cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/uhz9k4
title: Planktic foraminifera abundance of Hole 74-525A
DOI: 10.15468/sce2nk
title: Benthic foraminifera of sediment core MD99-2286
DOI: 10.15468/etu395
title: Occurrence of mammalia relicts at site Jaskinia Niedwiedzia
DOI: 10.15468/5hquz7
title: Plasm bearing foraminifera counts of multinet POS231/3_MSN1329
DOI: 10.15468/thjtbb
title: Planktic foraminifera counts of sediment core ELT48.022-PC
DOI: 10.15468/wym7g9
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 189-1172A
DOI: 10.15468/am7t2n
title: Total foraminifera counts of multinet M21/4_MSN705
DOI: 10.15468/ph5gg6
title: Relative abundances of middle Pleistocene benthic foraminifera in DSDP Site Site 90-594
DOI: 10.15468/swk7s3
title: Total foraminifera counts of multinet SO118_MSN1267
DOI: 10.15468/zkcc4w
title: Microzooplankton abundance measured on water bottle samples at station PS65/580-2
DOI: 10.15468/e3asrb
title: Nannofossil abundance of Hole 38-336
DOI: 10.15468/ndcjwv
title: Planktic foraminifera abundance of Hole 14-141
DOI: 10.15468/934gqh
title: Occurrence of mammalia relicts at site Istalloskö
DOI: 10.15468/cffuc8
title: Planktic foraminifera of surface sediments off Portugal and Morocco (Table 4)
DOI: 10.15468/ucwm79
title: Planktic foraminifera counts at CTD station M39/4_366CTD-22
DOI: 10.15468/7t7eg4
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 149-898A
DOI: 10.15468/bgggca
title: Live benthic foraminifera of surface sediments from the East Atlantic continental margin off Portugal (Table Tab. 4, 6)
DOI: 10.15468/n7baam
title: Range table from planktonic foraminifers in ODP Hole 178-1096B
DOI: 10.15468/3z9tgg
title: Phytoplankton abundance during Professor Vodyanitskiy cruise PV4
DOI: 10.15468/t28xzy
title: Phytoplankton abundance during Lev Titov cruise LT90/2
DOI: 10.15468/8hkqce
title: (Table 3+4) Abundance, biomass, production, and grazing of prokaryotes, nanoflagellates, ciliates, and dinoflagellates in three areas close to the Antarctic Peninsula in spring and summer 1995/96
DOI: 10.15468/cn242n
title: (Table 2) Range chart of calcareous nannofossils from Maud Rise sediment cores
DOI: 10.15468/7hs68t
title: Relative abundances of benthic foraminifera at the Cretaceous/Paleogene boundary in DSDP Hole 62-465A, Southern Hess Rise in the central North Pacific (Appendix A)

description: Uppermost Maastrichtian benthic foraminiferal assemblages (&gt;63 µm) are diverse, indicating mesotrophic conditions in lower bathyal DSDP Hole 465A (Hess Rise, central North Pacific), in 4 lower bathyal land sections in central-East and Northeastern Mexico, and in the upper to middle bathyal Agost section (Tethys area, Southeastern Spain). They indicate more eutrophic conditions in lower bathyal ODP Hole 1049C (Blake Nose, Northwestern Atlantic). Benthic foraminifers did not suffer significant extinction at the K/Pg boundary, but diversity and heterogeneity of the assemblages and the percentage of infaunal morphogroups decreased drastically in all sections, with the exception of DSDP Hole 465A where the percentage of infaunal taxa increased. These faunal changes probably reflect the effect on the benthic faunas of a widespread decrease in the food supply to the sea floor, as a result of the collapse of primary productivity at the K/Pg boundary. The decrease in food supply apparently affected the benthic faunas least at more eutrophic NW Atlantic ODP Site 1049 and at Pacific DSDP Site 465, which is distal from the impact site of the K/Pg bolide on the Yucatan Peninsula. At these sites the faunas recovered within the Parvulorugoglobigerina eugubina Biozone (~100 ky), although diversity and heterogeneity remained low through the early Danian, possibly indicating environmental stress. This stress might be related to a high or fluctuating food supply by primary producers that could not easily be used by the benthos, such as various bloom species of dinoflagellates. Benthic assemblages recovered more slowly (~300 ky) in the Mexican and Spanish sections. Low oxygen conditions after the K/Pg boundary could be inferred from the benthic assemblages at Agost (Southeastern Spain) only. A short episode of hypoxia, however, may be obscured at Pacific DSDP Hole 465A by drilling disturbance, and in the Mexican sections and Hole 1049C by incomplete sections due to downslope transport. Benthic foraminiferal assemblages thus appear to have been affected by the collapse of primary productivity at the K/Pg boundary to a different extent in different regions, and took different lengths of time for their recovery after the boundary.
