cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/3caz43
title: (Figure 6) Stratigraphic ranges of selected planktonic foraminifers at ODP Hole 101-628A
DOI: 10.15468/t8j57w
title: Assemblage of living benthic foraminifera in sediment core CD145_55803#5, &gt;150 µm
DOI: 10.15468/j34m4r
title: Size of planktic foraminifera at CTD station PS55/025
DOI: 10.15468/hyj9mq
title: Palaeoclimate records over the past 22,000 years of sediment core GeoB10053-7
DOI: 10.15468/m4zvve
title: Benthic foraminifera counts of sediment core GIK23063-3
DOI: 10.15468/mktpw7
title: Foraminifera distribution of sediment core TRI171-15
DOI: 10.15468/sxu79t
title: Distribution of planktonic foraminifera of sediment core SH1972_12
DOI: 10.15468/s35at6
title: Nannofossil abundance of Hole 6-50A
DOI: 10.15468/jcadx7
title: Range table from planktonic foraminifers in ODP Hole 171-1049C
DOI: 10.15468/ncxvb8
title: Planktic foraminifera abundance of Hole 9-81
DOI: 10.15468/qnvwds
title: Range table from planktonic foraminifers in ODP Hole 167-1014A
DOI: 10.15468/ya7egu
title: (Table 5) Pleistocene ostracodes from ODP Hole 104-644A
DOI: 10.15468/cub7wq
title: Meiofaunal abundance in sediments obtained during RRS Discovery cruise D297
DOI: 10.15468/rm53fr
title: Microzooplankton abundance and biomass at station TT043_17-1
DOI: 10.15468/uhkxyc
title: Range table from benthic foraminifers in ODP Hole 172-1058A
DOI: 10.15468/45j372
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V29-29
DOI: 10.15468/guq95f
title: Nannofossil abundance of Hole 38-338
DOI: 10.15468/qf932p
title: Planktic foraminifera abundance of Hole 40-360
DOI: 10.15468/35ec2q
title: (Table 2) Abundances of dinoflagellates in ODP Hole 105-646B
DOI: 10.15468/zvwh6w
title: Range table from planktonic foraminifers in ODP Hole 146-889A
DOI: 10.15468/4rh3kn
title: (Table 3) Abundance, preservation, and distribution of calcareous nannofossils in ODP Hole 135-840B
DOI: 10.15468/u5uhfu
title: Living benthic foraminifera at station M33/1_MC-25 (EAST), size fraction &gt;125 µm
DOI: 10.15468/e3rf7x
title: Nannofossil abundance of Hole 7-62
DOI: 10.15468/4x7ky8
title: (Appendix B) Dinoflagellate cysts in Southeast Pacific Ocean surface sediments

description: orty-eight surface sediment samples from the southeast (SE) Pacific (25-53°S) are investigated for the determination of the spatial distribution of organic-walled dinoflagellate cysts along the western South American continental margin. Fifty-five different taxa are recorded and reflect oceanic or coastal assemblages. The oceanic assemblages are characterised by low cyst concentrations and the dominance of autotrophs, while the coastal assemblages generally contain a higher number of cysts, which are mainly produced by heterotrophic species. Highest cyst concentrations are observed in the active upwelling system offshore Concepción (35-37°S). Brigantedinium spp., Echinidinium aculeatum, Echinidinium granulatum/delicatum and cysts of Protoperidinium americanum dominate assemblages related to upwelling. Echinidinium aculeatum appears to be the best indicator for the presence of all year round active upwelling cells. Other protoperidinioid cysts may also occur in high relative abundances in coastal regions outside active upwelling systems, if the availability of nutrients, co-responsible for the presence/absence of their main food sources such as diatoms and other protists, is sufficient. The importance of nutrient availability as a determining environmental variable influencing cyst signals on a regional scale (SE Pacific) is demonstrated through statistical analyses of the data. Because of the importance of nutrients, uncertainties about the outcomes of quantitative sea-surface temperature (SST) reconstructions (Modern Analogue Technique) based on dinoflagellate cysts may arise, since no interaction between different hydrographical variables is considered in this approach. The combination of the SE Pacific surface sample dataset with other published cyst data from the Southern Hemisphere resulted in a database which includes 350 samples: the 'SH350 database'. This database is used to test the accuracy of the quantitative reconstructions by calculating and comparing the estimated versus observed values for each site. An attempt to perform quantitative SST reconstructions on the last 25 cal ka of site ODP1233 (41°S; 74°27'W) is made and again stresses the importance of other environmental variables such as nutrient availability in determining the dinoflagellate cyst assemblages.
