cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/2fnk5q
title: (Appendix A) Campanian-Maastrichtian calcareous nannofossils in DSDP Hole 44-390A

description: The latest Cretaceous (Campanian–Maastrichtian) is characterized by several global cooling and intermittent warming events. These climatic changes influenced the palaeoceanography substantially, including changes of the deep water sources and surface water currents. One of the most prominent episodes of climatic cooling occurred during the Campanian–Maastrichtian transition. This study focuses on the palaeoclimate and palaeoceanography of the Campanian–Maastrichtian transition by analysing the calcareous nannofossils of DSDP Hole 390A (139.92–126.15 mbsf; Blake Nose). For the examination of calcareous nannofossils sixty samples were processed using the settling technique. Biostratigraphical index taxa (Broinsonia parca constricta, Uniplanarius trifidus, and Tranolithus orionatus) suggest a late Campanian age for the major part of the studied section. The calcareous nannofossils are well preserved, highly abundant (6.80 billion specimens/gram sediment) and diverse (80 species/sample). The assemblages are dominated by Prediscosphaera spp. (20.5%), Watznaueria spp. (20.3%) and Retecapsa spp. (9.8%). Cool water taxa (Ahmuellerella octoradiata, Gartnerago segmentatum, and Kamptnerius magnificus), however, appear less frequently and do not exceed more than 1%. Due to their rarity these cool water taxa do not support the existence of an intense cooling phase during the Campanian–Maastrichtian transition at DSDP Hole 390A. Around 133 mbsf several nannofossil taxa, however, show a distinctive turnover. Mesotrophic species like Discorhabdus ignotus, Zeugrhabdotus bicrescenticus and Zygodiscus exmouthiensis are abundant below 133 mbsf, whereas oligotrophic taxa like Watznaueria spp., Eiffellithus spp. and Staurolithites flavus become common above this level. These changes imply a decrease in the input of nutrients, perhaps caused by a reorganization of ocean currents (Palaeo Gulf Stream) and reduced upwelling.
DOI: 10.15468/ttjwbr
title: Coccolith counts of multinet M32/5_MSN974
DOI: 10.15468/y2mt8n
title: (Table 2) Components of turbidite samples of ODP Leg 101 holes
DOI: 10.15468/z576mz
title: Meiofauna abundance in sediment core 54301-009
DOI: 10.15468/9bvs8b
title: Nekton and plankton counts from RMT (4500 µm) hauls of cruise GAE 1975/76
DOI: 10.15468/ezb47d
title: Benthic meiofauna abundance in surface sediment of core PLG93_BCORE2
DOI: 10.15468/n6dd65
title: Total foraminifera counts of multinet M21/4_MSN695
DOI: 10.15468/xhfv9n
title: Abundance of phytoplankton, heterotrophic nanoflagellates and bacteria through the water column at time series station L4 in the Western English Channel in 2008
DOI: 10.15468/tnm75t
title: Planktic foraminifera counts of sediment core RC17-113
DOI: 10.15468/j2bb9n
title: (Table 7) Benthic foraminifera genera assemblage at DSDP Section 80-548A-22
DOI: 10.15468/b4hz7c
title: Total foraminifera counts of multinet M21/6_MSN776
DOI: 10.15468/tyjt63
title: Planktic foraminifera abundance of Hole 34-319
DOI: 10.15468/43tm45
title: Pollen analysis of sediment profile NI0 from Niklassee
DOI: 10.15468/rhb6ue
title: (Table 1) Benthic foraminiferal distribution at ODP Site 127-794
DOI: 10.15468/ugeymw
title: (Table 15) Distribution of ostracode species in Core PS51/135-4
DOI: 10.15468/pjsh5e
title: (Appendix B) Stratigraphic occurrence of radiolarian special and species groups in sediments of ODP Hole 199-1218A
DOI: 10.15468/2tudta
title: (Table 2) Dissolution index (XDX) values and average test mass for four species of planktonic foraminifera
DOI: 10.15468/m3wchy
title: Assemblage of living benthic foraminifera in sediment core SO129_MC-03, 63-125 µm fraction
DOI: 10.15468/b93tp9
title: Faunal assemblage of sediment core TR149-35
DOI: 10.15468/jywpte
title: Occurrence of mammalia relicts at site Laugerie-Haut e-Ouest
DOI: 10.15468/2fx65h
title: Nannofossil abundance of Hole 31-298A
DOI: 10.15468/2g4m42
