selected dinocysts and acritarchs of ODP Hole 104-644B
DOI: 10.15468/kkb38n
title: Planktic foraminifera abundance of Hole 84-567A
DOI: 10.15468/u8x36h
title: Range table from planktonic foraminifers in ODP Hole 159-960C
DOI: 10.15468/5tn2dh
title: Nannofossil abundance of Hole 24-237
DOI: 10.15468/jpuy8m
title: Lower Albian l'Arboudeysse section (Niveau Paquier) individuals per gram sediment of benthic foraminifera, in SE France
DOI: 10.15468/m2wy67
title: Nannofossil abundance of Hole 3-18
DOI: 10.14284/543
title: LifeWatch observatory data: zooplankton observations by imaging (ZooScan) in the Belgian Part of the North Sea

description: In the framework of the Lifewatch marine observatory a number of fixed stations on the Belgian Part of the North Sea (BPNS) are visited on a monthly or seasonal basis using the RV Simon Stevin. A grid of nine stations covers the coastal zone and are sampled monthly. Eight additional stations, located further at sea, are sampled on a seasonal basis. This dataset contains zooplankton observations in the Belgian Part of the North Sea (BPNS) since 2012. Zooplankton is sampled by vertical WP2 net tows, samples scanned with ZooScanner and identification with plankton analyser software, followed by manual validation.
DOI: 10.15468/2gu8hk
title: Abundance of phytoplankton in the Marmara Sea collected during the Bilim 2 cruise in Oktober 2008

description: The dataset is composed of 22 samples from 14 stations. The phytoplankton samples were collected by 5l Niskin bottles attached to the CTD system. The sampling depths were selected according to the CTD profiles and the in situ fluorometer readings. The samples (50 ml sea water) were preserved with prefiltered (0.2 micron) glutardialdehyde solution (1.5 ml of commercial glutardialdehyde (25%)) into dark colored glass bottles. Preserved samples were poured into 10 or 25 ml settling chambers (Hydro-Bios) for cells to settle on the bottom over a day. Species identification and enumeration were done under an inverted microscope (Olympus IX71). At least 400 specimen were tried to be counted in each sample.
DOI: 10.15468/m7aj4q
title: Plasm bearing foraminifera counts of multinet M21/1_MSN604
DOI: 10.15468/5rvhcz
title: (Table 4) Planktonic foraminifer species distribution, abundance, and preservation in DSDP Site 92-599
DOI: 10.15468/cze3d2
title: Faunal assemblage of sediment core GS7603-8
DOI: 10.15468/mc9vwk
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/092-6
DOI: 10.15468/y4c6kr
title: Microplankton abundance at bottle station SEPT-1999-K7
DOI: 10.15468/kz5dx4
title: Pollen analysis of sediment profile BLA00 from Blankensee
DOI: 10.15468/knk3g2
title: Phytoplankton abundance and species composition in the Gulf of Naples in March 1999 at Station MCSSI-phyto29-38
DOI: 10.15468/g82f3a
title: (Table 3c) Distribution of planktonic foraminiferal tests in sediments from Core NKA-40T
DOI: 10.15468/2bkbqd
title: Nano and microzooplankton abundance and biomass at station NBP97-01-05-10
DOI: 10.15468/3j6rxn
title: Distribution of agglutinated foraminifers in sediment core Well 6406/11-1
DOI: 10.15468/cjhmse
title: Range table from planktonic foraminifers in ODP Hole 171-1052E
DOI: 10.15468/hpp8cc
title: Plasm bearing foraminifera counts of multinet M36/6_MSN1194
DOI: 10.15468/gd2f79
title: Nannofossil abundance of Hole 25-249
DOI: 10.15468/39rjur
title: Plasm bearing foraminifera counts from multinet SO119_MSN1284
