cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/btbu7g
title: Benthic macrofauna abundance of sediment core 12930-093
DOI: 10.15468/724f4y
title: Total foraminifera counts from M35/1_MSN1044
DOI: 10.15468/sdvvtr
title: Abundance of microplankton from bottle APRIL-2000-K5
DOI: 10.15468/zyvk2a
title: Distribution of meiobenthos in surface sediments of the northeastern Atlantic (Table 1)
DOI: 10.15468/5gja2v
title: Occurrence of nannoplankton observed in Early Pliocene samples from Zanclean stratotype of Capo Rossello, Sicily (Table I)

description: Calcareous nannoplankton biostratigraphy has been worked out in the eastern Mediterranean utilizing deep-sea sediments recovered from DSDP Leg 42A Sites 375 and 376. These two drill sites were located approximately 55 km west of Cyprus on the Florence Rise. Sediments, ranging in age from early Miocene (Helicosphaera ampliaperta Zone) through Holocene, contain sufficient age-diagnostic species to recognize essentially all of the lowlatitude nannoplankton zones described by Bukry, although regional, secondary marker species are needed to define some zonal boundaries. Reworked Cretaceous and Paleogene nannoplankton occur throughout the stratigraphic interval studied, but not in quantities large enough to mask indigenous species. Sedimentation rates at Sites 375 and 376 were highest in the late Miocene and late Pleistocene. Open-marine, warm-water species of discoasters are present in significant numbers throughout the Miocene and Pliocene. Earliest Pliocene assemblages contain numerous specimens of ceratoliths. Nannoplankton in post-Messinian sediments at the drill sites and the Zanclean stratotype at Capo Rossello, Sicily, indicate that the base of the Amaurolithus tricorniculatus Zone (base of Triquetrorhabdulus rugosus Subzone) corresponds with the Miocene-Pliocene boundary.
DOI: 10.15468/axnvyd
title: Phytoplankton abundance measured on water bottle samples at station PS65/470-1
DOI: 10.15468/n22zvj
title: Distribution of benthic foraminifera of sediment core PS1388-3
DOI: 10.15468/kfg6vm
title: (Figure 1) Stratigraphic distribution of taxa at DSDP Hole 79-547B

description: Twenty-five samples from selected cored intervals of problematic Triassic-Jurassic age from Sites 545, 546, and Hole 547B have been analyzed palynologically to aid age determination. Section 545-73-1 yielded a marine palynoflora of Sinemurian-Bajocian age. A palynoflora of nonmarine origin and assigned a Rhaetian-Hettangian age was recovered from halite in Section 546-18-2. Marine palynofloras of Hettangian-early Pliensbachian age were recovered from Sample 547B-24-CC to Section 547B-14-2. Sections 547B-28-1 to 547B-25-3 yielded impoverished nonmarine palynofloras to which only a general Rhaetian-Hettangian age could be given.
DOI: 10.15468/ymqyhb
title: (Table 2) Distribution of nannofossils in DSDP Hole 87-583
DOI: 10.15468/6qu9ra
title: Occurrence of mammalia relicts at site Bettenroder Berg IX
DOI: 10.15468/ysnnbk
title: Distribution of meiobenthos in sediment core M23_203 of the northeastern Atlantic (Table 1)
DOI: 10.15468/99zn3r
title: Pollen profile from sediment core AV14_K2-4
DOI: 10.15468/xc3vvk
title: Occurrence of mammalia relicts at site Crumstadt 1
DOI: 10.15468/akqr4n
title: Faunal assemblage of sediment core GS7603-9
DOI: 10.15468/6k59uf
