cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/6awq7b
title: Phytoplankton abundance and species composition in the Gulf of Naples from February to December 1987
DOI: 10.15468/p8vcjm
title: Nano and microzooplankton abundance and biomass at station NBP97-01-19-2
DOI: 10.15468/9ytxme
title: Nannofossil abundance of Hole 58-443
DOI: 10.15468/ftqyfu
title: (Table 7) Distribution of ostracode species in surface sediments of the central Laptev Sea
DOI: 10.15468/pjry82
title: Benthic foraminifera abundance of Hole 42-371
DOI: 10.15468/yk2tmd
title: Microplankton abundance at bottle station SEPT-1999-K3
DOI: 10.15468/8vqtqe
title: (Table 5) Foraminiferal numbers of empty test of important species in surface sediments
DOI: 10.15468/fxv95v
title: Phytoplankton abundance in surface water in 1993, Ancon, Peru
DOI: 10.15468/9gy6yb
title: Nanoplankton data off Chipana Bay, summer 2006, Chile
DOI: 10.15468/nbkak8
title: Assemblage of living benthic foraminifera in sediment core CD145_55818#4, &gt;150 µm
DOI: 10.15468/2nasbu
title: (Table A.10) Foraminiferal census data of sediment core PS1243-1 during marine isotopic stage 1-3 (150-500 µm)
DOI: 10.15468/bxfnc6
title: (Figure 2) Planktonic foraminifera abundance in DSDP Hole 93-603C

description: Three holes were drilled at Site 603 on the continental rise off the U.S. east coast during DSDP Leg 93. A thick Pliocene section and a few meters of lowermost Quaternary sediments were recovered in Hole 603C. A detailed biostratigraphic analysis, based on planktonic foraminiferal distribution, allowed us to delineate precisely all the Pliocene zones (sensu Berggren, 1977). The Quaternary sequence was eroded beyond Ericson's Zone P. The calculated sediment accumulation rate remained relatively high during most of the Pliocene, reaching a maximum of 150 m/Ma in Zone PL4. Quantitative micropaleontological methods enabled us to delineate several paleoclimatic and paleoceanographic events, including those at 4.3 and 3.4 Ma.
DOI: 10.15468/scsa8h
title: (Table 16) Ranges of benthic foraminifers through the Neogene in ODP Hole 115-710A
DOI: 10.15468/xkbany
title: Range table from benthic foraminifers in ODP Hole 139-856E
DOI: 10.15468/g7zaa4
title: Occurrence of mammalia relicts at site Teufelsbrücke
DOI: 10.15468/emcbx7
title: Range table from planktonic foraminifers in ODP Hole 144-873B
DOI: 10.15468/2w89uv
title: Foraminifera abundance of Hole 48-405
DOI: 10.15468/7d3tsz
title: Total foraminifera counts of multinet M21/1_MSN614
DOI: 10.15468/7btd66
title: Phytoplankton abundance at station CD47_2805C#5
DOI: 10.15468/qzggrp
title: Nannofossil abundance of Hole 64-474
DOI: 10.15468/6mhqg7
title: Sarcodine counts and carbon biomass at station TT012_5-TM47
DOI: 10.15468/sy7pu6
title: Range table from benthic foraminifers in ODP Hole 144-879A
DOI: 10.15468/q8ut33
title: Plasm bearing foraminifera counts of multinet SO117_MSN1244
DOI: 10.15468/jvqcwp
title: (App 11) Relative contents of mass species of planktonic foraminifera in sediments from Core S-17954
DOI: 10.15468/dprhe4
title: (Figure 4) Distribution of benthic foraminifers in the Upper Cretaceous of DSDP Hole 71-511
DOI: 10.26093/cds/vizier.36580069
title: RVs of B stars in NGC 6231