title: (Table 1) Abundance of planktonic foraminifera in ODP Hole 113-689B, large size fraction
DOI: 10.15468/s2f9x8
title: (Figure 9) Distribution of Cretaceous planktonic foraminifers and associated organisms from DSDP Hole 77-536
DOI: 10.15468/79pxxq
title: Distribution of benthic foraminifera in DSDP Hole 24-238 in the Central Indian Ocean (Appendix A)

description: Deep-sea benthic foraminifera have been quantitatively analyzed in samples (&gt;125 µm size fraction) from Ocean Drilling Program (ODP) Site 238, to understand paleoceanographic changes in the Central Indian Basin over the past 1.9 Myr. Factor and cluster analyses of the 25 highest-ranked species made it possible to identify five biofacies, characterizing distinct deep-sea environmental settings. The environmental interpretation of each biofacies is based on the ecology of recent deep-sea benthic foraminifera. The benthic faunal record indicates fluctuating deep-sea conditions in environmental parameters including oxygenation, surface productivity and organic food supply. These changes appear to be linked to Indian summer monsoon variability, the main climatic feature of the Indian Ocean region. The benthic assemblages show a major shift at ~0.7 to 0.6 Ma, marked by major turnovers in the relative abundances of species, coinciding with an increased amplitude of glacial cycles. These cycles appear to have influenced low latitude monsoonal climate as well as deep-sea conditions in the Central Indian Ocean Basin.
DOI: 10.15468/57cwcp
title: (Table 8D) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 89-586B, Sections 15-4 through 19-3
DOI: 10.15468/ecg7y9
title: Range table from benthic foraminifers in ODP Hole 146-891A
DOI: 10.15468/6kar4j
title: Occurrence of mammalia relicts at site Ceremosnica
DOI: 10.15468/nhy5jm
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/045-9
DOI: 10.15468/udctg6
title: Occurrence of mammalia relicts at site Erdhöhle
DOI: 10.15468/4qkecw
title: Phytoplankton abundance in surface water in October 1997, Chimbote, Peru
DOI: 10.15468/brp5ws
title: Total foraminifera counts of multinet POS231/3_MSN1329
DOI: 10.15468/vrwqpe
title: (Table 4b) Abundances of Globorotalia menardii in sediment core INMD-111BX
DOI: 10.15468/v7qd5d
title: (Appendix Table 3) Distribution of live benthic foraminifera in surface sediments
DOI: 10.15468/7zbzr6
title: (Appendix 3) Assemblage of benthic foraminifera in sediment core M5/2_KL15
DOI: 10.15468/k7jdnu
title: (Table 10) Distribution of planktonic foraminifers in ODP Hole 112-688A
DOI: 10.15468/k9nffv
title: Occurrence of mammalia relicts at site Velika Pecina
DOI: 10.15468/m62z4v
title: Sarcodine counts and carbon biomass at station TT012_5-PMOC8
DOI: 10.15468/977ahg
title: (Table 11) Distribution of coccoliths along Core AMK7-786 from the Tajura Rift
DOI: 10.15468/6j6fgb
title: Relativ abundances of dead fauna of benthic foraminifera in surface sediments (Table C2.2)
DOI: 10.15468/yhfegb
title: Microplankton counts and carbon biomass at station TT007_12-CTD145
DOI: 10.15468/fm7ynb
title: Microzooplankton abundance and biomass at station TT043_29-1
DOI: 10.15468/y5uddg
title: Planktic foraminifera distribution of sediment core 75KS52
DOI: 10.15468/3q7m2t
title: Distribution of living benthic foraminifera in sediment cores of cruise M77 Leg 1 and 2, 63-2000 µm fraction

description: Recent benthic foraminifera and their distribution in surface sediments were studied on a transect through the Peruvian oxygen minimum zone (OMZ) between 10 and 12°S. The OMZ with its steep gradients of oxygen concentrations allows to determine the oxygen-dependent changes of species compositions in a relatively small area. Our results from sediments of thirteen multicorer stations from 79 to 823 m water depth demonstrate that calcareous species, especially bolivinids dominate the assemblages throughout the OMZ. The depth distribution of several species matches distinct ranges of bottom water oxygen levels. The distribution pattern inferred a proxy which allows to estimate dissolved oxygen concentrations for reconstructing oxygen levels in the geological past.