DOI: 10.15468/mb6szh
title: Radiolaria assemblage in sediment core GIK23424-3
DOI: 10.15468/yrrupc
title: Foraminifera abundance of Hole 59-449
DOI: 10.15468/xyj7tk
title: Coccolith counts of multinet M32/5_MSN986
DOI: 10.15468/mpgqnv
title: Dinoflagellate cyst species composition of recent surface samples (Appendix)

description: Dinoflagellate cysts and other organic-walled microfossils have been studied in recent surface sediments from the entire Norwegian-Greenland Sea. More than 30 taxa have been recognized, of which only few show a distinct distribution pattern, and allow description of four assemblages. The occurrence of most taxa is related to the relatively warmer waters of the Norwegian Sea. Algidaspaeridium? minutum s.1., Brigantedinium simplex and Impagidinium? pallidum are the only species showing a preference for colder water masses. Two species, I.? pallidum and Nematosphaeropsis labyrinthus are mainly restricted to the oceanic environment, whereas the other species have also been reported from neritic environments in previous studies. Due to the limited knowledge of the ecological and sedimentological factors influencing the occurrence of dinoflagellate cysts in oceanic environments, their distribution in recent sediments can be only related to surface water masses in a broad sense. Although the distribution of assemblages correlates with specific surface water masses, comparison with assemblages recovered from sediment traps deployed basinwide in the Norwegian-Greenland Sea (Dale and Dale, 1992) revealed some major discrepancies in species composition and percentage abundances. The differences cannot be explained with certainty at the moment, although there is some evidence that transport of dinoflagellate cysts and other fossilizable microplankton in water masses by currents, in sea-ice and sediments may modify the assemblages found in recent oceanic surface sediments from the Norwegian-Greenland Sea.
DOI: 10.15468/dunkev
title: Range table from planktonic foraminifers in ODP Hole 139-858C
DOI: 10.15468/pa58jm
title: Planktic foraminifera counts in surface sediment samples
DOI: 10.15468/escm49
title: (Appendix A) Abundance of benthic foraminifera in sediment core GIK17940-2
DOI: 10.15468/4msajv
title: Plasm bearing foraminifera counts from M35/1_MSN1061
DOI: 10.15468/eghxmu
title: Range table from planktonic foraminifers in ODP Hole 167-1010C
DOI: 10.15468/xvb7cq
title: (Figure 6) Distribution of benthic foraminifers in middle-upper and Quaternary in DSDP Site 71-512
DOI: 10.15468/njd3h8
title: (Table 6b) Calcareous nannofossil distribution on ODP Hole 117-731C
DOI: 10.15468/2fhkxp
title: Total foraminifera counts of multinet M21/2_MSN627
DOI: 10.15468/td9qyw
title: Nannofossil abundance of Hole 60-456A
DOI: 10.15468/6pzaw8
title: (Table 3) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903C
DOI: 10.15468/sqb9e3
title: Plasm bearing foraminifera counts of multinet M21/2_MSN650
DOI: 10.15468/npm3zq
title: Foraminifera and stable isotopes of sediment core PS1754-1
DOI: 10.15468/dgybcw
title: (Tab. 14) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 32-307, Hawaiian Magnetic Lineations
DOI: 10.15468/fyv6hy
title: Microplankton abundance at Station MARCH-1998-GN36199804610MSB01 in the euphotic zone of the Aegean Sea in March 1998. Part 1 - diatoms
DOI: 10.15468/jkfb9n
title: Range table from planktonic foraminifers in ODP Hole 182-1129B
DOI: 10.15468/7g9bap
title: Microplankton data off Chipana Bay, 2006, Chile
DOI: 10.15468/xt3mac
title: Microplankton counts and carbon biomass at station TT008_4-TM3
DOI: 10.15468/shj2p3
title: Total foraminifera counts of multinet SO118_MSN1252
DOI: 10.15468/av7qt8
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 159-960A
DOI: 10.15468/dy7p9v
title: Dinoflagellate abundance of Hole 85-572A
DOI: 10.15468/qh2wn3
title: Microplankton counts and carbon biomass at station TT011_9-CTD115