title: Fig. 4. Simplified macrofossil concentration in sediment core Lz1116
DOI: 10.15468/chwbey
title: Nannofossil abundance of Hole 94-611A
DOI: 10.15468/rh69gw
title: Total foraminifera counts of multinet M21/1_MSN610
DOI: 10.15468/bmsbfs
title: Microplankton abundance in the euphotic zone of the Aegean and Levantine Seas in August-September 1989
DOI: 10.15468/tkns57
title: Echinoderms in surface sediments off Sylt collected during HEINCKE cruise HE233
DOI: 10.15468/xk7tma
title: Microzooplankton abundance and biomass at station NBP97-08-04-5
DOI: 10.15468/m6e7vy
title: Distribution of planktic foraminifera of sediment core GIK23342-6 at stadium 5.5
DOI: 10.15468/nq8tz9
title: (Table 2) Distribution of calcareous nannofossils in the Paleocene of ODP Hole 113-689B
DOI: 10.15468/wm9ebf
title: (Appendix B1) Relative abundances of middle Eocene-late Oligocene calcareous nannofossils in ODP Hole 120-748B
DOI: 10.15468/td63rq
title: Occurrence of mammalia relicts at site Pestera lui Climente I
DOI: 10.15468/amkarj
title: Nannofossil abundance of Hole 47-398
DOI: 10.15468/dy5yxx
title: (Table 4) Planktonic foraminifers from ODP Hole 114-704B
DOI: 10.15468/gpcja6
title: Total foraminifera counts from multinet SO119_MSN1303
DOI: 10.15468/ufhvbe
title: Ostracoda in sediment core PS51/154-11
DOI: 10.15468/27gjbu
title: Planktic foraminifera counts at CTD station M39/4_361CTD-18
DOI: 10.15468/qe8tva
title: Nannofossil abundance of Hole 24-231
DOI: 10.15468/2jpa8h
title: (Table T5) Planktonic foraminifera stratigraphy of ODP Hole 198-1209A, Zones P9-P11
DOI: 10.15468/n3p8c6
title: Palynological analysis of sediment core GeoB3910-2
DOI: 10.15468/xu5qd4
title: Total foraminifera counts of multinet M12/3_MSN557
DOI: 10.15468/7qkx96
title: (Table 3h) Foraminiferal distribution chart of petroleum well Swan-3St
DOI: 10.15468/h3rnmb
title: Plasm bearing foraminifera counts from multinet SO119_MSN1285
DOI: 10.15468/hkzr46
title: Absolute abundance of particles and planktic foraminifera in sediment core GIK12310-4, Cape Barbas, North-West Africa (Appendix Tab. 2c)
DOI: 10.15468/nwgpc7
title: (Table 1) Distribution of calcareous nannofossils in ODP Hole 130-807C
DOI: 10.15468/xgy2d6
title: Occurrence of mammalia relicts at site Aveley
DOI: 10.15468/2q4jgt
title: Occurence of microfossils in Early Cretaceous sediments of DSDP Hole 25-249 (Tab. 1)

description: From 12 radiolarian-rich claystone samples of the DSDP-Leg 25, Site 249, situated in the western Indian Ocean southwest of Madagascar 4 species of agglutinated and 38 species of calcareous benthonic foraminifera are described, 13 of them in open nomenclature. As a lot of Valanginian species and Gavelinella barremiana occur in the foraminiferal faunas described here a Valanginian-Hauterivian age is assigned to them. These microfaunas investigated here yield some index species characteristic in the Lower Cretaceous deposits of Northern Germany and also from the near-by Madagascar. Nodosariids dominate in a striking way with 36 species, especially of Astacolus, Citharina, Lenticulina, Lingulina, Marginulinopsis, Nodosaria, Saracenaria, and Vaginulina. Important Neocomian species well-known from other DSDP sites, namely Praedorothia ouachensis (SIGAL) and planktonic foraminifers, are missing. The microfaunas of Site 249 have to be derived from shelf areas.