DOI: 10.15468/bv8fu7
title: (Table 3) Range chart of calcareous nannofossils from Weddell and Bellingshausen Sea sediment cores
DOI: 10.15468/4gwmh3
title: Planktic foraminifera abundance of Hole 14-140A
DOI: 10.15468/e5wcgc
title: Nannofossil abundance of Hole 10-86
DOI: 10.15468/qsgmbc
title: Analyses of the recent components of sediment core PS1277-1
DOI: 10.15468/a3bmq6
title: (Fig. 5) Distribution of Chironomids of sediment core Lz1103 from Duck Lake
DOI: 10.15468/9h7gxs
title: Foraminifera abundance of Hole 59-451
DOI: 10.15468/b9pde8
title: Results of palynological analysis of Hole 302-M0002A
DOI: 10.15468/d87ycq
title: (Table T1) Benthic foraminifer abundance of ODP Hole 210-1276A sediments

description: Benthic foraminifers were investigated from the western North Atlantic, Ocean Drilling Program (ODP) Site 1276, to document the occurrence of Eocene abyssal benthic foraminifers in this region. Foraminieferal fauna in the middle-upper Eocene consists mainly of agglutinated foraminifers such as Reticulophragmium amplectens, Spiroplectammina spectabilis, Recurvoides spp., and Paratrochamminoides cf. corpulentus with tube-shaped forms. These faunal associations are basically similar to that of ODP Legs 105 (Labrador Sea), 149, and 173 (Iberian margin).
DOI: 10.15468/z2733d
title: Range table from planktonic foraminifers in ODP Hole 145-887A
DOI: 10.15468/2etazq
title: Total foraminifera counts of multinet M21/1_MSN613
DOI: 10.15468/dgfxeg
title: Larval fish at time series station Helgoland Roads, North Sea, in 2003
DOI: 10.15468/dm7vs2
title: Planktic foraminifera abundance of Hole 31-299
DOI: 10.15468/s6dwwk
title: Range table from planktonic foraminifers in ODP Hole 175-1075A
DOI: 10.15468/ty3peu
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 151-907A
DOI: 10.15468/ee6eka
title: Abundance of benthic infauna in surface sediments from the North Sea sampled during Belgica cruise BG86/1
DOI: 10.15468/nqqvhy
title: Plasm bearing foraminifera counts from multinet M31/2_MSN897
DOI: 10.15468/8vtv92
title: Nano and microzooplankton abundance and biomass at station NBP97-01-23-2
DOI: 10.15468/nv5gts
title: Microplankton abundance at Station SEPT-1997-GN36199704606MNB05 in the euphotic zone of the Aegean Sea in September 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/w84xnp
title: (Table 20) Benthic foraminifera in early Miocene sediments of DSDP Hole 90-594
DOI: 10.15468/n5pcav
title: Palynology of a sediment profile from Lake Voulkaria in Greece
DOI: 10.15468/pbqbex
title: Planktic foraminifera counts of sediment core V19-178
DOI: 10.15468/5mjj45
title: Range table from planktonic foraminifers in ODP Hole 182-1134B
DOI: 10.15468/7wzz2v
title: Dinoflagellate cysts counts of sediment core MD95-2042

description: Dinoflagellate cysts were analysed from IMAGES core MD952042 (37°48?N; 10°01?W) retrieved from the Tagus Abyssal Plain. Previous results of stable isotope and magnetic susceptibility measurements as well as of planktonic foraminiferal temperature reconstruction from this core, suggest the occurrence of “Heinrich-like events” (i.e. large ice-sheet decay) during Marine Isotopic Stage 5 (MIS 5). Dinoflagellate assemblages of this time period have revealed six dinocyst events that are characterised by peaks in Bitectatodinium tepikiense percentages. These events occur synchronously with “Heinrich-like events” previously identified. They are coeval with major retreats of the forest on land, indicating, therefore, drastic changes in the regional climate. However, results from the Ice-Rafted Detritus (IRD) analysis of the &gt;150 ?m lithic fraction shows that MIS 5 of MD952042 has only recorded one significant input of iceberg discharge, located at the MIS 6/MIS 5 transition. It seems therefore that it is the only event that could be called a “true Heinrich event”.
