cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/z24kjf
title: (Table S2) Age determination of ODP Sites 202-1234 and 202-1235

description: Antarctic Intermediate Water is, at present, a water mass that brings oxygen to intermediate depths throughout the Southern Hemisphere oceans. Models have suggested that intermediate waters had higher concentrations of oxygen during the last glacial period (Meissner et al., 2005, doi:10.1029/2004PA001083; Liu et al., 2002, doi:10.1029/2001GL013938), consistent with globally reduced denitrification (Galbraith et al., doi:10.1029/2003PA001000) and increased production of Antarctic Intermediate Water (Lynch-Stieglitz and Fairbanks, 1994, doi:10.1029/93PA02446). However, some palaeoceanographic reconstructions (Bostock et al., 2004, doi:10.1029/2004PA001047; Pahnke and Zahn, 2005, doi:10.1126/science.1102163) have indicated that production decreased in the southeast Pacific Ocean at this time. Here we analyse the concentrations of Re and Mn, the sedimentary concentrations of which are controlled by the amount of dissolved oxygen at the sea floor, from three sediment cores located along the Chilean margin for the past 30,000 years. Our results from the cores, which bracket the present-day water-column extent of Antarctic Intermediate Water, show that the depth range of well-oxygenated Antarctic Intermediate Water increased off Chile during the Last Glacial Maximum. Dissolved oxygen content began to decrease approximately 17,000 years ago, coincident with rapid Antarctic warming and a poleward shift of the southern westerly winds (Anderson et al., 2009, doi:10.1126/science.1167441). Our estimates of productivity from accumulation rates of organic carbon and opal do not co-vary with the seafloor oxygen variations, ruling out local control of seafloor oxygenation. We conclude that the data are best explained by a combination of increased oxygenation and increased flux of Antarctic Intermediate Water during the Last Glacial Maximum.
DOI: 10.15468/wce6rt
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/090-4
DOI: 10.15468/5jedy9
title: Range table from planktonic foraminifers in ODP Hole 180-1108B
DOI: 10.15468/569knq
title: Range table from planktonic foraminifers in ODP Hole 172-1058A
DOI: 10.15468/5fff97
title: Foraminifera abundance of Hole 48-405
DOI: 10.15468/55262w
title: (Table T2) Abundance of dinoflagellates and other palynomorphs in ODP Hole 189-1171D sediments
DOI: 10.15468/yktxm6
title: Nannofossil abundance of Hole 7-63
DOI: 10.15468/2fhaw5
title: Benthic foraminifera distribution of sediment core ASV1200
DOI: 10.15468/9bhrzs
title: Total foraminifera counts of multinet M42/3_MSN1359
DOI: 10.15468/rrjwbu
title: Radiolaria assemblage in sediment core GIK23071
DOI: 10.15468/byp5m3
title: Microzooplankton abundance measured on water bottle samples at station PS58/049-3
DOI: 10.15468/8dbbkg
title: Plasm bearing foraminifera counts from M35/1_MSN1065
DOI: 10.15468/pdf9mq
title: Bulk components and planktonic foraminifera of sediment core GIK17748-2
DOI: 10.15468/33jnwz
title: Range table from nannofossils in ODP Hole 198-1207B
DOI: 10.15468/uu9et2
title: (Table 6) Planktonic foraminifer abundance of ODP Hole 162-982B
DOI: 10.15468/b4spz8
title: Planktic foraminifera counts at CTD station PS55/080-1
DOI: 10.15468/zfbbeg
title: (Table 15A) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 90-593
DOI: 10.15468/x5hn9m
title: Foraminifera species abundances from tow TT007_4-MOC7
DOI: 10.15468/k95x8m
title: Range table from benthic foraminifers in ODP Hole 151-910C
DOI: 10.15468/2jtqzx
title: Benthic foraminifera abundance of Hole 1-4
DOI: 10.15468/75ueg3
title: (Table 8) Relative abundance of benthic foraminifera in ODP Hole 112-682A, Part IV
