cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/xmsxw2
title: Total foraminifera counts from multinet M31/2_MSN894
DOI: 10.15468/7748xb
title: Benthic macrofauna abundance of sediment core 12930-084
DOI: 10.15468/jdgtqd
title: Nannofossil abundance of Hole 34-319
DOI: 10.15468/6dn387
title: Distribution of Upper Cretaceous deep water agglutinated foraminifera in sediments of the North Atlantic and its marginal seas (Tab. 1)

description: The stratigraphic and biogeographic distribution of more than 170 species of deep-water agglutinated benthic foraminifers (DWAF) from the North Atlantic and adjacent marginal seas has been compared with paleoenvironmental data (e.g. paleobathymetry, oxygenation of the bottom waters, amount of terrigenous input and substrate disturbance). Six general types of assemblages, in which deep water agglutinated taxa occur, are defined from the Turonian to Maastrichtian times: 1. High latitude slope assemblages 2. Low to mid latitude slope assemblages 3. Flysch-type assemblages 4. Deep water limestone assemblages (,,Scaglia,,-type) 5. Abyssal mixed calcareous-agglutinated assemblages 6. Abyssal purely agglutinated assemblages Latitudinal differences in faunal composition are observed, the most important of which is the lack or extreme paucity of calcareous forms in high latitude assemblages. East-to-west differences appear to be of comparatively minor importance. Most DWAF species occur in all studied regions and are thus considered as cosmopolitan. Biostratigraphic turnovers in the taxonomic content of assemblages are observed in the lowermost Turonian, mid-Campanian and in the upper Maastrichtian to lowermost Paleocene. These datum levels correspond to inter-regional and time-constant paleooceanographic events, which probably also affected the deep-water benthic biota. This allows us to use deep-water agglutinated foraminifers for biostratigraphy in the North Atlantic sequences deposited below CCD and to geographically extend the currently used zonal schemes which have been established in the Carpathian and Alpine areas.
DOI: 10.15468/9sp96q
title: Planktonic foraminifer occurrences and zonations from IODP Hole 313-M0027A
DOI: 10.15468/mbvg2e
title: Phytoplankton abundance and species composition in the Gulf of Naples in March 1999 at Station MCSSI-phyto57-65
DOI: 10.15468/sja39a
title: (Table 2) Abundances of planktonic and benthic foraminifera in ODP Hole 130-807A
DOI: 10.15468/znfewv
title: (Table 3) Range chart of calcareous nannofossils in ODP Hole 122-763B
DOI: 10.15468/8zpud9
title: (Table 2) Average major-element composition of glass shards from Toba Tephra Beds in Sumatra, Malaysia, India, and the Indian Ocean
DOI: 10.15468/m7usrz
title: (Table 3) Dinocyst ranges in ODP Hole 104-642D
DOI: 10.15468/r3ztau
title: Occurrence of mammalia relicts at site Sirgenstein
DOI: 10.15468/js9ef3
title: Planktic foraminifera assemblage in sediment core GIK23071-3
DOI: 10.15468/qjd7qb
title: Occurrence of mammalia relicts at site Bocksteingrotte/Lonetal
DOI: 10.15468/ba646r
title: Microplankton abundance at bottle station SEPT-1999-K1
DOI: 10.15468/pxj88m
title: Phytoplankton abundance in surface water in January 2007, Sechura Bay, Peru
DOI: 10.15468/83hmdv
title: (Table 1) Distribution of calcareous nannofossils in ODP Hole 167-1017E sediments

description: Ocean Drilling Program (ODP) Site 1017E (34°32.10'N, 121°6.43'W; 955.5 m water depth) is located on Santa Lucia Slope, ~50 km west of Point Arguello. The location of Hole 1017E, influenced by the California Current and associated coastal upwelling systems, is the best field to monitor paleoclimate change in the North Pacific. Living coccolithophorid is generally restricted in the photic zone and is one of the major primary producers in modern oceans. Thus, fossil coccolith assemblages can be used for paleoceanographic reconstruction in the surface waters. Winter (1985, doi:10.1016/0377-8398(85)90007-6) reported that the living coccolithophore flora in the California Current system of Southern California has significant variability in community structure, diversity, and standing crop. Wei and Peleo-Alampay (1995, doi:10.2973/odp.proc.sr.146-2.305.1995) reported that nannofossil diversity is low during oxygen isotope Stages 1-6 in the Santa Barbara Basin. These studies indicate that the low temperature and upwelling in the California Current system are responsible for the dominance of nannofossil flora in the California Borderland. However, very little is known about the paleoceanographic interpretation of nannofossil flora off Point Conception. The purpose of this report is to document the change in calcareous nannofossil assemblages for the last 27 k.y. in relation to the past surface water conditions at Hole 1017E.