DOI: 10.15468/jw8322
title: Nannofossil abundance of Hole 7-64A
DOI: 10.15468/stfvcb
title: Abundance of non-diatom phytoplankton measured on water bottle samples at station PS58/012-5
DOI: 10.15468/6ms4qp
title: Pollen profile from sediment core Fiekers Busch
DOI: 10.15468/qvabfj
title: Range table from planktonic foraminifers in ODP Hole 154-925A
DOI: 10.15468/c4878y
title: Plasm bearing foraminifera counts from M35/1_MSN1046
DOI: 10.15468/n3shdc
title: Plasm bearing foraminifera counts of multinet M36/6_MSN1195
DOI: 10.15468/e9yvq8
title: (Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part III
DOI: 10.15468/rdpeu4
title: Dinoflagellate abundance of Hole 85-572
DOI: 10.15468/3pqgmp
title: Ostracoda in sediment core BP00-07/05
DOI: 10.15468/d88evu
title: Echinoderms in surface sediments off Sylt collected during HEINCKE cruise HE262
DOI: 10.15468/x645tv
title: Absolute abundances of organic-walled dinoflagellate cysts from 116 marine surface samples
DOI: 10.15468/7fw2xp
title: Benthic foraminifera assemblage in sediment core BBLL2_MC4
DOI: 10.15468/r2czf2
title: Planktic foraminifera counts at CTD station PS55/018
DOI: 10.15468/c7hbvw
title: Nannofossil abundance of Hole 1-2
DOI: 10.15468/93garc
title: Planktic foraminifera counts of sediment core V27-60
DOI: 10.15468/24jwqt
title: Plasm bearing foraminifera counts of multinet M42/3_MSN1364
DOI: 10.15468/yg8bjb
title: Abundance of benthos infauna at station GIK23037-3
DOI: 10.15468/73d9y4
title: Coleccion de Invertebrados-Nemato2

description: Material depositado en la Colección de Invertebrados de la Fundación Miguel Lillo
DOI: 10.15468/k6t5dj
title: Phytoplankton abundance in surface water in September 1996, Ilo, Peru
DOI: 10.15468/pm9cku
title: Nannofossil abundance of Hole 47-398B
DOI: 10.15468/batxja
title: Phytoplankton abundance in surface water in March 1997, Ilo, Peru
DOI: 10.15468/8tdhma
title: Distribution of late Turronian planktonic foraminifers in ODP Hole 114-700B

description: The oldest Cretaceous sediments in the subantarctic region were recovered from ODP Hole 700B in the East Georgia Basin. Planktonic foraminifers from the deepest indurated limestones could be attributed to the Marginotruncana schneegansi Zone of late Turonian age.