DOI: 10.15468/fzg6gq
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1375
DOI: 10.15468/uedhaf
title: Abundance of benthos infauna at station GIK23060-1
DOI: 10.15468/b7282m
title: Range table from planktonic foraminifers in ODP Hole 141-862C
DOI: 10.15468/8tsxsy
title: Range table from benthic foraminifers in ODP Hole 154-926A
DOI: 10.15468/2dcp6k
title: Occurrence of mammalia relicts at site Predmosti
DOI: 10.15468/dpj4em
title: Dinoflagellate cysts of ODP Hole 189-1171D
DOI: 10.15468/xcazr5
title: Range table from planktonic foraminifers in ODP Hole 167-1019C
DOI: 10.15468/nu6zgc
title: (Table 1) Major and minor element concentrations in the livers of polar bears (Ursus maritimus) from Canada, Alaska and Greenland
DOI: 10.15468/pc2ktw
title: Planktic foraminifera counts at CTD station PS55/025
DOI: 10.15468/4emf6s
title: Microzooplankton abundance and biomass at station NBP97-08-33-5
DOI: 10.15468/rsa2pm
title: Nannofossil abundance of Hole 1-7
DOI: 10.15468/ny2nxs
title: Apectodinium spp. and percentage of endemic and bipolar dinoflagellate cysts of ODP Hole 182-1128D
DOI: 10.15468/3pkytq
title: Planktic foraminifera abundance of Hole 26-251A
DOI: 10.15468/ddqky7
title: Phytoplankton abundance in surface water in February 1998, Pisco, Peru
DOI: 10.15468/u8tn65
title: Distribution of planktic foraminifera (200-630 µm) of sediment core M8_057-2 (Table 4)
DOI: 10.15468/haayk2
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V27-20
DOI: 10.15468/zzvy4e
title: Total foraminifera counts of multinet M6/7_MSN125
DOI: 10.15468/9matax
title: (Appendix A1) Relative abundances of benthic foraminifera and stable carbon isotope ratios of Nuttallides truempyi at the Paleocene-Eocene thermal maximum in ODP Hole 198-1209B in the central Pacific
DOI: 10.15468/tnpqak
title: Microplankton abundance in the euphotic zone of the Aegean, Levantine and Ionian Seas in March-April 1992
DOI: 10.15468/34qpdp
title: Planktic foraminifera abundance of Hole 18-182
DOI: 10.15468/hspqpa
title: Content of coarse fraction and G. menardii in sediment corev V25-48
DOI: 10.15468/ysk7hy
title: (Figure 4) Distribution and relative abundances of the benthic foraminifers recovered from the Jurassic section of DSDP Hole 79-547B
DOI: 10.15468/3r8vpw
title: Occurrence of mammalia relicts at site Gladbeck
DOI: 10.15468/dnhr4y
title: Planktic foraminifera abundance of Hole 94-607
DOI: 10.15468/nsyhtq
title: (Appendix B) Foraminifera and stable carbon and oxygen isotope record of ODP Hole 105-647B
DOI: 10.15468/7v2ut6
title: Meiofauna abundance in sediment core 13200-024
DOI: 10.15468/xb9nj9
title: Diversity of total live benthic foraminiferal assemblages in South Atlantic surface sediments
DOI: 10.15468/yw668j
title: Planktic foraminifera abundance of Hole 29-278A
DOI: 10.15468/dpwbzc
title: Planktic foraminifera abundance of Hole 11-108
DOI: 10.15468/2wqcmg
title: Benthic macrofauna abundance of sediment core 13077-059
DOI: 10.15468/pp72cd
title: (Table 4) Planktic foraminifera counts in sediment core JM05-085-GC obtained during a R/V Jan Mayen cruise in 2005
DOI: 10.15468/gv4cnb
title: Sarcodine counts and carbon biomass at station TT012_5-TM69
DOI: 10.15468/hqt9eq
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1386
DOI: 10.15468/w2sev8
title: (App 7) Relative contents of benthic foraminifera species in sediments accumulated during last 1000 years, Core ASV11-987
DOI: 10.15468/7qe4yy
title: Total foraminifera counts from M35/1_MSN1059
DOI: 10.15468/6fdg8m
title: (Appendix A) Radiolarian abundances in sediment core MD96-2086
DOI: 10.15468/4qu7na
title: Palynology of a profile from Ahlequellmoor in Germany
DOI: 10.15468/bqs6af
title: Total foraminifera counts of multinet M10/2_MSN231
DOI: 10.15468/z4jvgh
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station JUNE-1998-MNB5
DOI: 10.15468/tvmacf
title: (Appendix A) Relative abundance of Emiliania huxleyi in sediment cores of the North Atlantic

description: The coccolithophore species Emiliania huxleyi is characterized by a wide range of sizes, which can be easily distinguished in the light microscope. In this study we have quantified the abundance of large (coccoliths &gt; 4 µm in maximum length) E. huxleyi specimens during the last 25 kyr in sedimentary records from eleven cores and drill sites in the NE Atlantic and W Mediterranean Sea, to prove its usefulness in the reconstruction of water mass dynamics and biostratigraphic potential. During the Last Glacial Maximum this large form, a cold-water indicator, was common in the NE Atlantic and Mediterranean, and its regional variation in abundance indicates a displacement of the climatic zones southwards in agreement with the development of ice sheets and sea ice in the Northern Hemisphere during this period. On the other hand, the gradient between northern and southern surface water masses in the Subtropical Gyre appears to have been more pronounced than at present, while the Portugal and Canary Currents were more intense. In the western Mediterranean basin temperatures were cooler than in the adjacent Atlantic, provoking a quasi-endemism of these specimens until the end of Heinrich Event 1. This may have been due to a restriction in the communication between the Atlantic and Mediterranean through the Strait of Gibraltar, the arrival of cold surface water and the amplification of cooling after the development of ice sheets in the Northern Hemisphere. During the deglaciation, large E. huxleyi specimens decreased in abundance at medium and low latitudes, but were still numerous close to the Subarctic region during the Holocene. In transitional waters this decrease to present day abundances occurred after Termination Ib. The abrupt change in abundance of this large E. huxleyi form is proposed as a new biostratigraphic event to characterize the Holocene in mid- to low-latitude water masses in the North Atlantic, although this horizon seems to be diachronous by 5 kyr from tropical to subarctic regions, in agreement with the gradual onset of warm conditions.