DOI: 10.15468/ha6c4c
title: Foraminifera species abundances from tow TT011_11-MOC72
DOI: 10.15468/e6kkfq
title: (Table 16) Benthic foraminifera in Eocene-Oligocene sediments of DSDP Hole 90-593
DOI: 10.15468/3688wh
title: Microplankton abundance at Station MARCH-1997-GN36199704601MSB07 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/5pdfgj
title: Distribution of meiobenthos in sediment core M23_199 (2) of the northeastern Atlantic (Table 1)
DOI: 10.15468/ceb9ap
title: Assemblage of living benthic foraminifera in sediment core GeoB3712-1
DOI: 10.15468/7pjfma
title: (Table 8) Relative abundance of benthic foraminifera in ODP Hole 112-682A, Part I
DOI: 10.15468/7y9ksm
title: Total foraminifera counts from M35/1_MSN1052
DOI: 10.15468/upmjxh
title: Range table from planktonic foraminifers in ODP Hole 155-946A
DOI: 10.15468/wpvzut
title: Assemblage of dinoflagellate cysts analysed in sediment core SO78-158-1
DOI: 10.6084/m9.figshare.24498613
title: Raw Data - <b>Relationship of biological maturation and body surface area with fast-phase cardiac autonomic recovery in Brazilian Jiu-jitsu athletes</b>

description: In Brazilian Jiu-Jitsu (BJJ), athletes engage in multiple bouts with short intervals between them to vie for the championship, this requires broad efficiency of fast-phase cardiac autonomic recovery (CAR). Our aim was to verify the relationship between biological maturation (BM) and body surface area (BSA) and fast-phase CAR in BJJ athletes. This cross-sectional study involved 150 BJJ athletes, including 94 children and adolescents (Age: 10.6±1.5 years) and 56 adults (Age: 25.3±14.4). BM was assessed through peak height velocity (PHV). Athletes' BSA was categorized as low, medium, or high via anthropometric evaluations. Participants underwent high-intensity intermittent anaerobic physical exercise, by radio telemetry we acquired the peak heart rate and 60-s after physical exercise. Finally, the rapid phase CAR was analyzed using the 60-s heart rate recovery index. The results indicated that the pre-PHV group exhibited superior CAR compared to the during-PHV, post-PHV, and adult groups (η2p=0.450). Athletes with low BSA demonstrated enhanced CAR compared to those with medium and high BSA. The study concluded that both CAR depends on BM and BSA (η2p=0.252), regardless of the age group and BM stage. These findings have significant implications for tailored training and performance strategies, considering individual variations in BM and BSA.[P1]
DOI: 10.15468/r8zk6k
title: Range table from benthic foraminifers in ODP Hole 178-1099A
DOI: 10.15468/n92f6y
title: Range table from benthic foraminifers in ODP Hole 144-871A
DOI: 10.15468/jvmsru
title: Range table from nannofossils in ODP Hole 199-1216A
DOI: 10.15468/zdqngk
title: (Table DR1) Biofacies, percentages of important benthic foraminifera and isotope data at ODP Site 758

description: The Indian monsoon system, as recorded by ocean-floor biota (benthic foraminifera) at Ocean Drilling Program Site 758 in the eastern equatorial Indian Ocean, has varied dramatically over the past 5.5 m.y., long after the onset of the monsoons at 10-8 Ma. Benthic foraminifera that thrive with high productivity year-round were common before the formation of Northern Hemisphere continental ice sheets ca. 3.1-2.5 Ma, indicating that the summer (southwest) monsoon had high intensity and long seasonal duration. Ca. 2.8 Ma benthic faunas became dominated by taxa that flourish with a seasonally strongly fluctuating food supply, indicating that the northeast (winter) monsoon, during which primary productivity is relatively low, increased in duration and strength to form a system similar to that of today. The change occurred coeval with the initiation of the Northern Hemisphere glaciation, documenting a close link between the development of the Indian monsoon and Northern Hemisphere glaciation.