DOI: 10.15468/j2geak
title: Sarcodine counts and carbon biomass at station TT011_9-CTD115
DOI: 10.15468/6dfs2m
title: Nannofossil abundance of Hole 4-31
DOI: 10.15468/8wfdf9
title: (Table T3) Calcareous nannofossil abundance of ODP Hole 189-1170A sediments
DOI: 10.15468/s86tpm
title: Sarcodine counts and carbon biomass at station TT011_15-CTD168
DOI: 10.15468/44k3k7
title: (Table 12) Distribution of planktonic foraminifers in ODP Hole 108-664D
DOI: 10.15468/srt64z
title: Analyses of the recent components in the sand fraction of sediment core PS1016-1
DOI: 10.15468/8queua
title: Range table from benthic foraminifers in ODP Hole 192-1184A
DOI: 10.15468/h3kztz
title: Distribution of foraminifera, pre-Pliocene foraminifera and macrofossil debris in sediment core CRP-2 (Table 1)

description: The stratigraphic distribution, assemblage content, paleoecology and age of foraminifera recovered in fourteen of sixteen samples from the 5.63 m thick CRP-2 (Lithostratigraphic Unit 2.2) are discussed. LSU 2.2 comprises four discrete lithologic beds. The upward sequence is informally referred to as the lower sand bed, diamicton bed, middle sand bed, and upper sand bed and it is surmised that these four units are closely related in time. The lower sand bed (~1.5m), which overlies lower Miocene sediments and from which it is separated by the Ross Sea Unconformity, contains traces of recycled Miocene diatoms but is otherwise barren of biogenic material. The diamicton bed (~2.42 m) contains 21 species of benthic foraminifera, with assemblages consistently dominated by Cassidulinoides porrectus, Ammoelphidiella antarctica, Rosalina cf. globularis, Cibicides refulgens, and Ehrenbergina glabra. The overlying middle sand bed (~1.9 m) contains 13 species. with C. porrectus and E. glabra dominant and A. antarctica less common than in the underlying diamicton bed. The upper sand bed (~0.46 m) contains four species and very few tests. The diamicton bed and middle sand bed assemblages are considered to be near in situ thanatocoenoses; and sediments interpreted as marine in origin but influenced by hyposaline waters and nearby ice. Planktic taxa are absent, perhaps indicating the presence of tidewater glaciers, sea ice and/or hyposaline surface waters. The small assemblage in the upper sand bed is more problematic and may be recycled. On the basis of foraminifera in the diamicton and middle sand beds. LSU 2.2 is assigned to the Pliocene. The overlying diamicton in LSU 2.1 contains abundant Quaternary foraminifera.
DOI: 10.15468/p98psk
title: Plasm bearing foraminifera counts from multinet M31/2_MSN888
DOI: 10.15468/szcmnz
title: Phytoplankton abundance measured on water bottle samples at station PS65/593-3
DOI: 10.15468/3tuh9p
title: Foraminifera abundance of Hole 60-459B
DOI: 10.15468/7b4nmg
title: (Figure 3) Distribution of planktonic foraminifers in the Cenozoic sediments of DSDP Hole 71-511
DOI: 10.15468/gsushd
title: Nannofossil abundance of Hole 11-103
DOI: 10.15468/eydmv2
title: Benthic foraminifera abundance of Hole 84-566
DOI: 10.15468/fuhv9k
title: (Table 3) Distribution of benthic foraminifers in middle Miocene sediments of ODP Hole 182-1134A in the Great Australian Bight
DOI: 10.15468/uaqu8a
title: Foraminifera abundance of Hole 48-406
DOI: 10.15468/84f97m
title: Planktonic and benthic foraminiferal stable isotopes, SSTs and thermocline temperature, coccoliths and benthic foraminiferal assemblages, and productivity reconstruction for sediment core MD06-3067

description: We present sea surface, upper thermocline, and benthic d18O data, as well as temperature and paleoproductivity proxy data, from the International Marine Global Change Study Program (IMAGES) Core MD06-3067 (6°31'N, 126°30'E, 1575 m water depth), located in the western equatorial Pacific Ocean within the flow path of the Mindanao Current. Our records reveal considerable glacial-interglacial and suborbital variability in the Mindanao Dome upwelling over the last 160 kyr. Dome activity generally intensified during glacial intervals resulting in cooler thermocline waters, whereas it substantially declined during interglacials, in particular in the early Holocene and early marine oxygen isotope stage (MIS) 5e, when upwelling waters did not reach the thermocline. During MIS 3 and MIS 2, enhanced surface productivity together with remarkably low SST and low upper ocean thermal contrast provide evidence for episodic glacial upwelling to the surface, whereas transient surface warming marks periodic collapses of the Mindanao Dome upwelling during Heinrich events. We attribute the high variability during MIS 3 and MIS 2 to changes in the El Niño Southern Oscillation state that affected boreal winter monsoonal winds and upper ocean circulation. Glacial upwelling intensified when a strong cyclonic gyre became established, whereas El Niño–like conditions during Heinrich events tended to suppress the cyclonic circulation, reducing Ekman transport. Thus, our findings demonstrate that variations in the Mindanao Dome upwelling are closely linked to the position and intensity of the tropical convection and also reflect far-field influences from the high latitudes.