DOI: 10.15468/qy84fk
title: (Table 3) Distribution of dinoflagellate cysts in ODP Hole 103-641A
DOI: 10.15468/xbvx86
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V34-88
DOI: 10.15468/7rcyam
title: Foraminifera species abundances from tow TT007_6-MOC12
DOI: 10.15468/gy4qmn
title: (Appendix E) Analyses of the benthic foraminifer assemblage at ODP Hole 112-681B
DOI: 10.15468/mwmcja
title: Polychaetes in surface sediments off Sylt collected during HEINCKE cruise HE272
DOI: 10.15468/ut5nrg
title: (Table 2) Counts of live (stained) benthic foraminifera from stations in the northern Gulf of California
DOI: 10.15468/qd6aab
title: (Appendix D) Stratigraphic occurrence of radiolarian special and species groups in sediments of ODP Hole 199-1220A
DOI: 10.15468/jwruze
title: Content of coarse fraction and G. menardii in sediment corev V25-49
DOI: 10.15468/ywrsuv
title: Benthic foraminifera abundance of Hole 96-622
DOI: 10.15468/ddkeuf
title: Nannofossil abundance of Hole 10-87
DOI: 10.15468/q83utn
title: (Table 10) Dinoflagellate cyst species distribution in ODP Hole 112-686B
DOI: 10.15468/bvpt7y
title: Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk

description: Based on analyses of taxonomic composition of planktonic foraminifera and oxygen isotopic composition of their shells in the sediment core V34-90 from the eastern slope of the USSR Academy of Sciences Rise in the southeast Sea of Okhotsk the main climatic and hydrological variations over the past 20 Ka have been traced and dated by the radiocarbon method. The followed periods have been revealed: glacial (20-12.5 Ka), deglaciation (12.5-8.0 Ka) with a pronounced cooling event (Late Drias about 10.8 Ka) and post deglaciation (last 8.0 Ka).
DOI: 10.15468/65b4vy
title: Sarcodine counts and carbon biomass at station TT012_5-PMOC7
DOI: 10.15468/qnb7kz
title: The nematoda fauna of sediment samples of Sarso Islands, Red Sea (Table 5)
DOI: 10.15468/m4h6uv
title: Microzooplankton abundance and biomass at station NBP97-08-36-1
DOI: 10.3886/qabx-kj88
title: Guatemala Threshold - Improving Customs: Final Analysis Report
DOI: 10.15468/vy99f5
title: (Appendix 2-8) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 86-577 in the western Pacific Ocean
DOI: 10.15468/qrg8ff
title: Nannofossil abundance of Hole 67-500
DOI: 10.15468/am27r3
title: Planktic foraminifera abundance of Hole 49-412
DOI: 10.15468/tt5rvg
title: Planktic foraminifera assemblage in sediment core GIK17725-1
DOI: 10.15468/2wu9ms
title: (Table 1) Late Pleistocene planktonic foraminifera of Hole 302-M0004C

description: Planktonic foraminifera populations were studied throughout the top 25 meters of the IODP ACEX 302 Hole 4C from the central Arctic Ocean at a resolution varying from 5cm (at the top of the record) to 10cm. Planktonic foraminifera occur in high absolute abundances only in the uppermost fifty centimetres and are dominated by the taxa Neogloboquadrina pachyderma. Except for a few intermittent layers below this level,most samples are barren of calcareous microfossils.Within the topmost sediments, Neogloboquadrina pachyderma specimens present large morphological variability in the shape and number of chambers in the finalwhorl, chamber sphericity, size, and coiling direction. Five morphotypeswere identified among the sinistral (sin.) population (Nps-1 to Nps-5), including a small form (Nps-5) that is similar to a non-encrusted normal form also previously identified in the modern Arctic Ocean watermasses. Twenty five percent of the sinistral population is made up by large specimens (Nps-2, 3, 4), with a maximal mean diameter larger than 250µm. Following observations made in peri-Arctic seas (Hillaire-Marcel et al. 2004, doi:10.1016/j.quascirev.2003.08.006), we propose that occurrence of these large-sized specimens of N. pachyderma (sin.) in the central Arctic Ocean sediments could sign North Atlantic water sub-surface penetration.