description: VizieR online Data Catalogue associated with article published in journal Astronomy & Astrophysics with title 'The observed multiplicity properties of B-type stars in the Galactic young open cluster NGC 6231.' (bibcode: 2022A&A...658A..69B)
DOI: 10.15468/p9aba5
title: Composition of the larger coarse silt fraction in surface sediments of the northwest African continental margin (Appendix Tab. 4)
DOI: 10.15468/tukhnf
title: Sarcodine counts and carbon biomass at station TT007_5-CTD53
DOI: 10.15468/jw29qu
title: Nannofossil abundance of Hole 8-73
DOI: 10.15468/mnhtqc
title: (Table 4) Concentrations of PCBs and MeSO2-PCBs in adipose tissue of polar bears (Ursus maritimus) between 1991-2007
DOI: 10.15468/2ynvej
title: Total foraminifera counts of multinet POS200/6_MSN837
DOI: 10.15468/r62kjx
title: (Table T3) Abundance of dinoflagellates and other palynomorphs in Maastrichtian-Eocene sediments from ODP Hole 189-1172D
DOI: 10.15468/vj9xkp
title: (Figure 3) Occurrence of planktonic foraminifers and other selected constituents in samples from DSDP Hole 80-548A
DOI: 10.15468/t7ur7k
title: Nannofossil abundance of Hole 47-397
DOI: 10.15468/rfbpxw
title: Microplankton abundance at Station SEPT-1997-GN36199704606MNB04 in the euphotic zone of the Aegean Sea in September 1997. Part 2 - dinoflagellates
DOI: 10.26093/cds/vizier.36720159
title: M67 late-type stars light curves

description: VizieR online Data Catalogue associated with article published in journal Astronomy & Astrophysics with title 'New insights into the rotational evolution of near-solar age stars from the open cluster M67.' (bibcode: 2023A&A...672A.159G)
DOI: 10.15468/4wcfdx
title: Diatom abundance measured on water bottle samples at station PS58/108-1
DOI: 10.15468/jjfdym
title: (Table 4a) Miocene biostratigraphy of the Reinbekian stage in Schleswig-Holstein
DOI: 10.15468/2eqkqb
title: (Figure 5) Range charts of selected dinoflagellate cysts in ODP Hole 122-763C
DOI: 10.15468/d67fpe
title: Phytoplankton abundance at station Sechin_2003-08-27_1, Casma, Peru
DOI: 10.15468/y4r3vq
title: Benthic macrofauna abundance of sediment core 13200-020
DOI: 10.15468/b49yxy
title: Planktic foraminifera (%) of sediment core MD97-2151
DOI: 10.15468/mcvqyd
title: Benthic foraminiferal assemblage in the 125-250 micron fraction of sediment core PS1745-5 (Table 5)
DOI: 10.15468/3tdrdb
title: Distribution of calcareous foraminifers in sediment core Well 6406/8-1
DOI: 10.15468/pzwhy5
title: Pollen profile from Wurzacher Becken

description: Interglacial lacustrine sediments of 0.3-0.6 m thickness are found in the basin of Wurzach over a distance of about 9 km as detected by 5 borings. The interglacial bed is intercalated between lacustrine sediments of Würm (above) and glaciolacustrine sediments of the Younger Riss (below). Most of the Würmian sediments are silty-sandy, calcareous and varved deposits. They were deposited as bottom sediments of a delta, which had formed in the glacial lake filling the Wurzach basin during the Upper Würm. The terminal moraine of the Younger Riss is found in the N and S of the Reed of Wurzach. In the NE it is overlain by sediments of Würm and Holocene age. The pollen bearing part of the new profile represents the last interglacial period (except its earliest phases), the two Lower Würm interstadials, which are equivalents of the Brørup and Odderade interstadial phases, and a third interstadial, the Dürnten, known from other localities in the forelands of the Alps with a forest vegetation, which consisted mainly of spruce and larch trees, and the intercalated stadial phases. These interstadials are different from those described earlier by FILZER, which on the contrary represent cold periods with highly increased reworking of pollen. The equivalents of the Brørup, Odderade and Dürnten interstadials are the "Kiefer-Fichten-Kampfzeit" and part of the "Kiefernzeit mit Fichte" of FILZER. The characteristic series of climatic events known already from a great number of sites scattered all over Europe and again at Wurzach proves that the Riss/Würm- and the Eem interglacial periods are time-equivalents. Differing amounts of Carpinus and Abies at different places in the northern foreland of the Alps are related to the migration history of the two species during the last interglacial period and must not be used to distinguish different types of interglacials (type Zeifen, type Pfefferbichl).
DOI: 10.15468/ytzvag
title: (Table 2) Benthic foraminiferal genera in DSDP Core 95-612-37-3
DOI: 10.26093/cds/vizier.36750105
title: LeMMINGs V. Nuclear activity and bulge properties

