cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/4gcpyh
title: Microzooplankton abundance measured on water bottle samples at station PS58/045-2
DOI: 10.15468/ds5jkm
title: (Table 2) Distribution of benthic foraminifers at DSDP Site 90-591
DOI: 10.15468/zgdyga
title: Range table from benthic foraminifers in ODP Hole 188-1165B
DOI: 10.15468/h46859
title: Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0001A
DOI: 10.15468/fs8q6h
title: Calcareous dinoflagellate cysts of surface sediment samples
DOI: 10.15468/dgxyjq
title: Phytoplankton abundance in surface water in September 1996, Pisco, Peru
DOI: 10.15468/npetss
title: (Appendix 1) Planktonic foraminifera abundances in ODP Site 181-1123
DOI: 10.15468/fjujq3
title: (Table S2b) Nannofossil species richness in the Wilson Lake section
DOI: 10.15468/9es9da
title: Microplankton abundance in the euphotic zone of the Levantine Sea in October-November 1991
DOI: 10.15468/mmz8me
title: (Table 1) Planktonic foraminifer stratigraphy in ODP Hole 167-1021C sediments
DOI: 10.15468/x2vx5s
title: Range table from benthic foraminifers in ODP Hole 160-967E
DOI: 10.15468/q6hprb
title: Sarcodine counts and carbon biomass at station TT007_9-CTD108
DOI: 10.15468/54wfsq
title: Occurrence of mammalia relicts at site Kesslerloch
DOI: 10.15468/afangz
title: Nannofossil abundance of Hole 29-284A
DOI: 10.15468/czbcc3
title: Planktic foraminifera assemblage in sediment core GIK23055-2
DOI: 10.15468/frdg5y
title: (Appendix 2-7) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 59-451 in the western Pacific Ocean
DOI: 10.15468/5yzwrw
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/043-2
DOI: 10.15468/9mf5gs
title: Late Cretaceous ostracods recorded from ODP Hole 113-689B

description: Twenty-six deep-sea ostracod species are described from the late Campanian to late Maastrichtian of ODP Site 689 in the Southern Ocean. Three are described as new: Cytherelloidea megaspirocostata, Agulhasina sudoceanica and Pennyella foveolata. Correspondence analysis identified three faunal sample groups. The first is mainly characterised by A. sudoceanica, Kirthe sp. and Cytherella sp. This is replaced, first temporarily (between c. 71 and 69 Ma) by a group mainly characterised by Argilloecia spp. and C. megaspirocostata, possibly a consequence of a short-lived global palaeoceanographic event marked by increased ventilation and cooling of intermediate waters at site 689. It then reappears before finally being replaced by a third group largely characterised by Eucythere cf. circumcostata, P. foveolataand Dutoitella mimica Dingle. This final change is coeval with a marked increase in the faunal density of ostracods, probably owing to an increase in food supply. However, the oxygen isotopic records of benthonic foraminifera suggests that the replacement of the first ostracod group by the third is a result of the long term Maastrichtian cooling of intermediate waters at high latitudes. This replacement is also coeval with a gradual change in benthonic foraminiferal assemblages at site 689. It is suggested, therefore, that Pennyella and Dutoitella had a greater potential of adapting to successively colder palaeoceanographical conditions than Agulhasina. The former genera have a cosmopolitan deep-sea distribution today.