DOI: 10.15468/ejuys7
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB04 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/wkpgxq
title: Total foraminifera counts of multinet M21/4_MSN712
DOI: 10.15468/kdpx2j
title: Planktic foraminifera abundance of Hole 11-98
DOI: 10.15468/y5p4rw
title: Occurrence of mammalia relicts at site Sernesul Rece Cave
DOI: 10.15468/ay5gqu
title: Range table from benthic foraminifers in ODP Hole 181-1122A
DOI: 10.15468/9a2c9q
title: Range table from benthic foraminifera in ODP Hole 199-1218A
DOI: 10.15468/7hdgn4
title: Dinoflagellate abundance of Hole 71-512
DOI: 10.15468/xe776a
title: Echinoderms in surface sediments off Sylt collected during HEINCKE cruise HE278
DOI: 10.15468/9t2mbt
title: (Table 1) Shallow-water foraminifera in ODP Hole 133-821A
DOI: 10.15468/qdev8k
title: Occurrence of mammalia relicts at site Crayford
DOI: 10.15468/qqhkke
title: Ostracoda abundance of Hole 44-392A
DOI: 10.15468/mp7hgw
title: Total living benthic foraminifera at station M33/1_MC-15 (WAST), size fraction &gt;30 µm
DOI: 10.15468/3whaxh
title: Oberservation of birds at station PS14/158 along 49° West
DOI: 10.15468/p37wpv
title: Plasm bearing foraminifera counts of multinet M36/6_MSN1196
DOI: 10.15468/txeqrw
title: Microzooplankton abundance measured on water bottle samples at station PS65/427-1
DOI: 10.15468/q3maed
title: Nannofossil abundance of Hole 94-607A
DOI: 10.15468/rk9ur4
title: Planktic foraminifera abundance of Hole 60-456
DOI: 10.15468/bharav
title: Sedimentological investigation on core V15-168
DOI: 10.15468/uthgms
title: Content of coarse fraction and G. menardii in sediment corev V25-47
DOI: 10.15468/w3ffxz
title: Dinoflagellates, pollen and spore abundance of Hole 29-280A
DOI: 10.15468/29ggu9
title: Nannofossil abundance of Hole 4-26
DOI: 10.15468/xw6cbj
title: Total foraminifera counts of multinet M12/3_MSN536
DOI: 10.15468/2zgwvc
title: Planktic foraminifera of sediment core GeoB1404-3
DOI: 10.15468/gdtj75
title: (Table 3) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-680A
DOI: 10.15468/4zkp3m
title: Range table from planktonic foraminifers in ODP Hole 152-914A
DOI: 10.15468/9nn9ns
title: (Table 18) Ranges of benthic foraminifers through the Neogene in DSDP Hole 23-219
DOI: 10.15468/2m22e2
title: Plasm bearing foraminifera counts of multinet M21/2_MSN628
DOI: 10.15468/q8fbyc
title: Total foraminifera counts of multinet M36/6_MSN1198
DOI: 10.15468/szmvyy
title: Nannofossil abundance of Hole 24-232A
DOI: 10.15468/8pxyg9
title: (Table 4b) Calcareous nannofossil distribution on ODP Hole 117-721B
DOI: 10.15468/ffpasu
title: Tab. 1 + 2: Distribution chart of nannoplankton species record

description: Between March and April of 1986 a series of water samples were taken in the South Atlantic to study the Recent calcareous nannoplankton assemblages in that part of the world. South of Africa, in the transitional floral zone, most of the coecolithophorid flora elements characteristic of this zone were recognized but in addition influences from the floras of the Indian Ocean were distinguished as well as floral elements belonging to the tropical and subtropical floral zones. It is concluded that the transitional floral zone should be redefined on the basis of seasonal changes of the assemblages. In the cold waters between the Subtropic and the Antarctic Convergences near the Antarctic continent, calcareous nannoplankton is scarce. Only a monospecific assemblage of malformed Emiliania huxleyi was found. Probably the combination of cold water and high hydro energy levels prevents the development of adiverse coccolith-bearing nannoplankton assemblage. South of the Antarctic Convergence no calcareous nannoplankton was found.