DOI: 10.15468/hqbf28
title: Benthic macrofauna abundance of sediment core 12930-059
DOI: 10.15468/wvyjah
title: Range table from planktonic foraminifers in ODP Hole 167-1012A
DOI: 10.15468/uvrbns
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station OCTOBER-1994-D4
DOI: 10.15468/2gnqjz
title: Total foraminifera counts of multinet M10/2_MSN298
DOI: 10.15468/qkcd6z
title: Nannofossil abundance of Hole 75-530
DOI: 10.15468/xdngwf
title: Pollen profile from Macon
DOI: 10.15468/89fv4s
title: Total foraminifera counts from M35/1_MSN1049
DOI: 10.15468/ztmwd8
title: (Table 12) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-688E, Part II
DOI: 10.15468/4wkrvj
title: Foraminifera abundance of Hole 58-442A
DOI: 10.15468/va9v2z
title: Palynological estimation of ODP Hole 189-1172A
DOI: 10.15468/z6m98u
title: Planktic foraminifera counts (census) of sediment core MD96-2084
DOI: 10.15468/eebgn5
title: Range table from benthic foraminifers in ODP Hole 159-961A
DOI: 10.15468/p5jbzt
title: (Table 2) Distribution of calcareous nannofossils from selected samples of ODP Hole 107-652A
DOI: 10.15468/e9s4sj
title: Planktic foraminifera abundance of Hole 22-213
DOI: 10.15468/gsyk5j
title: (Table 2) Distribution of sinsitral and dextral fohsellids in middle Miocene sediments of ODP Hole 130-806B from the Ontong Java Plateau, Pacific Ocean
DOI: 10.15468/6mscbf
title: Phytoplankton abundance at station CD47_3105C#4
DOI: 10.15468/qectqj
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/088-7
DOI: 10.15468/t6a79q
title: (Table 1) Numerical abundance counts of planktonic foraminifers and other biogenic constituents for ODP Hole 114-698A
DOI: 10.15468/635fcf
title: Range table from benthic foraminifers in ODP Hole 149-898B
DOI: 10.15468/qjhm3s
title: Range table from silicoflagellates, ebridians and actiniscidians in ODP Hole 141-860B
DOI: 10.15468/wx769s
title: Benthic foraminifera abundance of Hole 73-523
DOI: 10.15468/zyg5h9
title: (Appendix 2-4) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 31-292 in the western Pacific Ocean
DOI: 10.15468/4gqaax
title: Planktic foraminifera counts of sediment core V18-207
DOI: 10.15468/738hmh
title: (Table 11) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 90-589
DOI: 10.15468/csa236
title: Microzooplankton abundance measured on water bottle samples at station PS65/522-1
DOI: 10.15468/99qymh
title: Occurrence of mammalia relicts at site la Grotte du Thai
DOI: 10.15468/tvmk4s
title: (Figure 8b) Distribution of Cretaceous planktonic foraminifers, calpellionids and associated organisms from DSDP Hole 77-535
DOI: 10.15468/x5jzcm
title: Total foraminifera counts of multinet M21/4_MSN696
DOI: 10.15468/xvaqvt
title: Range table from ostracoda in ODP Hole 159-959D
DOI: 10.15468/87pmkc
title: Nematode abundances in sediments from the Nyegga pockmark area (Norwegian Sea) obtained during the VICKING expedition in 2006
DOI: 10.15468/gfbht2
title: (Table 3) Distribution of calcareous nannofossils in DSDP Hole 92-598
DOI: 10.15468/3qyx88
title: Planktic foraminifera abundance of Hole 27-263
DOI: 10.15468/c2jkhb
title: Uncorrected Mg/Ca and sea surface temperature data for Site 165-1000
DOI: 10.15468/rsnwra
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station SEPT-1998-MNB6
DOI: 10.15468/jqv2zj
title: Microzooplankton abundance and biomass at station NBP97-08-13-1
DOI: 10.15468/spf4s9
title: (Table DR1) Abundance of benthonic foraminifera in sediments from ODP Hole 113-690