DOI: 10.15468/6k7y59
title: (Table 1.2.1.1) Abundance of sympagic meiofauna of sea-ice core PS69/565-1
DOI: 10.15468/vkd4dn
title: Total foraminifera counts of trap L2_92_B50
DOI: 10.15468/4r53gy
title: Summary of ecologically and stratigraphically important foraminifera in surface samples of the NW African continental margin (Table 3)
DOI: 10.15468/ggbrsb
title: (Table 16) Distribution of ostracode species in Core PS51/080-13
DOI: 10.15468/vf93tm
title: (Table T15) Planktonic foraminifera stratigraphy of ODP Hole 198-1211A, Zones P6b-P8
DOI: 10.15468/8nkry6
title: Planktic foraminifera abundance of Hole 67-498
DOI: 10.15468/uumbyj
title: Planktic foraminifera abundance of Hole 23-229
DOI: 10.15468/yz4mkp
title: Nannofossil abundance of Hole 31-297
DOI: 10.15468/5vxw4g
title: Phytoplankton abundance at station Rigel_6_2005-04 in April 2005, Chipana, Chile
DOI: 10.15468/w879ra
title: Occurrence of mammalia relicts at site Dolni Vestonice
DOI: 10.15468/wkada2
title: Occurrence of mammalia relicts at site Euerwanger Bühl
DOI: 10.15468/grhemt
title: Nannofossil abundance of Hole 66-489A
DOI: 10.15468/rkvvsy
title: Planktic foraminifera abundance of Hole 39-354
DOI: 10.15468/xfya8c
title: Foraminifera abundance of Hole 60-455
DOI: 10.15468/9ubdea
title: Distribution of Quinqueloculina sp. in sediment core 13200-077
DOI: 10.15468/cuf5t2
title: Benthic foraminiferal abundances from eight sites of the Northwest Australian shelf

description: Foraminiferal analysis of Miocene to recent strata of the Northwest Shelf of Australia is used to chart West Pacific Warm Pool (WPWP) influence. The assemblage is typified by "larger" foraminifera with ingressions of the Indo-Pacific "smaller" taxa Asterorotalia and Pseudorotalia at around 4 Ma and from 1.6 to 0.8 Ma. A review of recent and fossil biogeography of these taxa suggests their stratigraphic distribution can be used to document WPWP evolution. From 10 to 4.4 Ma a lack of biogeographic connectivity between the Pacific and Indian Ocean suggests Indonesian Throughflow (ITF) restriction. During this period, the collision of Australia and Asia trapped warmer waters in the Pacific, creating a central WPWP biogeographic province from the equator to 26°N. By 3 Ma Indo-Pacific species migrated to Japan with the initiation of the "modern" Kuroshio Current coinciding with the intensification of the North Pacific Gyre and Northern Hemisphere ice sheet expansion. Indo-Pacific taxa migrated to the northwest Australia from 4.4 to 4 Ma possibly because of limited ITF. The absence of Indo-Pacific taxa in northwest Australia indicates possible ITF restriction from 4 to 1.6 Ma. Full northwest Australian biogeographic connectivity with the WPWP from 1.6 to 0.8 Ma suggests an unrestricted stronger ITF (compared to today) and the initiation of the modern Leeuwin Current. The extinction of some Indo-Pacific species in northwest Australia after 0.8 Ma may be related to the effects of large glacial/interglacial oscillations and uplift of the Indonesian Archipelago causing Indonesian seaway restriction.