DOI: 10.15468/29n5tn
title: Foraminifera abundance of Hole 58-444
DOI: 10.15468/2g525y
title: (Fig. 11) Distribution of dinoflagellate cysts in Early Cretaceous sediments of DSDP Hole 41-370 in the North Atlantic
DOI: 10.15468/g6y6um
title: Occurrence of mammalia relicts at site Kniegrotte
DOI: 10.6084/m9.figshare.21823455.v68
title: The ReptileEvolution.com Project

description: Taxon exclusion is the number one problem currently vexing paleontology. The search for pterosaur, turtle, bat, snake, whale, reptile and tetrapod ancestors continues to unnecessarily befuddle paleontologists who continue to work from cherry-picked, textbook and traditional taxon lists that overlook and omit pertinent taxa. That’s why the large reptile tree (LRT), the nearly completely resolved cladogram at the heart of www.ReptileEvolution.com, includes 2212 taxa. Larger taxon numbers minimize taxon exclusion issues. Results indicate the simple act of adding taxa resolves all phylogenetic issues.
DOI: 10.15468/z8gamn
title: Planktic foraminifera abundance of Hole 1-7
DOI: 10.15468/4mf65m
title: (Table 1) Abundance and biomass of diatom algae, dinofiagellates, green algae, and flagellates and their percentages in total phytoplankton abundance and biomass in the Obskaya Guba and adjacent Kara Sea in the latest September 2007
DOI: 10.15468/u8tp78
title: Total foraminifera counts of multinet SO118_MSN1265
DOI: 10.15468/3r3umm
title: Total foraminifera counts from multinet M31/2_MSN892
DOI: 10.15468/acnyne
title: (Table T4) Calcareous nannofossil abundance of ODP Site 189-1171 sediments
DOI: 10.15468/gs54yj
title: (Table 1) Calcareous nannofossil distribution at ODP Site 180-1109 from the Solomon Sea, western Pacific

description: The paleoceanography of the Solomon Sea for the last 195,000 years was investigated, based on the observations of 21 taxonomic groups of calcareous nannofossils in 144 samples taken from tocean drilling program (ODP) cores 1109A-1H and 1109C-2H. Oxygen isotope ratios in tests of the planktonic foraminifer Globigerinoides ruber allow us to assign the cores to oxygen isotope stages 7-1. Past sea-surface temperatures (SST) were estimated qualitatively using the composition of three Gephyrocapsa coccolith morphotypes; the high-, intermediate- and low-angel types that are classified based on the bridge angle of coccolith, can be used as proxies for warm, intermediate and cold temperature, respectively. Abundance of the high-angel type coccoliths increased and decreased during the interglacial and glacial periods, respectively. This tendency is consistent with the expected change of the Western Pacific Warm Pool (WPWP) development. However, a large shift in the abundance of the high-angle type coccolith recorded during early stage 3 did not correspond to the oxygen isotope record. The ratio of small (&lt;2.5 µm) placoliths of Reticulofenetsra and Gephyrocapsa to the low-photic species was higher during stage 2 than late stage 3 and 1. As the reduced blanketed effect to the WPWP would cause an increase in the number of small placoliths, a reduction of the WPWP in stage 2 is indicated by the increase of small placoliths and by the lower SST deduced from the composition of the Gephyrocapsa morphotypes. The decreasing trend of small placoliths after ~40 ka is similar to the results reported in several previous studies in the surrounding regions of Australia.
DOI: 10.15468/c2mudv
title: (Fig. 4) Distribution and stable isotope record of foraminifera, and ice-rafted debris sediment core PS1243-1
DOI: 10.15468/2nhyux
title: Phytoplankton abundance at station Rigel_6_2005-08 in August 2005, Chipana, Chile
DOI: 10.15468/h6yhys
title: (Table T8) Calcareous nannofossil stratigraphy of ODP Hole 198-1211A
DOI: 10.15468/dzrcrw
title: Benthic foraminifera abundance of Hole 34-320B
DOI: 10.15468/6bn7mx
title: Range table from planktonic foraminifers in ODP Hole 155-931B
DOI: 10.15468/mxm5sp