description: A mass extinction of deep-sea benthic foraminifera has been documented globally, coeval with the negative carbon isotope excursion (CIE) at the Paleocene-Eocene boundary, which was probably caused by dissociation of methane hydrate. A detailed record of benthic foraminiferal faunal change over ~30 k.y. across the carbon isotopic excursion at the Ocean Drilling Program Site 690 (Southern Ocean) shows that shortly before the CIE absolute benthic foraminiferal abundance at that site started to increase. 'Doomed species' began to decrease in abundance at the CIE by a few thousand years. After the extinction faunas were dominated by small species, which resemble opportunistic taxa under high-productivity regions in the present oceans. Calcareous nannofossils (primary producers), however, show a transition to more oligotrophic nannofloras exactly where the benthic faunas show the opposite. Plankton and benthos is thus decoupled. Possibly, a larger fraction of food particles reached the seafloor after the CIE, so that food for benthos increased although productivity declined. Enhanced organic preservation might have resulted from low-oxygen conditions caused by oxidation of methane. Alternatively, and speculatively, there was a food-source at the ocean floor. Benthic foraminifera dominating the post-extinction fauna resemble living species that symbiotically use chemosynthetic bacteria at cold seeps. During increased, diffuse methane escape from hydrates, sulfate-reducing bacteria could have produced sulfide used by chemosynthetic bacteria, which in turn were used by the benthic foraminifera, causing extinction by a change in food supply.
DOI: 10.15468/87rdqc
title: (Appendix) Abundances of benthic foraminifera in ODP Hole 105-646B
DOI: 10.15468/twu89e
title: (Table 14) Benthic foraminifera in late Miocene sediments of DSDP Hole 90-592
DOI: 10.15468/vstsaq
title: Distribution of planktic foraminifera in surface sediment samples from cruise SO136
DOI: 10.15468/rw57gb
title: Benthic foraminifera abundance of Hole 80-549A
DOI: 10.15468/3bejz2
title: Foraminifera abundance of Hole 24-236
DOI: 10.15468/ue9gze
title: Plasm bearing foraminifera counts from M35/1_MSN1052
DOI: 10.15468/v7nwwp
title: Total foraminifera counts of multinet M10/2_MSN332
DOI: 10.15468/znw66q
title: (Table S5) Pliocene/Pleistocene benthic foraminiferal abundances from ODP Hole 172-1055B
DOI: 10.15468/7e3hee
title: Planktic foraminifer Globorotalia menardii counts on sediment core GeoB5133-1
DOI: 10.15468/cv9p9g
title: Total foraminifera counts of multinet M21/4_MSN713
DOI: 10.15468/5u7kf8
title: Total foraminifera counts of multinet M21/4_MSN700
DOI: 10.15468/467jvd
title: Phytoplankton abundance in surface water in May 1997, Callao, Peru
DOI: 10.15468/2v9xc9
title: (Table 5) Distribution of nannofossils in DSDP Hole 87-583F
DOI: 10.15468/gxt2h4
title: Occurrence of mammalia relicts at site Jägerhaus-Höhle
DOI: 10.15468/sx2y2c
title: Range table from planktonic foraminifers in ODP Hole 171-1050C
DOI: 10.15468/qspj89
title: Nematode genera abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/362-1
DOI: 10.15468/kmvmdj
title: Distribution of Quinqueloculina sp. in sediment core 13077-015
DOI: 10.15468/v3u376
title: Foraminifera species abundances from tow TT007_9-MOC18
DOI: 10.15468/a9hvuy
title: (Table 7) Distribution of Maestrichtian to late Campanian nannofossils in ODP Hole 108-661A
DOI: 10.15468/ndv8fj
title: Planktic foraminifera counts of sediment core V22-26
DOI: 10.15468/ya69px
title: (Table 2.2.1.1) Abundance of sympagic meiofauna of sea-ice core IO-9
DOI: 10.15468/zwfpqn
title: Phytoplankton abundance at station Casma_2003-03-27_1, Casma, Peru
DOI: 10.15468/jvhb4r
title: Living benthic foraminifera at station M33/1_MC-15 (WAST), size fraction 63-125 µm
DOI: 10.15468/apzvds
title: Planktic foraminifera abundance of Hole 51-417D
DOI: 10.15468/57wpn9
title: Coleccion Moluscos

description: Datos de todos los lotes de material seco depositados en la colección de moluscos del Instituto de Invertebrados, área Zoología de la Fundación Miguel Lillo. Incluyen datos de colecta, numero de ejemplares por lote y sistemática.