DOI: 10.15468/dksxjf
title: Assemblage of living benthic foraminifera in sediment core SO117_MC468, &gt;125 µm fraction
DOI: 10.15468/vb3wc6
title: Meiofauna abundances in sediments from the Storegga Slide (Norwegian Sea) obtained during the VICKING expedition in 2006
DOI: 10.15468/d99fjm
title: Ostracoda abundance of Hole 13-132
DOI: 10.15468/cr4cst
title: Planktic foraminifera abundance of Hole 62-463
DOI: 10.15468/m746nd
title: (Table 10B) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 90-588A
DOI: 10.15468/brzvqe
title: Sarcodine counts and carbon biomass at station TT011_3-CTD33
DOI: 10.15468/jy8ema
title: (Table T3) Calcareous nannofossil stratigraphy of ODP Hole 198-1207B
DOI: 10.15468/chg9ej
title: Phytoplankton abundance and species composition in the Gulf of Naples in June 1999 at station MCSSII-phyto75-83
DOI: 10.15468/hghxfq
title: Nannofossil abundance of Hole 11-104
DOI: 10.15468/mvc6n8
title: Planktic foraminifera counts at CTD station PS55/037
DOI: 10.15468/gu68kz
title: Abundance of benthic infauna in surface sediments from the North Sea sampled during HEINCKE cruise HE133
DOI: 10.15468/f8u7k4
title: Diatom abundance measured on water bottle samples at station PS58/043-2
DOI: 10.15468/4tyefk
title: Phytoplankton abundance at station Casma_2003-03-13_2, Casma, Peru
DOI: 10.15468/tcenjz
title: Analyses of the recent components of sediment core PS1016-1
DOI: 10.15468/42unn7
title: Total foraminifera counts from M35/1_MSN1053
DOI: 10.15468/45yyde
title: Planktic foraminifera counts of sediment core V29-45
DOI: 10.15468/bmajtg
title: Range table from planktonic foraminifers in ODP Hole 139-857C
DOI: 10.15468/8hhzkw
title: Range table from planktonic foraminifers in ODP Hole 139-856A
DOI: 10.15468/p6b7ym
title: Dinoflagellate abundance of Hole 81-552A
DOI: 10.15468/kb96pq
title: (Table 4) Differences in king penguin (Aptenodytes patagonicus) colony arrivals and departures based on age, Possession Island
DOI: 10.15468/a3u38g
title: Dinoflagellate abundance of Hole 22-214
DOI: 10.15468/3mydgp
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1382
DOI: 10.15468/bwe58n
title: (Table 3) Ranges of upper Eocene Holocene planktonic foraminifera in ODP Hole 119-744A
DOI: 10.15468/jgp8d9
title: (Figure 7) Distribution and character of selected biogenic and lithologic components at DSDP Hole 79-545
DOI: 10.15468/fwej97
title: (Table 2) Planktic foraminiferal species and number of specimens present in 5 cc of sediment per sample at DSDP Site 77-540, Late Cretaceous
DOI: 10.15468/g6rxy8
title: Benthic foraminiferal assemblages (living), surface data
DOI: 10.22003/xfel.eu-data-900134-00
title: FastCCD Commissioning
DOI: 10.22003/xfel.eu-data-900173-00
title: Digitizer tests
DOI: 10.15468/zzpnut
title: Distribution of planktonic foraminifera of sediment core SH1972_2
DOI: 10.15468/c6yc2q
title: (Table T2) Plankontic foraminifera stratigraphy of ODP Hole 184-1146A
DOI: 10.15468/qzyjrz
title: Lower Cretaceous vertical distribution of calcareous dinoflagellate cysts in ODP Hole 122-761C

description: Low-diversity calcareous dinoflagellate cysts were studied by SEM in 10 samples from the Lower Cretaceous of Hole 761C (256-235 mbsf). The ?late Aptian/Albian age interval can be recognized because of the calcispheres present. The new orthopithonelloid genus Bitorus is introduced.