DOI: 10.15468/k57wvy
title: (Table 1) Preservation of sporomorphs in lithologic units III and IV of ODP Hole 120-750B
DOI: 10.15468/4fhwsm
title: Matter enrichment of the macrofauna community of MAC station 13200-005
DOI: 10.15468/9ku7s8
title: Abundance of microplanton determined from water bottle samples during AEGAEO cruise LIA-8
DOI: 10.15468/5z8j6e
title: (Table 3) Percentages of planktonic foraminiferal species and varieties from the sediment surface samples from the South China Sea
DOI: 10.15468/ajh68b
title: (Table 3) Palynomorph concentrations for ODP Site 105-645
DOI: 10.15468/a827p6
title: Microzooplankton abundance and biomass at station NBP97-08-09-1
DOI: 10.15468/gqdfdf
title: (Fig. 2) Abundance of Uvigerina pygmaea in sediment core MD95-2040
DOI: 10.15468/denaqk
title: (Table S1) Relative abundances of coccolithophore taxa in surface sediment samples from the Equatorial and Southeastern Pacific

description: This study aims to contribute to a more detailed knowledge of the biogeography of coccolithophores in the Equatorial and Southeastern Pacific Ocean. Census data of fossil coccoliths are presented in a suite of core-top sediment samples from 15°N to 50.6°S and from 71°W to 93°W. Following standard preparation of smear slides, a total of 19 taxa are recognized in light microscopy and their relative abundances are determined for 134 surface sediment samples. Considering the multivariate character of oceanic conditions and their effects on phytoplankton, a Factor Analysis was performed and three factors were retained. Factor 1, dominated by Florisphaera profunda and Gephyrocapsa oceanica, includes samples located under warm water masses and indicates the occurrence of calcite dissolution in the water column in the area offshore Chile. Factor 2 is related to cold, low-salinity surface-water masses from the Chilean upwelling, and is dominated by Emiliania huxleyi, Gephyrocapsa sp. &lt; 3 µm, Coccolithus pelagicus and Gephyrocapsa muellerae. Factor 3 is linked to more saline, coastal upwelling areas where Calcidiscus leptoporus and Helicosphaera carteri are the dominant species.
DOI: 10.15468/9z74sj
title: Distribution of Quinqueloculina sp. in sediment core 12930-084
DOI: 10.15468/tqs4jz
title: Relative abundance of planktic foraminifera in sediment core GeoB1523-1
DOI: 10.15468/qbdp8y
title: Phytoplankton abundance in surface water in October 1997, Ilo Peru
DOI: 10.15468/k37q5s
title: (Appendix 2-3) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 30-289 in the western Pacific Ocean
DOI: 10.15468/yrjkbc
title: Planktic foraminifera abundance of Hole 33-315A
DOI: 10.15468/qfxraz
title: (Table 5) Absolute abundances of planktonic foraminifera in Maastrichtian to upper Thanetian sediments of DSDP Hole 43-384
DOI: 10.15468/bhyas3
title: Abundance of microplankton from bottle APRIL-2000-K2
DOI: 10.15468/y2nbnr
title: Benthic meiofauna abundance in surface sediment of core PLG93_BCORE5
DOI: 10.15468/dda6r8
title: Meiofauna abundance in sediment core 12930-018
DOI: 10.15468/r9eywv
title: (Figure 5) Distribution and relative abundances of microbiota recovered from the Jurassic section of DSDP Hole 79-547B
DOI: 10.15468/86jw3f
title: Living benthic foraminifera at station M33/1_MC-30 (SAST), size fraction &gt;125 µm
DOI: 10.15468/6zz7pv
title: Microplankton counts and carbon biomass at station TT007_5-CTD53
DOI: 10.15468/33yzzf
title: Planktic foraminifera abundance of Hole 62-465A
DOI: 10.15468/pnzwx8
title: Phytoplankton abundance at bottle station A8/2
DOI: 10.15468/7rg736
title: (Table 4) Planktonic foraminifer abundance of ODP Hole 162-981A
DOI: 10.15468/afa65p
title: Phytoplankton abundance at station CD47_0606C#7
DOI: 10.15468/ju2qdj
title: Nematode genera abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/395-1
DOI: 10.15468/fnbuqp
title: Nannofossil abundance of Hole 64-481A
DOI: 10.15468/aqzyhc
title: Molluscs in surface sediments off Sylt collected during HEINCKE cruise HE218