DOI: 10.15468/jr5wqn
title: Nannofossil abundance of Hole 60-458
DOI: 10.15468/uf9r5r
title: Analyses of the recent components of sediment core PS1277-1
DOI: 10.15468/bcscqa
title: Nannofossil abundance of Hole 7-65
DOI: 10.15468/9mtfxh
title: (Table A.10) Foraminiferal census data of sediment core PS1243-2 during marine isotopic stage 1-3 (150-500 µm)
DOI: 10.15468/8xht38
title: Planktic foraminifera counts of sediment core RC08-49
DOI: 10.15468/2tn8wq
title: Total foraminifera counts of multinet M33/1_MSN1029
DOI: 10.15468/npb9vn
title: (Appendix A2) Cenomanian benthic foraminifera of ODP Site 207-1260
DOI: 10.15468/maen67
title: Plasm bearing foraminifera counts of multinet M12/3_MSN562
DOI: 10.15468/2se5rp
title: Faunal assemblage of sediment core TR149-31
DOI: 10.15468/g32x6h
title: (Table 12B) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 90-590B
DOI: 10.15468/fwhqfm
title: Large protozoan and small metazoan abundance measured on concentrated water bottle samples at station PS65/587-16
DOI: 10.15468/fr2yty
title: Planktic foraminifera abundance of Hole 29-284A
DOI: 10.15468/p9bc63
title: Matter enrichment of the macrofauna community of MAC station 13368-008
DOI: 10.15468/php767
title: Planktic foraminifera abundance of Hole 49-409
DOI: 10.15468/epbudd
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station SEPT-1998-IR64
DOI: 10.15468/rw2mej
title: Nannofossil abundance of Hole 10-91
DOI: 10.15468/x28626
title: (Table 2) Nannofossil occurrence in ODP Hole 101-627B
DOI: 10.15468/vj9yap
title: Phytoplankton abundance at station Casma_2003-01-30_2, Casma, Peru
DOI: 10.15468/6g5g7k
title: Dinoflagellate cyst counts on sediment core ABC26

description: In the reconstruction of bioproductivity in surface waters the extent to which a proxy has been diagenetically altered is often a matter of debate. Here we investigate how organic- and calcareous-walled dinoflagellate cysts can be used for separately estimating bioproductivity and oxygen related diagenesis. This is achieved by studying the cyst content of the most recent Eastern Mediterranean sapropel S1, that is thought to have been deposited under conditions of increased primary production in surface waters and possible anoxia in the bottom waters. Based on chemical evidence, it has been shown that the visible sapropelic layer represents only the residual lower part of what was initially a much thicker sapropel, as a result of post-depositional decay of organic matter related to oxygen penetration into the sediments. The effect of aerobic organic matter decay on the cyst associations is studied through the comparison of the unaffected, lower part of the initial sapropel and the 'oxidised' upper part. Comparing the unaffected sapropelic sediments with pre- and post-sapropelic material gives insight into the relationship between fossil cysts assemblages and palaeoproductivity. Impagidinium aculeatum, Impagidinium patulum, Operculodinium israelianum, Polysphaeridium zoharyi and probably Impagidinium spp., Impagidinium paradoxum and Nematosphaeropsis labyrinthus are very resistant against aerobic decay and their accumulation rates appear to be primarily related to productivity in surface waters. Protoperidinium and Echinidinium species, on the other hand, are shown to be very sensitive and can be used to recognise oxygen-related decay. The calcareous-walled dinoflagellate cysts seem to be unaffected by oxic organic matter decay in Mediterranean sediments.