DOI: 10.15468/yvf9nw
title: (Table 12) Distribution of planktonic foraminifera shells with different preservation in deposits from DSDP Hole 30-289
DOI: 10.15468/p7tt86
title: Distribution of benthic foraminifers (living) in surface sediments (Table 4)
DOI: 10.22003/xfel.eu-data-900207-00
title: Maxeler project validation
DOI: 10.22003/xfel.eu-data-900264-00
title: Maxeler project validation
DOI: 10.22003/xfel.eu-data-900279-00
title: EEE Lab Digitizer Tests
DOI: 10.15468/3857n5
title: Planktic foraminifera counts of sediment core RC13-158
DOI: 10.15468/3xx57w
title: Total foraminifera counts from multinet M31/2_MSN893
DOI: 10.15468/qy4rz5
title: (Table 5) Distribution of planktonic foraminifers in ODP Hole 126-793A
DOI: 10.15468/2bgbc4
title: (Figure 5) Stratigraphic ranges of selected planktonic foraminifers at ODP Hole 101-627B
DOI: 10.15468/3ndv5w
title: Range table from planktonic foraminifers in ODP Hole 172-1054B
DOI: 10.15468/ex7unn
title: Distribution of planktic foraminifera (125-250 µm) of box sediment core PS1243-2
DOI: 10.15468/jaabd4
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB02 in the euphotic zone of the Aegean Sea in spring 1997. Part 1 - diatoms
DOI: 10.15468/mcahhk
title: Range table from benthic foraminifers in ODP Hole 181-1124C
DOI: 10.15468/49pynk
title: (Table 5a) Calcareous nannofossil distribution on ODP Hole 117-722A
DOI: 10.22003/xfel.eu-data-006076-00
title: Probing the Surface Diffusion of Gold Nano Bipyramids Near the Melting Using Optical Laser Pump and X-ray Probe Technique (SPI Experiment)
DOI: 10.15468/q234md
title: Phytoplankton abundance in surface water in March 1997, Pisco, Peru
DOI: 10.22003/xfel.eu-data-004417-00
title: Visualizing polaron formation in perovskite quantum dots
DOI: 10.15468/xy5kxt
title: Size of planktic foraminifera at CTD station PS55/077-1
DOI: 10.15468/37s5bt
title: Sarcodine counts and carbon biomass at station TT011_11-CTD142
DOI: 10.15468/f87sb5
title: (Table T5) Calcareous nannofossil stratigraphy of ODP Hole 198-1209C
DOI: 10.15468/zf9per
title: Planktic foraminifera abundance of Hole 60-456A
DOI: 10.15468/ebtfu8
title: Phytoplankton abundance and species composition in the Gulf of Naples in June 1999 at station MCSSII-phyto66-74
DOI: 10.15468/h5e4xr
title: (Appendix 2, Part 2) Distribution of Maestrichtian to Paleocene benthic foraminifera in ODP Site 113-689
DOI: 10.15468/jbsmdv
title: Percentages of planktonic foraminifera species in sediment core RC24-1
DOI: 10.15468/85mdcg
title: Total foraminifera counts from multinet M32/3_MSN958
DOI: 10.15468/xvxhfy
title: Nannofossil abundance of Hole 10-97
DOI: 10.15468/dnyrjz
title: Nano and microzooplankton abundance and biomass at station NBP97-01-15-3
DOI: 10.22003/xfel.eu-data-004463-00
title: Low-Z Mixtures at Planetary Interior Conditions
DOI: 10.22003/xfel.eu-data-006056-00
title: Commissioning of high signal-to-noise single particle imaging instrumentation at SPB/SFX
DOI: 10.15468/dyw2r3
title: Nannofossil abundance of Hole 39-357
DOI: 10.15468/35zr5a
title: Nannofossil abundance of Hole 9-83
DOI: 10.15468/zdseya
title: Benthic foraminifera distribution of sediment core ASV11-858-3 (ASV 858)
DOI: 10.15468/ap92v8
title: Assemblage of living benthic foraminifera in sediment core GeoB3705-2
DOI: 10.15468/wfz4g7
title: Dinoflagellates of sediment core GeoB1523-1