DOI: 10.15468/zq4cbe
title: (Data S1) Palynology of IODP Hole 318-U1360A
DOI: 10.15468/szxrh3
title: (Table T2) Biogenic and mineral composition of sediments cored in Vaale, Schleswig-Holstein
DOI: 10.15468/9kuqxk
title: Range table from benthic foraminifers in ODP Hole 160-969B
DOI: 10.15468/vz3ptq
title: Planktic foraminifera counts of sediment core V24-28
DOI: 10.15468/kv58fg
title: Coccoliths in sediment core PS1113-1
DOI: 10.15468/wz7bg2
title: Benthic foraminifera distribution of sediment core ASV11-987 (ASV987)
DOI: 10.15468/2dygyy
title: Range table from ostracoda in ODP Hole 159-960C
DOI: 10.15468/pqvmyb
title: Nannofossil abundance of Hole 6-57A
DOI: 10.15468/zhy4eq
title: Phytoplankton abundance at station Casma_2003-02-27_1, Casma, Peru
DOI: 10.15468/aedstj
title: (Table 2) Abundance, preservation, and distribution of calcareous nannofossils in ODP Hole 135-840A
DOI: 10.15468/x5a9q9
title: Nannofossil abundance of Hole 73-521
DOI: 10.15468/gjvxs6
title: (Appendix 1) DSDP Site 94-607A ostracode species census data
DOI: 10.15468/8ygysx
title: (Tab. 11) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 32-304, Japanese Magnetic Lineations east of Japan
DOI: 10.15468/xbe5x6
title: Abundance and carbon biomass of phytoplankton at station TT007_5-CTD51
DOI: 10.15468/jtm75w
title: Range table from planktonic foraminifers in ODP Hole 182-1129D
DOI: 10.15468/8rx5as
title: Range table from benthic foraminifers in ODP Hole 149-899B
DOI: 10.15468/apwp65
title: Distribution of Quinqueloculina sp. in sediment core 13200-081
DOI: 10.15468/7jkx5g
title: (Table 3) Paleotemperature estimates for ODP Hole 105-646B
DOI: 10.15468/c25vgp
title: Range table from planktonic foraminifers in ODP Hole 157-954B
DOI: 10.15468/jeyr95
title: Abundance of phytoplankton, heterotrophic nanoflagellates and bacteria through the water column at time series station L4 in the Western English Channel in 2009
DOI: 10.15468/ta87gg
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V22-38
DOI: 10.15468/fa7a47
title: Diatom abundance of Hole 60-453
DOI: 10.15468/j9tzrm
title: Abundance of macrobenthos organisms in the northern Wadden Sea in 2010
DOI: 10.15468/n53up3
title: (Table 10) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-712A
DOI: 10.15468/4az95m
title: Planktic foraminifera counts of sediment core MD95-2040
DOI: 10.15468/dkt2gc
title: Total foraminifera counts from multinet SO119_MSN1286
DOI: 10.15468/bnz2xp
title: Total foraminifera counts of multinet M21/5_MSN733
DOI: 10.15468/jm2ses
title: Occurrence of mammalia relicts at site l´Abri des Battuts I
DOI: 10.15468/ry2ty6
title: Coccolith counts of multinet M32/5_MSN979
DOI: 10.15468/4wuk48
title: (Table 16B) Occurrences of planktonic foraminifers in DSDP Holes 90-594 and 90-594A
DOI: 10.15468/q5wv36
title: (Table 4) Standing stock values of important species in surface sediments
DOI: 10.15468/ur7pjp
title: (Table T2) Biostratigraphy of calcareous nannofossil taxa in ODP Hole 183-1136A
DOI: 10.15468/bxssqc
title: (Table 1) Oligocene benthic foraminifers abundance in ODP Hole 124-767B
DOI: 10.15468/mn6mm9
title: Nannofossil abundance of Hole 49-407
DOI: 10.15468/rj2cm8
title: Range table from benthic foraminifers in ODP Hole 139-856A
DOI: 10.15468/3ew5qa
title: Benthic foraminifera abundance of Hole 56-435A
DOI: 10.15468/7an943
title: Benthic macrofauna abundance of sediment core 12930-022
DOI: 10.15468/t46ejk
title: (Table T2) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole 171B-1049B
DOI: 10.15468/4apd7u
title: (Table 5) Ranges of benthic foraminifers from the late Oligocene to the early Miocene in ODP Hole 115-714A
DOI: 10.15468/43s3x5
title: Total foraminifera counts of multinet M21/4_MSN703
DOI: 10.15468/k7cdyw
title: Pollen data of trap CB1
DOI: 10.15468/2hzagt
title: Nannofossil abundance of Hole 9-82A
DOI: 10.15468/yz7k7u
title: (Appendix 2) Stratigraphic distribution of key and potential stratigraphic calcareous nannofossil markers in the upper Campanian–Maastrichtian of ODP Hole 122-762C