description: VizieR online Data Catalogue associated with article published in journal Astronomy & Astrophysics with title 'LeMMINGs. V. Nuclear activity and bulge properties: A detailed multi-component decomposition of e-MERLIN Palomar galaxies with HST.' (bibcode: 2023A&A...675A.105D)
DOI: 10.15468/4pxdup
title: Content of G. menardii in sediment core V25-69
DOI: 10.15468/zf34re
title: Distribution of planktic foraminifera (125-250 µm) of sediment core PS1243-1
DOI: 10.15468/wnqtqb
title: Raw counts of dinoflagellate cysts in several IODP and DSDP holes
DOI: 10.15468/45xxzn
title: Planktic foraminifera assemblage in sediment core SU92-21
DOI: 10.15468/uswweg
title: Plasm bearing foraminifera counts of multinet M12/3_MSN557
DOI: 10.15468/46ftr4
title: Nannofossil abundance of Hole 5-32
DOI: 10.15468/bqfmp3
title: (Table 2) Monthly statistics of king penguin (Aptenodytes patagonicus) colony arrivals, Possession Island
DOI: 10.15468/pcn92j
title: (Table B) Abundance of benthic fauna associated with shrimp swarms at hydrothermal fields on the Mid-Atlantic Ridge
DOI: 10.15468/t7p2nh
title: Analyses of the recent components of sediment core PS1217-1
DOI: 10.15468/8dnt9z
title: Census of calcareous nannofossil taxa expressed as percent of total number of individuals counted, ODP Site 119-744
DOI: 10.15468/kue53d
title: Range table from planktonic foraminifers in ODP Hole 146-888B
DOI: 10.15468/k7t7t4
title: Total foraminifera counts of multinet M21/2_MSN656
DOI: 10.15468/yq4xn5
title: (Table 2c) Percentages of energy flow of macrobenthos species in samples from Cruise AMK54 stations in the Novaya Zemlya Trough
DOI: 10.15468/w3fz98
title: (Table 2) Relative abundance of benthic foraminifera in ODP Hole 112-680B
DOI: 10.15468/zevm6h
title: Phytoplankton abundance at station Sechin_2003-10-03_1, Casma, Peru
DOI: 10.15468/agd49e
title: Range table from planktonic foraminifers in ODP Hole 152-918D
DOI: 10.15468/nqdnh8
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 191-1179B
DOI: 10.15468/z2tw42
title: Tab. A6: Anzahl von M. balthica während der Ansiedlungszeit
DOI: 10.15468/mwg7th
title: Phytoplankton abundance at station DI183_11872#3
DOI: 10.15468/bdcaw5
title: Range table from planktonic foraminifers in ODP Hole 192-1184A
DOI: 10.15468/334grf
title: (Table 1) Mineralogy of ODP Hole 113-692B
DOI: 10.15468/krndxa
title: Total foraminifera counts of multinet M36/6_MSN1195
DOI: 10.26093/cds/vizier.36750090
title: dE galaxies K-band images

description: VizieR online Data Catalogue associated with article published in journal Astronomy & Astrophysics with title 'Deep K-band surface brightness photometry of dE galaxies. I. Local Volume and Virgo cluster.' (bibcode: 2023A&A...675A..90P)
DOI: 10.15468/5d6mza
title: Planktic foraminifera abundance of Hole 40-363
DOI: 10.15468/nku7yb
title: Total foraminifera counts of multinet M21/6_MSN766
DOI: 10.15468/3etgcr
title: (Appendix A2) Relative abundance of key planktonic foraminifera in Oligocene sediments of ODP Site 199-1218 in the equatorial Pacific
DOI: 10.15468/2njjtu
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 151-911A
DOI: 10.26093/cds/vizier.36759001
title: HD 100453 disk K1-band image