description: Large numbers of calcareous dinoflagellate cysts and the vegetative calcareous coccoid species Thoracosphaera heimii are generally found in sediments underlying oligotrophic and/or stratified (sub)surface water environments. It is difficult to distinguish between the relative importance of these two environmental parameters on calcareous cyst and T. heimii distribution as they usually covary, but this information is essential if we want to apply cysts properly in the reconstruction of palaeoenvironments and past surface water hydrography. In the multi-proxy core GeoB 1523-1 from the Ceará Rise region in the western equatorial Atlantic Ocean (covering the past 155 ka), periods of greatest oligotrophy are not synchronous with periods of greatest stratification (Rühlemann et al., 1996, doi:10.1016/S0025-3227(96)00048-5; Mulitza et al., 1997, doi:10.1130/0091-7613(1997)025&lt;0335:PFAROP&gt;2.3.CO;2; 335-338; Mulitza et al., 1998, doi:10.1016/S0012-821X(98)00012-0), giving us the unique opportunity to differentiate between the effects of both parameters on cyst accumulation. The calcareous cyst record of the core reflects prominent increases in accumulation rate of nearly all observed species only during the nutrient-enriched but more stratified isotopic (sub)stages 5.5, 5.3, 5.1 and 1. In this respect, the distribution trends in the core are more similar to those of the eastern equatorial upwelling region (GeoB 1105-4) than they are to those of the oligotrophic north-eastern Brazilian continental slope (GeoB 2204-2), even though temporal changes in bioproductivity are principally in antiphase between the eastern and western equatorial regions. We conclude that stratification of the upper water column and the presence of a well-developed thermocline are probably the more important factors controlling cyst distribution in the equatorial Atlantic, whereas the state of oligotrophy secondarily influences cyst production within a well-stratified environment.
DOI: 10.15468/b3pknp
title: Occurrence of mammalia relicts at site Condover
DOI: 10.15468/pjxrm3
title: Occurrence of planktic foraminifera in Pliocene to Holocene sediments of DSDP Hole 81-552A in the North Atlantic (Appendix 2)

description: A new planktic foraminifer transfer function (GSF18) related 5 North Atlantic assemblages to winter and summer sea surface temperature. GSF18, based on recombined and simplified core top census data, preserves most environmental information and reproduces modern North Atlantic conditions with approximately the same accuracy as previous transfer functions, but can be more readily applied to faunal samples ranging in age from Pliocene to Holocene. Transfer function GSF18 has been applied to faunal data from Deep Sea Drilling Project Hole 552A to produce a 2.5 m.y. sea-surface temperature (SST) time series. Estimates show several periods between 2.3 and 4.6 Ma during which mean SST's were both several degrees warmer and several degrees cooler than modern conditions. Between 2.9 and 4.0 Ma SST was generally warmer than modern except for a 250 k.y. interval centered at 3.3 Ma. Maximum SST, with respect to modern conditions, occurred after the cool interval near 3.1 Ma when SST was approximately 3.6° C warmer than present conditions. Comparison of SST estimates with stable isotope data suggest that after peak warming at 3.1 Ma, there was an overall surface water cooling with concomitant build up of global ice volume, culminating in Northern Hemisphere glaciation. This event is also indicated by the presence of ice rafted detritus in 552A sediments at about 2.45 Ma.
DOI: 10.15468/cavb2d
title: Nannofossil abundance of Hole 6-47
DOI: 10.15468/59yy2z
title: Coccolith counts of multinet M32/5_MSN982
DOI: 10.15468/97e7h8
title: Range table from benthic foraminifers in ODP Hole 159-962B
DOI: 10.15468/qag4m7