DOI: 10.15468/d4kxxj
title: Assemblage of living benthic foraminifera in sediment core GeoB4904-7
DOI: 10.15468/x8gcuk
title: Range table from benthic foraminifers in ODP Hole 175-1075A
DOI: 10.15468/aumk2u
title: Nannofossil abundance of Hole 8-71
DOI: 10.15468/pqtkmj
title: Analyses of the recent components of sediment core PS1223-1
DOI: 10.15468/72dsqj
title: Abundance of planktic foraminifera at CTD station PS55/079-1
DOI: 10.15468/cceb9r
title: Benthic foraminiferal assemblage (dead) in MUC SC1-K, size fraction &gt;150 µm
DOI: 10.15468/2nkgbx
title: Planktic foraminifera counts of sediment core V22-188
DOI: 10.15468/4q4y34
title: (Table 2) Distribution of ice-rafted fossils in ODP Hole 104-643A
DOI: 10.15468/786rd2
title: Percentages of planktonic foraminifera species in sediment core RC13-189
DOI: 10.15468/gjmbsz
title: Occurrence of mammalia relicts at site Schweizerbild
DOI: 10.15468/szyjkm
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB05 in the euphotic zone of the Aegean Sea in spring 1997. Part 2 - dinoflagellates
DOI: 10.15468/2eb375
title: Occurrence of mammalia relicts at site Trou Jadot
DOI: 10.15468/azpmz7
title: Benthic foraminiferal abundances at the Cretaceous/Paleogene boundary of ODP Hole 117-1049C at Blake Nose, Northwest Atlantic (Appendix A)

description: Sediments recovered at lower bathyal ODP Site 1049 on Blake Nose (Northwestern Atlantic) offer an opportunity to study environmental changes at the Cretaceous/Paleogene (K/P) boundary relatively close to the Chicxulub impact structure on the Yucatan peninsula, Mexico. In Hole 1049C, the boundary is located at the base of a 9-cm-thick layer with abundant spherules, considered to be impact ejecta. Uppermost Maastrichtian oozes below, and lowermost Danian pelagic oozes above the spherulebed contain well-preserved bathyal benthic foraminifera. The spherule-bed itself, in contrast, contains a mixture of shallow (neritic) and deeper (bathyal) species, and specimens vary strongly in preservation. This assemblage was probably formed by reworking and down-slope transport triggered by the K/P impact. Across the spherule-bed (i.e., the K/P boundary) only ~7% of benthic foraminiferal species became extinct, similar to the low extinction rates of benthic foraminifera worldwide. Quantitative analysis of benthic foraminiferal assemblages and morphogroups in the &gt;63-µm size fraction indicates a relatively eutrophic, stable environment during the latest Maastrichtian, interrupted by a sudden decrease in the food supply to the benthos at the K/P boundary and a decrease in diversity of the faunas, followed by a stepped recovery during the earliest Danian. The recovery was probably linked to the gradual recovery of surface-dwelling primary producers.