title: Occurrence of mammalia relicts at site Falkensteinhöhle
DOI: 10.15468/q9jdtn
title: (Table 8) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-685A
DOI: 10.15468/gfdjd8
title: (Table 3) Stratigraphic distribution of silicoflaggelates, ebridians and actiniscidians in upper Pliocene to Pleistocene sediments of ODP Hole 104-644A
DOI: 10.15468/j9r8cg
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB04 in the euphotic zone of the Aegean Sea in spring 1997. Part 2 - dinoflagellates
DOI: 10.15468/72nsqq
title: Phytoplankton abundance at station Sechin_2003-11-06_1, Casma, Peru
DOI: 10.15468/t5x5ku
title: Microplankton abundance at Station SEPT-1997-GN36199704606MNB04 in the euphotic zone of the Aegean Sea in September 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/ke837b
title: Nannofossil abundance of Hole 14-144A
DOI: 10.15468/6s2khc
title: Planktic foraminifera counts of sediment core V18-191
DOI: 10.15468/hsrc4f
title: Range table from planktonic foraminifers in ODP Hole 155-941B
DOI: 10.15468/f869vu
title: Total foraminifera counts of multinet M6/7_MSN119
DOI: 10.15468/tmagm6
title: Coccolith counts of multinet M32/5_MSN990
DOI: 10.15468/v2u24p
title: Nannofossil abundance of Hole 34-321
DOI: 10.15468/6ft55p
title: (Table 2) Planktonic foraminifera species found in sediment trap samples and bottom sediments at Station Vy20-3178
DOI: 10.15468/wav8ve
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-15-5
DOI: 10.15468/au6qkj
title: Abundance of planktic foraminifera at CTD station PS55/037
DOI: 10.15468/qy78d9
title: Ostracoda abundance of Hole 42-375
DOI: 10.15468/3857qx
title: (Figure 1h) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3171-4-6
DOI: 10.15468/caepjh
title: Sarcodine counts and carbon biomass at station TT007_2-TM2
DOI: 10.15468/ku55m2
title: Range table from ostracoda in ODP Hole 151-910C
DOI: 10.15468/29s8ea
title: Total foraminifera counts of multinet POS247/2_MSN1375
DOI: 10.15468/7mj7a8
title: Abundance of benthos infauna at station GIK23025-2
DOI: 10.15468/9udenk
title: Benthic foraminifera and nannofossil abundance of Hole 40-364
DOI: 10.15468/9jk5u7
title: Plasm bearing foraminifera counts of multinet M21/1_MSN619
DOI: 10.15468/xacqkt
title: Abundance of radiolaria at station UT99-22-1
DOI: 10.15468/tjec4b
title: Occurrence of mammalia relicts at site Tornewton Cave
DOI: 10.15468/ura7fa
title: (Fig. 3) Age and multiproxy studies of sediment core GeoB7186-3
DOI: 10.15468/p6n2g4
title: Range table from planktonic foraminifers in ODP Hole 182-1128B
DOI: 10.15468/76evah
title: Concentration of siliceous microplankton in surface sediments, brine
DOI: 10.15468/kj8car
title: (Table 17) Benthic foraminifera in early Miocene sediments of DSDP Hole 90-593
DOI: 10.15468/2sve9y
title: Occurrence of mammalia relicts at site Nikolaushöhle
DOI: 10.15468/hnzknc
title: Total foraminifera counts of multinet M36/2_MSN1107
DOI: 10.15468/4anez3
title: Macrofauna abundance in surface sediment sampled during cruise DI229
DOI: 10.15468/smjqs7
title: Abundance and composition of meiobenthos in surface sediments at Fladen Ground stations in August 1975, North Sea (Table 4)
DOI: 10.15468/daue33
title: Range table from planktonic foraminifers in ODP Hole 159-959B
DOI: 10.15468/rnrm2k
title: (Table 4) Distribution of planktonic and selected benthic foraminifers from DSDP Hole 87-583A
DOI: 10.15468/vvht62
title: (Figure 1) Dinoflagellate cyst stratigraphy of DSDP Hole 80-548A

description: Cyst assemblages from Sites 548, 549, and 550 were examined and gave evidence of early Eocene to late Miocene age. These assemblages were compared with other North Atlantic DSDP sites and with onshore sections in Denmark, southern England, Spain, and Italy. Some environmental interpretation is attempted for the Miocene assemblages; pollen, spores, and dinoflagellate cyst species were used to interpret the proximity of the shoreline. Key species are illustrated, along with some forms that are not discussed.