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/090-4
DOI: 10.15468/yb7u5x
title: Megafauna abundance and biomass from trawl samples obtained during cruise DI229
DOI: 10.15468/3f6aug
title: (Table T1) Neogene stratigraphy of diatoms, ebridians and endoskeletal dinoflagellates in ODP Hole 183-1138A
DOI: 10.15468/y2mefz
title: Total foraminifera counts from multinet M31/2_MSN887
DOI: 10.15468/y58u2f
title: Range table from planktonic foraminifers in ODP Hole 144-871A
DOI: 10.15468/vwp42j
title: (Table T5) Calcareous nannofossil stratigraphy of ODP Hole 198-1212B
DOI: 10.15468/ykq9sc
title: Planktic foraminifera abundance of Hole 80-550
DOI: 10.15468/x82ytp
title: (Table 2b) Downcore distribution of live benthic foraminifera of sediment core PS1394-3, Weddell Sea
DOI: 10.15468/weg68u
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB02 in the euphotic zone of the Aegean Sea in March 1998. Part 1 - diatoms
DOI: 10.15468/n45e8s
title: Analyses of the recent components of sediment core PS1223-1
DOI: 10.15468/pubcs4
title: Distribution of planktonic foraminifera in sediment core MD95-2041
DOI: 10.15468/an4fgc
title: Phytoplankton abundance during Alexander von Humboldt cruise AvH90/4
DOI: 10.15468/ztudbb
title: (Table 2) Distribution of planktonic foraminiferal species in bottom sediments from Core LV28-42-5, Sea of Okhotsk
DOI: 10.15468/7xff5y
title: Analyses of the recent components in the sand fraction of sediment core PS1402-2
DOI: 10.15468/esw4xt
title: Planktic foraminifera abundance of Hole 11-106
DOI: 10.15468/jerayb
title: Happywhale - Humpback Whale in Indian Ocean

description: Original provider: Happywhale Dataset credits: Happywhale and contributors Abstract: Happywhale.com is a resource to help you know whales as individuals, and to benefit conservation science with rich data about individual whales. Supplemental information: Sightings and images were submitted to Happywhale by contributors. A portion of the Happywhale data were transferred to OBIS-SEAMAP upon the agreement between Happywhale and OBIS-SEAMAP. There may be duplicate records among Happywhale datasets and other OBIS-SEAMAP datasets. The precision of date/time vary per record. Some records have date accuracy up to year only. This dataset includes sightings and photos from the following 35 contributors in alphabetic order: Alan Straton; Alex Bradshaw; Alex Vogel; Angie Gullan; Benjamin Wambergue; Bianca Tree; Brooke Lloyd; Cees Tineke; Conor Ryan; David Donnelly; Deb Philipps; Deep Voice; Devienne Gilles; Doriane; Dustin; Eddy Thys; EJs Encounters; Esther van der Stappen; Gary Allport; Gill Braulik; Lana; Linda Heads; Linda Horton; Marian Herz; Melanie Keyte; Michael Sheehan; Pamela Le Noury; Pedro Víctor Albaladejo Fresnadillo; peter allsop; Ramzy Haddad; Rodrigo A. Martinez Catalan; Sarah Gower; Violaine Dulau; Wayne Sentman; Yara Tibirica
DOI: 10.15468/uypz25
title: Foraminifera abundance of sediment core C1966.435
DOI: 10.15468/nchg8f
title: Ostracoda abundance of Hole 42-376
DOI: 10.15468/9y5rpc
title: Ostracoda abundance of Hole 48-405
DOI: 10.15468/9xzss9
title: Nannofossil abundance of Hole 9-77A
DOI: 10.15468/pqhh4t
title: Molluscs in surface sediments off Sylt collected during HEINCKE cruise HE255
DOI: 10.15468/s3mjpy
title: (Table 2) Occurrences of diatoms species in DSDP Hole 41-366
DOI: 10.15468/mbqqkf
title: Range table from benthic foraminifers in ODP Hole 172-1056B
DOI: 10.15468/vv5ac5
title: Assemblage of living benthic foraminifera in sediment core GeoB1720-3
DOI: 10.15468/fkg4ua
title: Benthic meiofauna abundance in surface sediment of core PLG93_BCORE4
DOI: 10.15468/4quk4v