DOI: 10.15468/nppqry
title: Phytoplankton abundance in surface water in September 1996, Callao, Peru
DOI: 10.15468/heb66e
title: (Table 15) Ranges of benthic foraminifers through the early-middle Miocene in ODP Hole 115-709A
DOI: 10.15468/ruy5eg
title: Plasm bearing foraminifera counts of multinet M21/5_MSN728
DOI: 10.15468/3ep2x3
title: Relative abundance of ostracods in sediment core Oh09
DOI: 10.15468/d9p2n7
title: Planktic foraminifera abundance of Hole 7-62
DOI: 10.15468/73uytg
title: Range table from benthic foraminifers in ODP Hole 189-1170D
DOI: 10.15468/zbn642
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB01 in the euphotic zone of the Aegean Sea in March 1998. Part 3 - coccolithophores and other groups
DOI: 10.15468/jybnmc
title: Stable oxygen and carbon isotope ratios of Globigerinoides obliquus of quantitative range chart of the ostracodes in the Pliocene-Pleistocene interval of ODP Hole 107-654A

description: Deep-water benthic ostracodes from the Pliocene-Pleistocene interval of ODP Leg 107, Hole 654A (Tyrrhenian Sea) were studied. From a total of 106 samples, 40 species considered autochthonous were identified. Detailed investigations have established the biostratigraphic distribution of the most frequent ostracode taxa. The extinction levels of Agrenocythere pliocenica (a psychrospheric ostracode) in Hole 654A and in some Italian land sections lead to the conclusion that the removal of psychrospheric conditions took place in the Mediterranean Sea during or after the time interval corresponding to the Small Gephyrocapsa Zone (upper part of early Pleistocene), and not at the beginning of the Quaternary, as previously stated. Based on a reduced matrix of quantitative data of 63 samples and 20 variables of ostracodes, four varimax assemblages were extracted by a Q-mode factor analysis. Six factors and eight varimax assemblages were recognized from the Q-mode factor analysis of the quantitative data of 162 samples and 47 variables of the benthic foraminifers. The stratigraphic distributions of the varimax assemblages of the two faunistic groups were plotted against the calcareous plankton biostratigraphic scheme and compared in order to trace the relationship between the benthic foraminifers and ostracodes varimax assemblages. General results show that the two populations, belonging to quite different taxa, display almost coeval changes along the Pliocene-Pleistocene sequence of Hole 654A, essentially induced by paleoenvironmental modifications. Mainly on the base of the benthic foraminifer assemblages (which are quantitatively better represented than the ostracode assemblages), it is possible to identify such modifications as variations in sedimentation depth and in bottom oxygen content.
DOI: 10.15468/kezapq
title: Range table from planktonic foraminifers in ODP Hole 192-1183A
DOI: 10.15468/6tjqbk
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/038-3
DOI: 10.15468/7hhs5j
title: Nannofossil abundance of Hole 3-22
DOI: 10.15468/8v56ec
title: (Appendix 1, Table 4) Relative abundances of benthic foraminifera in Late Quaternary sediments of ODP Hole 122-760A in the southeast Indian Ocean
DOI: 10.15468/g9uckz
title: Range table from benthic foraminifera in ODP Hole 199-1220B
DOI: 10.15468/vru5cz
title: Microzooplankton abundance and biomass at station TT045_28-2