DOI: 10.15468/3gbrhd
title: Plasm bearing foraminifera counts of multinet M21/5_MSN735
DOI: 10.15468/9eum9t
title: (Table 8) Pliocene to Pleistocene nannofossil range chart for ODP Hole 134-833B
DOI: 10.15468/x968cp
title: (Table 3) Distribution of planktonic foraminifers in ODP Hole 108-657A
DOI: 10.15468/3en9jg
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/011-3
DOI: 10.15468/28pffb
title: (Table 6) Distribution of diatoms in Miocene to Pleistocene sediments of DSDP Hole 7-66
DOI: 10.15468/6d6qha
title: Benthic foraminifera abundance of Hole 48-401
DOI: 10.15468/vt9u4v
title: (Table 7) Distribution of early to middle Eocene calcareous nannofossils in ODP Hole 149-900A
DOI: 10.15468/7nncpp
title: Fig. 11: Benthic foraminifera assemblage of sediment core MD97-2131
DOI: 10.15468/bm6nhy
title: Nannofossil abundance of Hole 26-253
DOI: 10.15468/7vxzz6
title: Microzooplankton abundance and biomass at station NBP97-03-14-3
DOI: 10.15468/v4apjn
title: (Table 3) Distribution of middle Eocene calcareous nannofossils in ODP Hole 149-897C
DOI: 10.15468/dj9c89
title: Distribution of planktic foraminifers of core Y71-06-12
DOI: 10.15468/dsshgc
title: Range table from benthic foraminifers in ODP Hole 198-1213B
DOI: 10.15468/xbfask
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB01 in the euphotic zone of the Aegean Sea in spring 1997. Part 1 - diatoms
DOI: 10.15468/9xc3s8
title: Assemblage of living benthic foraminifera in sediment core SO117_MC469, 63-125 µm fraction
DOI: 10.15468/f5d53m
title: Abundance and carbon biomass of phytoplankton at station TT007_2-CTD26
DOI: 10.15468/mfvcym
title: Benthic foraminiferal number, diversity, and species abundance of size fraction 63-125µm across sapropel S6 in core M44/3_KL83 from the middle bathyal of the eastern Levantine Basin
DOI: 10.15468/yp8n6z
title: Plasm bearing foraminifera counts of multinet POS231/3_MSN1331
DOI: 10.15468/cq64cw
title: Range table from planktonic foraminifers in ODP Hole 177-1089A
DOI: 10.15468/agzny6
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC12-339
DOI: 10.15468/7k88p3
title: Distribution of planktic foraminifera (250-500 µm) of box sediment core GIK23059-2
DOI: 10.15468/gxatvt
title: Palynomorph concentrations in ODP Hole 105-645B samples (Table 1)

description: Significant changes in terrestrial and marine environments of Baffin Bay occurred throughout the late Pliocene to Holocene. Upper Pliocene and lowermost Pleistocene sediments contain abundant pollen and spores, which indicates the existence of open, coniferous, boreal forest to forest tundra in areas surrounding Baffin Bay. The late Pliocene-earliest Pleistocene also is characterized by relatively rich, dinoflagellate cyst and acritarch assemblages of boreal character, in which the dominance of Cymatiosphaera and Peridiniaceae may indicate neritic influx of sediments. In contrast, the late-early Pleistocene to Holocene interval is marked by a sparse terrestrial and marine palynoflora, with rare productive intervals. The general paucity of the Pleistocene palynoflora suggests low primary productivity, both on land and offshore, probably caused by cold, dry, high arctic conditions.