title: Total foraminifera counts of multinet M21/3_MSN687
DOI: 10.15468/uy9yt8
title: Census of calcareous nannofossil taxa expressed as percent of total number of individuals counted, ODP Site 120-748
DOI: 10.15468/4urqvt
title: (Table T3) Calcareous nannofossil abundance of ODP Hole 189-1171A sediments
DOI: 10.15468/mzkkya
title: Size of planktic foraminifera at CTD station PS55/063
DOI: 10.15468/89prs2
title: Range table from planktonic foraminifers in ODP Hole 139-856G
DOI: 10.15468/4emqx3
title: Nannofossil abundance of Hole 16-156
DOI: 10.15468/sbn9ne
title: Fig. 11: Benthic foraminifera assemblage of sediment core MD97-2128
DOI: 10.15468/agz9kn
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/048-3
DOI: 10.15468/gjaq2f
title: (Appendix 2-5) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 31-296 in the western Pacific Ocean
DOI: 10.15468/kkqfr9
title: Assemblage of living benthic foraminifera in sediment core SO118_MC-43, 63-125 µm fraction
DOI: 10.15468/nzrpea
title: Range table from benthic foraminifers in ODP Hole 144-878A
DOI: 10.15468/rq4qqh
title: Coccoliths in sediment core PS1295-4
DOI: 10.15468/yjezqb
title: Assemblage of living benthic foraminifera in sediment core CD145_55803#5, 63-150 µm
DOI: 10.15468/ytws69
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB04 in the euphotic zone of the Aegean Sea in spring 1997. Part 1 - diatoms
DOI: 10.15468/vffqmq
title: Benthic foraminiferal number, diversity, and species abundance of size fraction &gt;125µm across sapropel S6 in core M40/4_KL51 from the lower bathyal of the western Levantine Basin
DOI: 10.15468/y2dfmm
title: Phytoplankton abundance at station Sechin_2003-12-17_1, Casma, Peru
DOI: 10.15468/49eepd
title: Abundance of planktic foraminifera at CTD station PS55/078-1
DOI: 10.15468/c4qj8r
title: Census of calcareous nannofossil taxa expressed as percent of total number of individuals counted, ODP Site 113-689
DOI: 10.15468/tb5pxy
title: Range table from planktonic foraminifers in ODP Hole 174-1073A
DOI: 10.15468/8jnbpg
title: Nannofossil abundance of Hole 67-494A
DOI: 10.15468/cmahjk
title: Foraminifera distribution of sediment core SDSE194
DOI: 10.15468/64h7mw
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station NOVEMBER-1994-D2
DOI: 10.15468/rheeze
title: Plasm bearing foraminifera counts of multinet M21/2_MSN641
DOI: 10.15468/mzhf7b
title: (Table 2) Benthic foraminiferal assemblage in the early Pleistocene interval of ODP Site 162-984
DOI: 10.15468/4dh6r2
title: Ostracoda abundance of Hole 11-105
DOI: 10.15468/44xusy
title: Relative abundance of planktonic foraminifera in sediment core L-198
DOI: 10.15468/7t3bvn
title: (Table 1) Relative abundances of benthic foraminifera in ODP Site 128-798C
DOI: 10.15468/chszjj
title: Occurrence of mammalia relicts at site Ettingen
DOI: 10.15468/aqjb8b
title: Total foraminifera counts from M35/1_MSN1058
DOI: 10.15468/eqzfh6
title: Nannofossil abundance of Hole 73-519
DOI: 10.15468/wv2ymq
title: Abundance of planktic foraminifera at CTD station PS55/025
DOI: 10.15468/9qbg8t
title: Planktic foraminifera assemblage in sediment core GeoB1113-4
DOI: 10.15468/ymv7qb
title: Analyses of the recent components in the sand fraction of sediment core PS1011-1
DOI: 10.15468/4z34xc
title: Abundance of nematoda in sediment profile M3/1_031 from the Iberian deep sea basin (Table 5)
DOI: 10.15468/8v46fe
title: Planktic foraminifera abundance of Hole 9-82A
DOI: 10.15468/yypf8e
title: (Appendix D) Total cyst counts, and abundances of Selenopemphix undulata sp. nov. in ODP Site 146-893
DOI: 10.15468/khvagt
title: Microfossil abundance of Hole 39-358