description: VizieR online Data Catalogue associated with article published in journal Astronomy & Astrophysics with title 'Dynamical detection of a companion driving a spiral arm in a protoplanetary disk.' (bibcode: 2023A&A...675L...1X)
DOI: 10.15468/w9jrac
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/048-3
DOI: 10.15468/87wacj
title: Nannofossil abundance of Hole 1-4
DOI: 10.15468/pkcyc2
title: (Table 2) Distribution of benthic foraminifera in ODP Hole 120-748A
DOI: 10.15468/8mufd8
title: Diatom assamblage in samples from sediment trap NB6
DOI: 10.15468/hyjsu4
title: Planktic foraminifera abundance of Hole 4-25
DOI: 10.15468/3nrycg
title: Microfossil abundance of Hole 50-415
DOI: 10.15468/b2w3zr
title: Planktic foraminifera abundance of Hole 84-570
DOI: 10.15468/hhtupa
title: (Table 1) Relative abundance of planktic foraminifera at DSDP Site 48-401 from the Bay of Biscay, North Atlantic
DOI: 10.15468/wnvq69
title: Microzooplankton (larger protists and small copepods) abundance measured on concentrated water bottle samples at station PS65/509-16
DOI: 10.15468/bz3r7t
title: Dinoflagellate abundance of Hole 94-611
DOI: 10.15468/rqp8an
title: (Table 3) Distribution of calcareous nannofossils in Cretaceous sediments recovered in ODP Site 129-801
DOI: 10.15468/xrk2wh
title: (Table 11) Benthic foraminifera in Pliocene sediments of DSDP Hole 90-591
DOI: 10.15468/9sbgqk
title: Planktic foraminifera abundance of Hole 67-498A
DOI: 10.15468/btgdv3
title: Meiofauna abundance in sediment core 13200-012
DOI: 10.15468/msg72k
title: Plasm bearing foraminifera counts of multinet M21/1_MSN609
DOI: 10.15468/jjrfdf
title: Nannofossil abundance of Hole 10-87
DOI: 10.15468/p3nk38
title: Benthic foraminifera abundance of Hole 76-533A
DOI: 10.15468/m5e85d
title: Planktic foraminiferal assemblage for the 10kyr time slice from different sediment cores
DOI: 10.15468/qwsh47
title: Macrobenthos in surface sediments off Sylt collected during HEINCKE cruise HE236
DOI: 10.15468/wrpwzj
title: (Appendix) Distribution of planktonic foraminifers at DSDP Hole 72-516F, Coniacian-Santonian to upper Maestrichtian

description: During Leg 72 in the western South Atlantic, Cretaceous sediments were recovered only at Hole 516F (Rio Grande Rise). Late Cretaceous planktonic foraminifers were found in Cores 516F-89 through 516F-122 (between 964 and 1235 m sub-bottom); they are assigned to the late Coniacian to the latest Maestrichtian. Frequency and preservation of planktonic foraminifers are moderate in the upper Maestrichtian and deteriorate from there to the base. Only the upper Maestrichtian Abathomphalus mayaroensis Zone can be clearly delimited according to the generally accepted planktonic foraminiferal zonation; moreover, some of the more important zonal and stage boundary markers were not found. The Cretaceous/Tertiary boundary is well documented without any major hiatus, and in spite of the poorly recognized zonal boundaries, the Upper Cretaceous sequence is apparently continuous. There are possible correlations between planktonic foraminiferal distribution in Hole 516F and those in Site 356 (Sao Paulo Plateau) and Sites 357 and 21 (Rio Grande Rise).
DOI: 10.15468/cv8hch
title: Familias: STROPHOCHELEIDAE, ODONTOSTOMIDAE

description: Datos de todos los lotes de material seco de las siguientes familias STROPHOCHELEIDAE, , ODONTOSTOMIDAE 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/e3xkj3
title: (Figure 7) Distribution of benthic foraminifers in the Oligocene to upper Miocene DSDP of Hole 71-513A
DOI: 10.15468/k6kjb6
title: Planktic foraminifera abundance of Hole 29-284
DOI: 10.15468/qut6x7
title: Relative abundance of planktonic foraminifera in Pliocene and Pleistocene sediments of DSDP Hole 32-310 from Hess Rise, Central North Pacific (Table II)