DOI: 10.15468/uvmh25
title: (Appendix) Late Cretaceous calcareous nannofossils of DSDP Holes 80-549 and 80-551

description: he early late Cretaceous (Cenomanian–early Turonian) is thought to have been one of the warmest periods of the Phanerozoic. This period was characterised by tropical sea surface temperatures of up to 36 °C and a pole-to-equator-gradient of less than 10 °C. The subsequent Turonian–Maastrichtian was characterised by a continuous climatic cooling, peaking in the Maastrichtian. This climatic cooling and the resulting palaeoceanographic changes had an impact on planktic primary producer communities including calcareous nannofossils. In order to gain a better understanding of these Cenomanian–Maastrichtian palaeoceanographic changes, calcareous nannofossils have been studied from the proto North Atlantic (Goban Spur, DSDP Sites 549, 551). In order to see potential differences between open oceanic and shelf dwelling nannofossils, the data from Goban Spur have been compared to findings from the European shelf (northern Germany). A total of 77 samples from Goban Spur were studied for calcareous nannofossils revealing abundant (mean 6.2 billion specimens/g sediment) and highly diverse (mean 63 species/sample) nannofossil assemblages. The dominant taxa are Watznaueria spp. (mean 30.7%), Prediscosphaera spp. (mean 18.3%), Zeugrhabdotus spp. (mean 8.3%), Retecapsa spp. (mean 7.2%) and Biscutum spp. (mean 6.6%). The Cenomanian assemblages of both Goban Spur (open ocean) and Wunstorf (shelf) are characterised by elevated abundances of high fertility taxa like Biscutum spp., Zeugrhabdotus spp. and Tranolithus orionatus. Early Turonian to Maastrichtian calcareous nannofossil assemblages of Goban Spur are, however, quite different to those described from European sections. Oceanic taxa like Watznaueria spp., Retecapsa spp. and Cribrosphearella ehrenbergii dominate in Goban Spur whereas the fertility indicators Biscutum spp. and T. orionatus are more abundant in the European shelf assemblages. This shift from a homogeneous distribution of calcareous nannofossils in the Cenomanian towards a heterogeneous one in the Turonian–Maastrichtian implies a change of the ocean circulation. The “eddy ocean” system of the Cenomanian was replaced by an oceanic circulation similar to the modern one in the Turonian–Maastrichtian, caused by the cooling. The increased pole-to-equator-gradients resulted in an oceanic circulation similar to the modern one.
DOI: 10.15468/mrfhcg
title: Number of dead benthic foraminifera in Nordensheld Bay, Novaja Zemlja
DOI: 10.15468/zwqq62
title: Dinoflagellate cysts in surface sediment samples of METEOR cruises M20/2, M23/1, M34/1, M34/2, M34/3 and M34/4

description: To enhance the limited information available about the palaeo-ecological significance of calcareous dinoflagellates, we have studied their lateral distribution in surface sediments of the equatorial and south Atlantic between 13°N and 36°S. Calcareous dinoflagellate cysts appear to be widely distributed throughout the studied area. In the surface sediments, concentrations (cyst per gram dry sediment) of the vegetative stage Thoracosphaera heimii are generally higher than that of the (presumably) calcareous resting cysts. Distribution patterns in surface sediments of Orthopithonella granifera (Fütterer) Keupp and Versteegh, Rhabdothorax spp. Kamptner., Sphaerodinella albatrosiana (Kamptner) Keupp and Versteegh S. albatrosiana praratabulated, Sphaerodinella tuberosa var. 1 (Kamptner) Keupp and Versteegh and S. tuberosa var. 2 and the ratios between these species have been compared with temperature, salinity, density and stratification gradients in the upper water column. Rhabdothorax spp. is characteristically present in sediments of more temperate regions characterized by high seasonality. Dinoflagellates producing these cysts are able to tolerate high nutrient concentrations, and mixing of the water column. S. albatrosiana is abundant in regions characterized by high sea surface temperatures and oligotrophic surface water conditions. In contrast, the distribution of S. tuberosa var. 2 is negatively related to temperature. The other cyst species did not show a characteristic pattern in relation to the studied environmental gradients. The ratio of Sphaerodinella tuberosa var. 2 to Orthopithonella granifera can be used for reconstructing the presence of stratification in the upper 50 m of the water column, whereas the ratios of S. tuberosa var. 2 to Sphaerodinella albatrosiana and of O. granifera to Rhabdothorax spp. might be used for palaeotemperature reconstructions. Calcareous dinoflagellate cysts are abundant in oligotrophic areas and may be useful for the reconstruction of palaeoenvironmental conditions.
DOI: 10.15468/u44s7x
title: Phytoplankton abundance during OCEANIA cruise Oceania90
DOI: 10.15468/483uax
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1374
DOI: 10.15468/tfse7q
title: Assemblage of living benthic foraminifera in sediment core GeoB3703-4
DOI: 10.15468/7a3mmd
title: Planktic foraminifera counts of sediment core V19-185
DOI: 10.15468/rnwtqs
title: Benthic macrofauna abundance and biomass in surface sediment during cruise PLG95A
DOI: 10.15468/5unpzw
title: Range table from planktonic foraminifers in ODP Hole 170-1042B
DOI: 10.15468/eg5gs6
title: Phytoplankton abundance at station Rigel_5_2005-07 in July 2005, Chipana, Chile