DOI: 10.15468/kjx56d
title: Planktic foraminifera counts at CTD station M39/4_402CTD-55
DOI: 10.15468/en7q8v
title: Diversity, standing stock and distribution of living benthic foraminifera suborder groups (Table 3+5)
DOI: 10.15468/mqmffh
title: Total foraminifera counts of multinet M21/4_MSN704
DOI: 10.15468/bhnjg3
title: Abundance of broken diatom frustules measured on water bottle samples at station PS58/088-4
DOI: 10.15468/8pgb6z
title: Neogene palynomorpha from site 81-552
DOI: 10.15468/rj76gg
title: Relative abundance of planktic foraminifera in sediment core K708-001
DOI: 10.15468/ejerzy
title: Oberservation of birds at station PS14/143 along 49° West
DOI: 10.15468/nzw7y6
title: Benthic foraminiferal assamblage in the &gt;125 micron fraction of sediment core PS1745-5 (Table 8)
DOI: 10.15468/3fmbfd
title: Planktic foraminifera assemblage in sediment core SO42-74KL
DOI: 10.15468/bveprn
title: Nannofossil abundance of Hole 9-79
DOI: 10.15468/26eyv5
title: Occurrence of mammalia relicts at site Pestera Bursucilor
DOI: 10.15468/x58wn7
title: Range table from planktonic foraminifers in ODP Hole 155-930B
DOI: 10.15468/g4qxgb
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/j9pmwz
title: Foraminifera species abundances from tow TT011_7-MOC66
DOI: 10.15468/v9gxm5
title: Pollen profile ADR353
DOI: 10.15468/5megd8
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 159-959D
DOI: 10.15468/bp5vh7
title: Benthic macrofauna abundance of sediment core 13078-015
DOI: 10.15468/ktgpqh
title: (Table 2) Stratigraphic occurrence of selected diatom species from DSDP Hole 12-112
DOI: 10.15468/m498y9
title: (Table 2) Biostratigraphy of marine benthic and planktonic taxa in sediment core GIK14350 near Dagebüll, northern Germany

description: Together with foraminifers and ostracods, echinoderm remains are very frequent in Eemian sediments of the Dagebuell Well DA-1. The appearance of holothurian sclerites is particularly noteworthy. In the present study, remains of Holothuroidea from the European Pleistocene are described. These remains could be assigned to the Recent genus Psolus OKEN 1815. Furthermore, a short synopsis of disarticulate holothurian fossils in Holocene and Pleistocene sediments is given.
DOI: 10.15468/s43k7e
title: Plasm bearing foraminifera counts from multinet M32/3_MSN957
DOI: 10.15468/f5xpfu
title: (Table 1) Distribution of planktonic foraminifers in ODP Hole 126-787B
DOI: 10.15468/n9457y
title: Coccolith counts of multinet M32/5_MSN981
DOI: 10.15468/hhyfc2
title: Distribution of planktic foraminifera (250-500 µm) of sediment core PS1246-4
DOI: 10.15468/58esr3
title: Fossil occurrence of planktonic foraminifera from IODP Hole 322-C0011B
DOI: 10.15468/v72abd
title: Occurrence of mammalia relicts at site Veternica
DOI: 10.15468/ngqvhn
title: Occurrence of mammalia relicts at site la Grotte des Eglises
DOI: 10.15468/7eb6ng
title: Nannofossil abundance of Hole 15-149
DOI: 10.15468/vbxpk7
title: Analyses of the recent components in the sand fraction of sediment core PS1014-1
DOI: 10.15468/f99qeh
title: (Table T7) Calcareous nannofossil stratigraphy of ODP Hole 198-1210B
DOI: 10.15468/jxh6yd
title: Benthic foraminifera abundance of Hole 41-366A
DOI: 10.15468/w6bj6x
title: Total foraminifera counts of multinet POS247/2_MSN1386
DOI: 10.15468/p73gyy
title: Range table from planktonic foraminifers in ODP Hole 155-942C
DOI: 10.15468/22rdmz
title: (Fig. 5) Sea-surface temperature reconstructions of sediment core MD99-2304
DOI: 10.15468/h5du7s
title: (Table 4) Distribution of Upper Cretaceous agglutinated benthic foraminifers in ODP Hole 129-801A