DOI: 10.15468/bz5vb3
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-22-5
DOI: 10.3886/w035-8r39
title: Guatemala Threshold - Improving Customs: Final Analysis Report
DOI: 10.15468/hu2yj7
title: (Table 6) Pleistocene nannofossil range chart for ODP Hole 134-830B
DOI: 10.15468/cmxsq7
title: Foraminifera distribution of sediment core T87/2/27G
DOI: 10.15468/6kgua3
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB02 in the euphotic zone of the Aegean Sea in spring 1997. Part 2 - dinoflagellates
DOI: 10.15468/fw4uuz
title: Nannofossil abundance of Hole 9-77B
DOI: 10.15468/cs8v96
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC13-228
DOI: 10.15468/mph2yq
title: Abundance of benthos infauna at station POS128/2_258
DOI: 10.15468/q6pxrd
title: Range table from planktonic foraminifers in ODP Hole 182-1126D
DOI: 10.15468/p2pteh
title: Planktic foraminifera abundance of Hole 29-284
DOI: 10.15468/p9y2wf
title: (Appendix Table 2) Number of planktonic foraminiferal genera and species in Late Creatceous sediments of ODP Hole 122-763B from the Exmouth Plateau, eastern Indian Ocean
DOI: 10.15468/r6c5kp
title: Oberservation of birds at station PS14/149 along 49° West
DOI: 10.15468/47ugjz
title: Dinoflagellate abundance of Hole 38-338
DOI: 10.15468/j8hkqf
title: Assemblage of living benthic foraminifera in sediment core SO118_MC-35, &gt;125 µm fraction
DOI: 10.15468/uethpg
title: Relative abundance of Neogene nannofossils at ODP Site 138-846 from the eastern equatorial Pacific
DOI: 10.15468/bjfzyp
title: Nannofossil abundance of Hole 8-72
DOI: 10.15468/ky5cd4
title: Nannofossil abundance of Hole 1-2
DOI: 10.15468/qdt29t
title: Census of calcareous nannofossil taxa expressed as percent of total number of individuals counted, ODP Site 114-699
DOI: 10.15468/ymc232
title: (Table 3) Calcareous nannofossil distribution in the Upper Cretaceous of ODP Site 120-750
DOI: 10.15468/x4g77t
title: (Table 2) Pleistocene to Miocene ostracodes from ODP Hole 104-642B
DOI: 10.15468/ebm3zg
title: Assemblage of dinoflagellate cysts analysed in sediment core SO78-173-3
DOI: 10.15468/bbh7ty
title: Assemblage of living benthic foraminifera in sediment core GeoB4917-5
DOI: 10.15468/z648dy
title: Planktic foraminifera abundance of Hole 26-251
DOI: 10.15468/g6693w
title: (Table 4) Pleistocene to Miocene ostracodes from ODP Hole 104-643A
DOI: 10.15468/6uv3w4
title: (Table T4) Abundance of foraminifers and presence of other fragments in ODP Hole 188-1166A sediments
DOI: 10.15468/petm3b
title: Total foraminifera counts of multinet M10/2_MSN317
DOI: 10.15468/3t5947
title: Range table from planktonic foraminifers in ODP Hole 180-1118A
DOI: 10.15468/8aa3mc
title: Occurrence of mammalia relicts at site Pestera Livadita
DOI: 10.15468/7wucxv
title: Analyses of the recent components in the sand fraction of sediment core PS1223-1
DOI: 10.15468/tswczn
title: (Table 6) Dinoflagellate cyst species distribution in ODP Hole 112-679D
DOI: 10.15468/y497c4
title: (Table 1) Distribution of Upper Cretaceous agglutinated benthic foraminifers in DSDP Hole 20-196
DOI: 10.15468/5a33tz
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V30-97
DOI: 10.15468/zzf7ve
title: Benthic foraminifera abundance of Hole 42-380A
DOI: 10.15468/hwm3kv
title: Range table from planktonic foraminifers in ODP Hole 139-856E
DOI: 10.15468/7sryhb