description: Late Neogene planktonic foraminifera have been examined at Site 310 in the Central North Pacific and their stratigraphic ranges and frequencies are presented here. Blow's (1969) zonation developed for tropical regions has been applied where applicable. Where tropical index taxa are rare or absent in this temperate region, Globorotalia crassaformis, and the evolutionary bioseries G. conoidea - G. conomiozea and G. puncticulata - G. inflata have been found useful for zonal subdivisions. A correlation between stratigraphic ranges and frequency distributions of these species at Site 310 in the Central North Pacific, and Site 284 in the Southwest Pacific indicates that these species are relatively consistent biostratigraphic markers in temperate regions of both the North and South Pacific Oceans. An informal zonation for temperate latitudes of the Southwest Pacific has been established by Kennett (1973) and a similar zonal subdivision can be made at Site 310. Paleoclimatic/paleoceanographic interpretations based on coiling ratios, percent abundance, and phenotypic variations of Neogloboquadrina pachyderma indicate four major cold events during early, middle, and late Pliocene, and early Pleistocene. Faunal correlations of these events with similar events elsewhere in the Northeast and Southwest Pacific which have been paleomagnetically dated indicate the following approximate ages for these cold events: 4.7 Ma, 3.0 Ma, 2.6-1.8 Ma, and 1.2 Ma. Faunal assemblages have been divided into three groups representing cool, intermediate, and warmer water assemblages. Cool water assemblages are dominated by ~60% N. pachyderma; intermediate temperature faunas are dominated by species of Globigerina and Globigerinita and contain between 20% and 30% N. pachyderma. Warmer water assemblages are dominated by species of Globorotalia and contain &lt;10% N. pachyderma. Frequency oscillations within these groups, in addition to paleotemperature parameters evident in N. pachyderma, afford refined paleoclimatic/paleoceanographic interpretations.
DOI: 10.15468/k5uchr
title: (Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part II
DOI: 10.15468/t7rg53
title: (Table 3) Ostracode distribution in ODP Hole 122-761C
DOI: 10.15468/manhwq
title: (Table 1) Abundance of dead benthic foraminifera in surface sediments of the Arctic Ocean
DOI: 10.15468/sya9s5
title: (Table 4) Ranges of benthic foraminifers from the early Oligocene to the early Miocene in DSDP Hole 22-214
DOI: 10.15468/3f4p4v
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 1995-1999. Part 3
DOI: 10.15468/9u8e5v
title: Occurrence of mammalia relicts at site Sandalja II
DOI: 10.15468/dsbz3a
title: (Figure 2) Distribution of planktonic foraminifers in the Albian of DSDP Hole 71-511
DOI: 10.15468/qnuxug
title: Phytoplankton abundance duringG. O. Sars cruise GS90/6
DOI: 10.15468/rdkhdk
title: Abundance and carbon biomass of phytoplankton at station TT007_8-CTD102
DOI: 10.15468/ubfuhp
title: Microplankton abundance at Station SEPT-1997-GN36199704605MSB01 in the euphotic zone of the Aegean Sea in September 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/wf79gr
title: Pollen analysis of sediment profile BIB00 from Biber See
DOI: 10.15468/mjkn33
title: (Table 7) Distribution of planktonic and selected benthic foraminifers from DSDP Hole 87-583G
DOI: 10.15468/8qffbg
title: Percentages of planktonic foraminifera species in sediment core V25-59
DOI: 10.15468/tbbpzt
title: Microplankton abundance at Station MARCH-1997-GN36199704601MSB06 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/4xamja
title: Content of coarse fraction and G. menardii in sediment corev V25-57
DOI: 10.15468/v3pjtp
title: Analyses of the recent components of sediment core PS1219-1
DOI: 10.15468/b4uzvb
title: Foraminifera abundance of Hole 60-454
DOI: 10.15468/3jekez
title: Planktic foraminifer Globorotalia menardii counts on sediment core GeoB5132-3
DOI: 10.15468/r9yebb
title: Benthic macrofauna abundance in surface sediments of the east Greenland continental slope (75° N section)
DOI: 10.15468/hks8qb
title: Distribution of Quinqueloculina sp. in sediment core 13200-051
DOI: 10.15468/xu69kq
title: (Table 4) Range chart of calcareous nannofossils from Ross Sea sediment cores
DOI: 10.15468/vbjf8r
title: Total foraminifera counts of multinet M10/2_MSN297
DOI: 10.15468/nxe8sn
title: (Table 2) Benthic foraminifera in Pliocene sediments of DSDP Hole 89-586B
DOI: 10.15468/xmh9jc
title: Fossil occurrence of planktonic foraminifera from IODP Hole 315-C0001H
DOI: 10.15468/6jracv
title: Phytoplankton abundance off Guañape bay in Juli 2003, Peru
DOI: 10.15468/xy4fzx
title: Range table from benthic foraminifers in ODP Hole 139-858A
DOI: 10.15468/nd9bdv
title: (Table 1) Benthic foraminifera in late Miocene sediments of DSDP Hole 89-586B
DOI: 10.15468/4exg9x
title: (Table VII) Benthic foraminifera abundance in the Great Belt Channel
DOI: 10.15468/7dtjdj
title: Benthic foraminifera abundance of Hole 42-374
DOI: 10.15468/f26nc8
title: (Table 11) Relative frequencies of planktonic foraminifers and cluster arrangement of ODP Holes 127-794A and 127-197B
DOI: 10.15468/nqfsax
title: Microzooplankton abundance and biomass at station TT045_27-4
DOI: 10.15468/k6fnyx
title: Planktic foraminifera abundance of Hole 19-189
DOI: 10.15468/v4wb43
title: Range table from planktonic foraminifers in ODP Hole 169-1035E
DOI: 10.15468/q2hx2p
title: Pollen profile from sediment core AV14_K2-2
DOI: 10.15468/7rsmqe
title: Ostracoda abundance of Hole 56-435
DOI: 10.15468/k55sks
title: Occurrence of mammalia relicts at site Barrington
DOI: 10.15468/sd5kum
title: Planktic foraminifera abundance of Hole 73-522
DOI: 10.15468/hh7snk
title: Planktic foraminifer Globorotalia menardii counts on sediment core GeoB5117-1
DOI: 10.15468/6g2v3w
title: Size of planktic foraminifera at CTD station PS55/043
DOI: 10.15468/vffkm3
title: Microfossil abundance of Hole 29-278
DOI: 10.15468/6g75uc
title: Foraminifera distribution of sediment core Skyros
DOI: 10.15468/hzr7p3
title: (Table 10) Occurrence of benthic foraminifera in ODP Hole 112-688A
DOI: 10.15468/v7a5m4
title: Planktic foraminifera abundance of Hole 11-102
DOI: 10.15468/nmamem
title: Benthic macrofauna abundance of sediment core 12930-081
DOI: 10.15468/vf6qvw
title: Planktic foraminifera abundance of Hole 16-157
DOI: 10.15468/drjdbm
title: (Table 4) Abundance, preservation, and distribution of calcareous nannofossils in ODP Hole 135-840C
DOI: 10.15468/nu3m9g
title: Nannofossil abundance of Hole 9-77A
DOI: 10.15468/n7ftbg
title: Abundance of benthic infauna in surface sediments from the North Sea sampled during two Michael Sars cruises in 2000
DOI: 10.15468/emmbhq
title: Range table from planktonic foraminifers in ODP Hole 145-884B
DOI: 10.15468/f28yjc
title: Relative abundance of dead benthic foraminifera of sediment core M5/2_88MC
DOI: 10.15468/qxcjba
title: Phytoplankton abundance during Professor Vodyanitskiy cruise PV30_1
DOI: 10.15468/g22b4t
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 174-1071B
DOI: 10.15468/vzyb9z
title: (Figure 7) Stratigraphic ranges of selected planktonic foraminifers at ODP Hole 101-630A
DOI: 10.15468/awzf9g
title: Microzooplankton abundance and biomass at station TT045_4-1
DOI: 10.15468/p7pwb4
title: Planktic foraminifera assemblage in sediment core GIK13289-1
DOI: 10.15468/qvq557
title: (Table 3) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-705A
DOI: 10.15468/sg68cx
title: Nannofossil abundance of Hole 9-80A
DOI: 10.15468/t2t5jj
title: Calcareous dinocysts along profile Ruegen
DOI: 10.15468/67q7xx
title: Nannofossil abundance of Hole 6-49
DOI: 10.15468/47rtkf
title: Distribution of planktonic foraminifera in Oligocene-Miocene of three drill sites from the netherlands Peel area