DOI: 10.15468/rvz97t
title: Relative abundances of benthic foraminifers of sediment core Svanic90_9004
DOI: 10.15468/dyk5hf
title: Range table from planktonic foraminifers in ODP Hole 144-874B
DOI: 10.15468/c9h4pu
title: Pollen analysis of sediment profile TR0 from Truennensee
DOI: 10.15468/hjh233
title: Nannofossil abundance of Hole 78-543
DOI: 10.15468/yzhvcw
title: Microfossil abundance of Hole 16-158
DOI: 10.15468/vgh6fc
title: Total foraminifera counts of multinet FCA97C_MSN1339
DOI: 10.15468/vd22tw
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station MARCH-94-GN3619940280100500
DOI: 10.15468/6dyvdd
title: Abundance of epibenthic echinoderms at seafloor photography station POS196_1018
DOI: 10.15468/mc9fne
title: (Table 14) Distribution of planktonic foraminifers in ODP Hole 108-665A
DOI: 10.15468/n4pad8
title: Occurrence of mammalia relicts at site Geißenklösterle
DOI: 10.15468/sjhn9x
title: Planktic foraminifera counts of sediment core RC13-154
DOI: 10.15468/89fjr2
title: Composition of the coccolith flora in sediment core GeoB1710-3
DOI: 10.15468/zvfpuv
title: Microzooplankton abundance and biomass at station TT045_15-2
DOI: 10.15468/garz3h
title: Relative abundance of planktic foraminifera in sediment core RC08-39
DOI: 10.15468/9yu5pp
title: Benthic foraminifera abundance of Hole 84-566C
DOI: 10.15468/8vja9p
title: (Table 17) Nannoplankton distribution in sediment core ANS3-T4
DOI: 10.15468/mmk45v
title: (Appendix B) Relative abundances of larger size planktonic foraminifera in latest Maastrichtian sediments of DSDP Hole 74-525A from Walvis Ridge, South Atlantic
DOI: 10.15468/8rj33h
title: Total foraminifera counts of multinet M21/4_MSN720
DOI: 10.15468/5zsz7c
title: Range table from benthic foraminifers in ODP Hole 172-1059B
DOI: 10.15468/9qv833
title: Nannofossil abundance of Hole 37-333
DOI: 10.15468/aqna9v
title: (Table 1) Fauna composition of the community of Amphiodia urtica - Nephtys ferruginea in bottom sediments from the central part of the shelf in the California upwelling zone
DOI: 10.15468/h62cf6
title: Diatom assamblage in samples from sediment trap OG5
DOI: 10.15468/wk495a
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1389
DOI: 10.15468/ayp7sf
title: Planktic foraminifera counts at CTD station PS55/083-1
DOI: 10.15468/ekgpzv
title: Phytoplankton abundance at station Sechin_2003-07-15_2, Casma, Peru
DOI: 10.15468/mrgnkk
title: (Table 1) Dinoflagellate range chart of ODP Hole 120-748C
DOI: 10.15468/vwrkq4
title: (Table 15) Calcareous nannofossil occurrences in ODP Hole 130-805C
DOI: 10.15468/3j4dzz
title: (Appendix D) Analyses of the benthic foraminifer assemblage at ODP Hole 112-680B
DOI: 10.15468/9t3dnj
title: Plasm bearing foraminifera counts from M35/1_MSN1048
DOI: 10.15468/c54t9j
title: Dinoflagellate cysts of ODP Hole 189-1172D
DOI: 10.15468/n4kvkq
title: Planktic foraminifera abundance of Hole 45-395
DOI: 10.15468/kumr84
title: Planktic foraminifera abundance of Hole 19-191A
DOI: 10.15468/4cx426
title: (Table 2) Distribution of planktic foraminifers of sediment core D11957P
DOI: 10.15468/854dtk
title: Total foraminifera counts of multinet M36/6_MSN1196
DOI: 10.15468/fx64cc
title: Ostracod species in Oligocene sediments of core CRP-3
DOI: 10.15468/a7ge7v
title: Benthic macrofauna abundance of sediment core 13077-093
DOI: 10.15468/gnjgu7
title: Molluscs in surface sediments off Sylt collected during HEINCKE cruise HE293
DOI: 10.15468/a75krd
title: (Appendix 8) Distribution of barnacles, bivalves, gastropods, and calcified worm tubes in sediment samples collected between 1995 and 2010 in the San Francisco Bay coastal system