DOI: 10.15468/fa6gv9
title: Macrobenthos in surface sediments off Sylt collected during HEINCKE cruise HE262
DOI: 10.15468/ak37v2
title: Planktic foraminifera counts of sediment core V19-201
DOI: 10.15468/npkjcz
title: Occurrence of mammalia relicts at site l´Abri du Pont d´Ambon
DOI: 10.15468/rgu37x
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/042-2
DOI: 10.15468/cmm4tt
title: (Table 8) Distribution of planktonic and selected benthic foraminifers from DSDP Hole 87-584
DOI: 10.15468/2ctsup
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V29-179
DOI: 10.15468/pfppkp
title: Range table from benthic foraminifers in ODP Hole 145-887A
DOI: 10.15468/w6fy9w
title: (Table 2) Neogene benthic foraminifers of ODP Hole 120-748B
DOI: 10.15468/zfwzph
title: (Appendix 2, Table 4) Relative abundances of benthic foraminifera in Late Quaternary sediments of ODP Hole 122-762B in the southeast Indian Ocean
DOI: 10.15468/s6nxjq
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB03 in the euphotic zone of the Aegean Sea in spring 1997. Part 1 - diatoms
DOI: 10.15468/y73xey
title: Meiofauna densities from in situ feeding experiments in the Nazare Canyon conducted with sediments from ROV push-core JC10-95-PUC09
DOI: 10.15468/qxn6yv
title: Planktic foraminifera abundance of Hole 80-548
DOI: 10.15468/h6kp58
title: Total living benthic foraminifera at station M33/1_MC-03 (NAST), size fraction &gt;30 µm
DOI: 10.15468/qgnp4f
title: Nannofossil abundance of Hole 15-153
DOI: 10.15468/z8nk3v
title: Benthic macrofauna abundance of sediment core 13077-023
DOI: 10.15468/2f7b62
title: Nematode densities from in situ feeding experiments in the Nazare Canyon conducted with sediments from ROV push-core JC10-95-PUC09
DOI: 10.15468/2uudsb
title: Range table from planktonic foraminifers in ODP Hole 139-858B
DOI: 10.15468/chbnx7
title: Nannofossil abundance of Hole 10-90
DOI: 10.15468/hazevg
title: (Table 12A) Occurrences of planktonic foraminifers in selected samples of DSDP Holes 90-590 and 90-590A
DOI: 10.15468/a6haht
title: (Table 1) Occurrence and abundance of late Early Cretaceous radiolarians at DSDP Hole 62-463
DOI: 10.15468/ump6fd
title: Total foraminifera counts of multinet POS247/2_MSN1385
DOI: 10.15468/yc9d5w
title: (Appendix A) Benthic foraminiferal assemblages in sediments of the last 550 kyr of ODP Hole 130-807A from the Ontong Java Plateau, Pacific Ocean
DOI: 10.15468/xe48tc
title: Assemblage of living benthic foraminifera in sediment core CD145_55808#3, &gt;150 µm
DOI: 10.15468/gs3w2p
title: (Table 10) Planktonic foraminifer abundance of ODP Site 162-986
DOI: 10.15468/dgtcac
title: Biological data measured on water bottle sampels at station AT_II-119/5_26-4
DOI: 10.15468/a2qs9j
title: (Table 11) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-687A
DOI: 10.15468/8hz4p5
title: Nano and microzooplankton abundance and biomass at station NBP97-01-10-2
DOI: 10.15468/cbs94h
title: Nannofossil abundance of Hole 16-157
DOI: 10.15468/gafrgt
title: Range table from nannofossils in ODP Hole 139-855A
DOI: 10.15468/ku55ut
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-18-1
DOI: 10.15468/etkv45
title: Nannofossil abundance of Hole 19-192
DOI: 10.15468/5c7p9m
title: (Table 1) Distribution of planktonic foraminifers in ODP Hole 125-786A
DOI: 10.15468/kd9vxe
title: Relative abundance of dead benthic foraminifera in East Atlantic surface sediments off Senegal and Gambia (Table 2)
DOI: 10.15468/vyqhc4
title: (Figure 5) Planktonic foraminifera distribution in ODP Hole 101-628A
DOI: 10.15468/uk4bvj
title: Microzooplankton abundance measured on water bottle samples at station PS58/043-2
DOI: 10.15468/apd7rn
title: Abundance and carbon biomass of phytoplankton at station TT012_5-CTD56
DOI: 10.15468/63kjpm
title: (Table 2a) Abundance of macrobenthos species in samples from Cruise AMK54 stations in the Novaya Zemlya Trough
DOI: 10.15468/ruer68
title: Occurrence of mammalia relicts at site Pestera la Adam