DOI: 10.15468/cmu7sm
title: (Table 3B) Occurrence and estimated abundance of planktonic foraminifers at DSDP Holes 85-572C and 85-572D
DOI: 10.15468/a8r5zc
title: (Table 2) Relative abundance of benthic foraminifera in sediment core CD17-30
DOI: 10.15468/b7sy89
title: Microzooplankton abundance measured on water bottle samples at station PS65/514-2
DOI: 10.15468/emghku
title: Foraminifera abundance of Hole 57-440A
DOI: 10.15468/fbp4tp
title: Size of planktic foraminifera at CTD station M39/4_402CTD-55
DOI: 10.15468/sd2r5u
title: Assemblage of living benthic foraminifera in sediment core SO118_MC-52, 63-125 µm fraction
DOI: 10.15468/d8f7p3
title: Planktic foraminifera abundance of Hole 72-518
DOI: 10.15468/yrrw8j
title: Benthic foraminiferal assamblage in the 125-250 micron fraction of sediment core PS1906-1 (Table 6)
DOI: 10.15468/99jsdy
title: (Figure 2) Occurrence of planktonic foraminifers and other selected constituents in samples from DSDP Hole 80-548
DOI: 10.15468/7y2aph
title: Occurrence of mammalia relicts at site Sütto_6
DOI: 10.15468/zkjns5
title: (Table 7) Fatty acid composition of adipose tissue from polar bears (Ursus maritimus) between 1991-2007
DOI: 10.15468/nxq2sy
title: Benthic foraminifera and algae abundance of Hole 35-325
DOI: 10.15468/q3fgza
title: Pollen profile from Seminary School Basin
DOI: 10.15468/2bag9a
title: (Table 13) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-715A
DOI: 10.15468/sff949
title: Microzooplankton abundance and biomass at station TT043_4-1
DOI: 10.15468/wnrcyb
title: Benthos counted on dredged samples during Valdivia cruise VA53
DOI: 10.15468/ykv8bb
title: Abundance and carbon biomass of phytoplankton at station TT012_5-CTD63
DOI: 10.15468/45cnyu
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V28-56
DOI: 10.15468/j4yv3n
title: Calcareous dinoflagellate cysts of multicorer M51/3_562-5, grain fraction &lt; 20µm
DOI: 10.15468/r3zgyn
title: Nematode genera abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/312-1
DOI: 10.15468/jg77dc
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC08-145
DOI: 10.15468/kggshn
title: Range table from benthic foraminifera in ODP Hole 199-1215B
DOI: 10.15468/zmv2ue
title: (Table 3) Distribution of late Cretaceous nannofossils in DSDP Hole 77-538A
DOI: 10.15468/aaewm9
title: (Table 2) Pleistocene nannofossil range chart for ODP Hole 134-828A
DOI: 10.15468/ckqsvu
title: Plasm bearing foraminifera counts of multinet POS231/3_MSN1335
DOI: 10.15468/ncpmnm
title: Nannofossil abundance of Hole 15-146A
DOI: 10.15468/zwa6tc
title: Plasm bearing foraminifera counts from M35/1_MSN1074
DOI: 10.15468/4tu7e7
title: (Table 1) Planktonic foraminifera community at DSDP Hole 94-608
DOI: 10.15468/4kfz3e
title: Microplankton abundance in the euphotic zone of the Aegean, Levantine and Ionian Seas in March-April 1987
DOI: 10.15468/794kt2
title: Foraminifera abundance of sediment core C1960.201
DOI: 10.15468/ftdee7
title: Benthic foraminifera abundance of Hole 84-570
DOI: 10.15468/87mv3s
title: Planktic foraminifera assemblage in sediment core SU90-I06
DOI: 10.15468/kq5wcm
title: Planktic foraminifera counts of sediment core V16-20
DOI: 10.15468/ycrygd
title: (Table 3) Abundance of planktonic foraminifera in ODP Hole 115-708A
DOI: 10.15468/a9zn8u
title: (App 3) Relative contents of benthic foraminifera in sediments from Core ASV1200
DOI: 10.15468/w5vqdr
title: Abundance of calcareous dinoflagellates of sediment core GeoB1214-1