DOI: 10.15468/m7jyac
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station JULY-1994-D2
DOI: 10.15468/a47bv4
title: (Table 4) Distribution of Cretaceous calcareous nannofossils in ODP Hole 114-700B
DOI: 10.15468/5m7qtj
title: (Appendix Table 3) Relative abundances of planktonic foraminiferal species in sediment core MD01-2390
DOI: 10.15468/5tvkt5
title: (Table 2.2.1.1) Abundance of sympagic meiofauna of sea-ice core IO-11
DOI: 10.15468/ztdxtg
title: Benthic foraminifera counts of sediment core PS1852-2
DOI: 10.15468/vzgwfj
title: Planktonic foraminifer occurrences and zonations from IODP Hole 313-M0029A
DOI: 10.15468/f2scwj
title: Dead benthic foraminifera of surface sediment of the Persian Gulf (Table 2)
DOI: 10.15468/b3xrft
title: Range table from benthic foraminifers in ODP Hole 198-1207A
DOI: 10.15468/9rzn85
title: Planktic foraminifera counts at CTD station PS55/063
DOI: 10.15468/pdr2q8
title: (Figure 3) Stratigraphic distribution of planktonic foraminifera in the Neogene of ODP Hole 122-761B
DOI: 10.15468/8qjtg5
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 1984-1991. Part 2
DOI: 10.15468/cnrcrk
title: Microplankton counts and carbon biomass at station TT011_8-CTD96
DOI: 10.15468/48g5vd
title: (Table 4) Percentages of planktonic foraminiferal taxa from the 214 surface-sediment samples from the South China Sea and the western Pacific
DOI: 10.15468/jux3hw
title: Planktic foraminifera abundance of Hole 9-76
DOI: 10.15468/qx593h
title: (Table 15) Distribution of planktonic foraminifers in ODP Hole 108-666A
DOI: 10.15468/s82vsr
title: Total foraminifera counts of multinet FCA97C_MSN1345
DOI: 10.15468/x9tbu7
title: Benthic macrofauna abundance of sediment core 13200-008
DOI: 10.15468/yfaj9n
title: (Appendix 6) Benthic foraminifera at termination II in sediment core GIK23256-1 in the Arctic Ocean
DOI: 10.15468/c2dxx5
title: Phytoplankton abundance at station Rigel_1_2005-02 in Febraury 2005, Chipana, Chile
DOI: 10.15468/95g7ms
title: Dinoflagellate abundance of Hole 81-555
DOI: 10.15468/n3rqbz
title: Relative abundance of Neogene nannofossils at ODP Site 165-998 from the Caribbean
DOI: 10.15468/3guy43
title: Nannofossil abundance of Hole 27-259
DOI: 10.15468/tx6aaq
title: Benthic foraminifera abundance of Hole 93-603
DOI: 10.15468/xkuy9y
title: Occurrence of mammalia relicts at site Raagelund
DOI: 10.15468/dhcxkw
title: (Table A.01) Planktic foraminiferal census data of sediment core GIK23414-9
DOI: 10.15468/ghfmf4
title: Foraminifera abundance of Hole 64-481
DOI: 10.15468/xx477q
title: Planktic foraminifera counts of sediment core V27-178
DOI: 10.15468/emwzaf
title: Total foraminifera counts of multinet M21/2_MSN648
DOI: 10.15468/ugp8qm
title: Distribution of living benthic foraminifera in surface sediments of the Norwegian Sea (Table 2)
DOI: 10.15468/aevfs8
title: Planktic foraminifera abundance of Hole 14-142
DOI: 10.15468/u8bus7
title: Distribution of Quinqueloculina sp. in sediment core 12930-014
DOI: 10.15468/mtgzrd
title: Nannofossil abundance of Hole 73-521A
DOI: 10.15468/8k3pf6
title: Analyses of the recent components in the sand fraction of sediment core PS1276-1
DOI: 10.15468/xgkg6p
title: Phytoplankton abundance during Arnold Veimer cruise AV90/2
DOI: 10.15468/6qvk57
title: (Table T1) Calcareous nannofossil stratigraphy of ODP Site 198-1213
DOI: 10.15468/nf4yr4
title: Total foraminifera counts from M35/1_MSN1065
DOI: 10.15468/e6zf5q
title: Foraminifera abundance of Hole 33-317A
DOI: 10.15468/6qb357
title: Total foraminifera counts of multinet M21/2_MSN650
DOI: 10.15468/ebcsxp