description: Es ist Ihnen wohl bekaililt, daß bei der Feingliederung des Tertiärs im Tethysraum immer mehr die planktonischen Foraminiferen berücksichtigt werden. Diese Fossilien hatten durch ihre Lebensweise die Möglichkeit einer großen horizontalen Verbreitung und sind deswegen für die Stratigraphie besonders wichtig. Sehr weit ist die Feingliederung des Oligo-Miocän zum Beispiel fortgeschritten in Trinidad, wo neuerdings BOLLI (1957) ein sehr detailliertes Schema aufgestellt hat. Man muß aber für eine allgemeine Verwendung einer solchen Einteilung noch sehr vorsichtig sein.
DOI: 10.15468/76q88m
title: (Table 4) Occurrence of benthic foraminifers in ODP Hole 116-719A
DOI: 10.15468/x83mtk
title: Range table from benthic foraminifers in ODP Hole 172-1055B
DOI: 10.15468/gr6u5q
title: Occurrence of mammalia relicts at site Oblazowa 2
DOI: 10.15468/bmss9q
title: (Table 4) Abundance of Pulleniatina obliquiloculata in sediment core ERDC-112BX
DOI: 10.15468/v3cvbk
title: (Table 4) Relative abundance of selected benthic foraminifera in ODP Hole 104-642D
DOI: 10.15468/pj4vss
title: (Table 2) Vertical distribution of live benthic foraminifera in surface sediments at NEW-Polynya stations
DOI: 10.15468/5rhguq
title: Benthic macrofauna abundance of sediment core 12930-044
DOI: 10.15468/d9rtht
title: (Table 4) Pleistocene nannofossil range chart for ODP Hole 134-827B