title: (Appendix C) Stratigraphic range and relative abundance of Paleogene planktonic foraminifera in ODP Hole 120-748B
DOI: 10.15468/5r2f6w
title: (Appendix C) Distribution of benthic foraminifera in surface sediments from the Chatham Rise
DOI: 10.15468/z5jvrx
title: Range table from ostracoda in ODP Hole 144-873B
DOI: 10.15468/bbcgh8
title: Range table from ostracoda in ODP Hole 143-865A
DOI: 10.15468/h964vf
title: Nannofossil abundance of Hole 47-398A
DOI: 10.15468/37qkd9
title: Abundance of benthic infauna in surface sediments from the North Sea sampled during Walther Herwig cruise WH220
DOI: 10.15468/8xafrt
title: Calcareous dinoflagellate cysts of multicorer M51/3_569-3, grain fraction &lt; 20µm
DOI: 10.15468/jbbf54
title: Microplankton counts and carbon biomass at station TT012_5-CTD59
DOI: 10.15468/gq8cb8
title: Abundance of planktic foraminifera at CTD station PS55/019
DOI: 10.15468/a8gcpa
title: Phytoplankton abundance at station Sechin_EP1 in 2002, Casma, Peru
DOI: 10.15468/gkr7nz
title: Pollen analysis of sediment profile MU1 from Muggesfelder See
DOI: 10.15468/zw232s
title: Occurrence of mammalia relicts at site Remetehegy
DOI: 10.15468/x3vckw
title: (Table T5) Biogenic and mineral composition of sediments cored in Westerland, Sylt
DOI: 10.15468/bzpp5w
title: Distribution of planktic foraminifers of core 138-846B
DOI: 10.15468/xcztf3
title: Phytoplankton abundance in surface water in September 1996, Chimbote, Peru
DOI: 10.15468/6929qk
title: Planktic foraminifera abundance of Hole 6-48B
DOI: 10.15468/v9khcj
title: Smear slide analysis for the boxcorer GeoB4205-1
DOI: 10.15468/zas354
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station JUNE-1998-IR43
DOI: 10.15468/7nc6ew
title: Abundance of radiolaria at station UT99-4-2
DOI: 10.15468/8p28vq
title: Distribution of meiobenthos in sediment core M19_216-2 of the northeastern Atlantic (Table 1)
DOI: 10.15468/46z7uq
title: (Table V) Distribution of diatoms in samples from Heidemann Valley trench, Antarctica
DOI: 10.15468/xmv7yc
title: Total foraminifera counts from multinet M31/3_MSN923
DOI: 10.15468/3x4a4d
title: Total foraminifera counts from M35/1_MSN1046
DOI: 10.15468/b8wd62
title: Ostracoda abundance of Hole 95-613
DOI: 10.15468/etkc5c
title: (Table T4) Paleocene calcareous nannofossil abundance of ODP Hole 173-1069A
DOI: 10.15468/cx685k
title: Microzooplankton abundance and biomass at station NBP97-08-08-1
DOI: 10.15468/qtm6em
title: (Table 5) Distribution of late Eocene calcareous nannofossils in ODP Hole 149-900A
DOI: 10.15468/tjg5h9
title: Sarcodine counts and carbon biomass at station TT008_5-PMOC6
DOI: 10.15468/w2pc6q
title: (Table 2.2.1.1) Abundance of sympagic meiofauna of sea-ice core IO-13
DOI: 10.15468/bybzzy
title: Percentages of planktonic foraminifera species in sediment core V25-75
DOI: 10.15468/c32cvx
title: Total foraminifera counts of multinet POS231/3_MSN1331
DOI: 10.15468/pdhwuy
title: (Appendix B) Benthic foraminifera in Indian Ocean surface sediments