title: Microzooplankton abundance and biomass at station NBP97-03-03-5
DOI: 10.15468/2jkb8t
title: Nannofossil abundance of Hole 67-499B
DOI: 10.15468/ruwyke
title: Foraminifera abundance of sediment core IN68-9
DOI: 10.15468/fb2ea7
title: Range table from planktonic foraminifers in ODP Hole 155-938A
DOI: 10.15468/ta5dhj
title: Results of palynological analysis of Hole 302-M0004C
DOI: 10.15468/zdj5dp
title: (Fig. 2) Abundance of Globobulimina affinis in sediment core MD95-2040
DOI: 10.15468/m2cabu
title: Stratigraphic distribution of marine palynomorph species recorded for the Miocene of ODP Hole 105-645E (Table 1)

description: A total of 145 samples were analyzed for palynology, and all were found to be productive. Residues are dominated by pollen, terrestrial spores, and land plant tissues. Marine palynomorphs occur in all samples, which allowed us to recognize five Miocene dinocyst assemblage zones. Dinocyst assemblages indicate cool-water conditions and suggest a neritic rather than fully oceanic environment, with not only North Atlantic and Norwegian Sea affinities, but also containing both notable protoperidiniacean and possible endemic elements. Dinocyst assemblages indicate an early Miocene age for the bottom of Hole 645E and an age no younger than early late Miocene (Sample 105-645E-24R, CC) near the top of the interval studied. These age assignments provide an estimated initiation of ice rafting in Baffin Bay at between 7.4 and 9.5 Ma. Increased terrigenous influx and apparent disappearance of certain dinocyst taxa occur in the middle to late Miocene and may be related to oceanographic changes or climatic deterioration. Spores and pollen indicate a climate that varied within a temperate regime during the early and middle to early late Miocene, followed by climatic deterioration. Four new dinocyst species are described: Batiacasphaera gemmata, Impletosphaeridium prolatum, Operculodinium vacuolatum, and Selenopemphix brevispinosa. The acritarch genus Cyclopsiella Drugg and Loeblich is emended, and two new combinations have been created: Cyclopsiella granosa (Matsuoka) and Cyclopsiella? laevigata (Chateauneuf). Cyclopsiella granosa (Matsuoka) n. comb. is considered a subjective junior synonym of Cyclopsiella granulata He and Li. Ascostomocystis granulatus Chateauneuf has been provisionally allocated to Cyclopsiella and renamed Cyclopsiella? chateauneufii. Two new acritarch species are described: Cyclopsiella spiculosa and Cymatiosphaera! baffinensis.
DOI: 10.15468/ahn6y6
title: Sarcodine counts and carbon biomass at station TT012_5-PMOC5
DOI: 10.15468/8neg3g
title: Dinoflagellate cysts from sediment core PS1295-4
DOI: 10.15468/2tb37n
title: (Appendix A) Stable isotope ratios of Cibicidoides sp. and planktonic foraminifera from the Mid-Miocene of ODP Hole 119-744B of the Kerguelen Plateau, Antarctica
DOI: 10.15468/84x2ur
title: Phytoplankton abundance and species composition in the Gulf of Naples and the Gulf Salerno in November 1985
DOI: 10.15468/nxt4d5
title: Range table from benthic foraminifers in ODP Hole 178-1103A
DOI: 10.15468/sba7fc
title: Relative abundance of live (Rose Bengal stained) benthic foraminifera in East Atlantic surface sediments off Senegal and Gambia (Table 1)
DOI: 10.15468/y8vmmh
title: Nannofossil abundance of Hole 16-157A
DOI: 10.15468/5be76b
title: Counting of benthic foraminifera of ODP Hole 182-1132B
DOI: 10.15468/fk2rsf
title: Radiolaria assemblage in sediment core GIK23414-6
DOI: 10.15468/kremf4
title: (Table 3) Distribution and relative abundance of planktonic foraminifers in ODP Hole 114-704A