description: Multivariate analysis was performed on percentages of 46 species of unstained deep-sea benthic foraminifera from 131 core-top to near-core-top samples (322–5013 m) from across the Indian Ocean. Faunal data are combined with GEOSECS geochemical data to investigate any relationship between benthic foraminifera (assemblages and species) and deep-sea properties. In general, benthic foraminifera show a good correlation to surface productivity, organic carbon flux to the sea floor, deep-sea oxygenation and, to a lesser extent, to bottom temperature, without correlation with the water depths. The foraminiferal census data combined with geochemical data has enabled the division of the Indian Ocean into two faunal provinces. Province A occupies the northwestern Indian Ocean (Arabian Sea region) where surface primary production has a major maximum during the summer monsoon season and a secondary maximum during winter monsoon season that leads to high organic flux to the seafloor, making the deep-sea one of the most oxygen-deficient regions in the world ocean, with a pronounced oxygen minimum zone (OMZ). This province is dominated by benthic foraminifera characteristic of low oxygen and high organic food flux including Uvigerina peregrina, Robulus nicobarensis, Bolivinita pseudopunctata, Bolivinita sp., Bulimina aculeata, Bulimina alazanensis, Ehrenbergina carinata and Cassidulina carinata. Province B covers southern, southeastern and eastern parts of the Indian Ocean and is dominated by Nuttallides umbonifera, Epistominella exigua, Globocassidulina subglobosa, Uvigerina proboscidea, Cibicides wuellerstorfi, Cassidulina laevigata, Pullenia bulloides, Pullenia osloensis, Pyrgo murrhina, Oridorsalis umbonatus, Gyroidinoides (= Gyroidina) soldanii and Gyroidinoides cf. gemma suggesting well-oxygenated, cold deep water with low (oligotrophic) and pulsed food supply.
DOI: 10.15468/g8rw26
title: (Table 10) Ranges of benthic foraminifers through the Oligocene in DSDP Hole 24-238
DOI: 10.15468/yag458
title: Range table from planktonic foraminifers in ODP Hole 144-873A
DOI: 10.15468/53x7yf
title: (Table 1) Distribution of ostracods in Jurassic sediments of DSDP Hole 79-547

description: Eighteen samples from the Early Jurassic (Hettangian to Pliensbachian) and nine from the Bajocian to Berriasian interval have been examined. The ostracode fauna has been left largely in open nomenclature pending a more detailed study. At least four new genera, listed simply as Gen. nov. A-D sp. nov. have been recognized. Although many new species are present, there is a similarity between this ostracode fauna and that of northwest Europe of comparable age. This is particularly true for the Early Jurassic from which Bairdia guttulae Herrig, 1979, Ptychobairdia cf. aselfingenensis (Lord and Moorley, 1974), Monoceratina scrobiculata Triebel and Bartenstein, 1938, Bairdia sp. 4134 Michelsen, 1975, Ogmoconcha cf. contractula Triebel, 1941, and Paracypris cf. redcarensis Blake, 1876 have been obtained. Monoceratina vulsa (Jones and Sherborn, 1888), present in the Toarcian to Callovian of Britain, is recorded here from a sample provisionally dated as Bajocian to Callovian on foraminiferal evidence. The more important species are illustrated and their distribution recorded in Table 1.
DOI: 10.15468/bfq6gx
title: (Table 7) Distribution of Pleistocene to Miocene nannofossils in ODP Hole 108-661A
DOI: 10.15468/g4v5uy
title: (Table 1) Occurrence of bottom invertebrates in the Canary upwelling area
DOI: 10.15468/wt66k4
title: (Table 6) Distribution of live benthic foraminifera in deep-sea surface sediments of the Scotia Sea, part 2
DOI: 10.15468/5x76cm
title: Range table from benthic foraminifers in ODP Hole 144-871B