DOI: 10.15468/yhxzx3
title: (Tab. 13) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 32-306, Shatsky Rise southeast of Japan
DOI: 10.15468/gh627c
title: Occurrence of mammalia relicts at site Bärenfelsgrotte
DOI: 10.15468/upagkd
title: Dinoflagellate cysts from the Upper Hauterivian (Cretaceous) of a claystone-marlstone succession in the clay-pit Frielingen
DOI: 10.15468/xq27hx
title: Plasm bearing foraminifera counts from M35/1_MSN1050
DOI: 10.15468/7deg56
title: Phytoplankton abundance at station Sechin_2003-09-18_2, Casma, Peru
DOI: 10.15468/dsujx9
title: (Appendix A5) Relative abundances of planktonic foraminifera of sediment core GeoB1711-5
DOI: 10.15468/87a8vd
title: Size of planktic foraminifera at CTD station M39/4_404CTD-57
DOI: 10.22002/rxsqk-8zb05
title: Data for "Enabling Al sacrificial anodes in tetrahydrofuran electrolytes for reductive electrosynthesis"
DOI: 10.15468/cyaxeg
title: Abundance of dinoflagellates and ciliates at time series station Helgoland Roads, North Sea, in 2007
DOI: 10.5519/qd.1g9l5adl
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (16 records)
DOI: 10.15468/dfehqt
title: (Table 4) Relative abundances of stratigraphically useful planktonic foraminifers from ODP Site 167-1013 sediments
DOI: 10.15468/hk4b2x
title: (Table 12) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-688A
DOI: 10.15468/9x68y4
title: Occurence of foraminifera and other microfossils in sediment core CRP-2/2A (Table 1)

description: Sparse to moderately abundant foraminiferal assemblages from Oligocene and Lower Miocene sediments in the CRP-2/2A drillhole contain C.27 genera and 42 species of calcareous benthic foraminifera. No planktic or agglutinated taxa were observed. On the basis of their faunal characteristics, four Foraminiferal Units are defined in drillhole succession: Foraminiferal Unit I (26.91-193.95 mbsf), mostly sparse assemblages with Elphidium magellanicum and Cribroelphidium sp.; Foraminiferal Unit II (193.95-342.42 mbsf), mostly moderately abundant assemblages with Cassidulinoides aequilatera and Eponides bradyi; Foraminiferal Unit III (342.42-486.19 mbsf), moderately abundant to sparse assemblages characterised by Cassidulinoides chapmani and Stainforthia sp.; and Foraminiferal Unit IV, Improverished (486.19-624.15, total depth, mbsf), with mostly barren residues, but with large Milioliidae recorded in situ at various horizons in the drill core. Foraminiferal Units I-IV lack taxa allowing correlation to standard zonal schemes. Inspection of faunal records from CIROS-1 and DSDP 270 indicates that, although the faunas show an overall similarity, CRP-2/2A Foraminiferal Units I-IV are not identifiable at these sites. The units are therefore most likely to reflect local environmental changes, and probably will prove useful for local correlation, but their lateral extent is undetermined. All four assemblages apparently represent various glacially-influenced shelf environments, and appear to reflect a long term deepening trend from Units IV to II, from perhaps inner to mid or outer-shelf depths, followed by a return to shallower, inner shelf, conditios for Unit I.
DOI: 10.15468/t2awka
title: Stable isotopes, diversity and composition of foraminifera in sediment core GeoB3004-1
DOI: 10.15468/uqatxs
title: Ratios of juvenile to total ostracode fauna in surface sediment samples from the Persian Gulf (Table 1b)
DOI: 10.15468/zfjbfw
title: Total foraminifera counts of multinet M21/2_MSN639
DOI: 10.15468/63x9f9
title: (Appendix A1) Abundances of planktonic and benthic foraminifera in the Turonian to Coniacian sediments of ODP Site 207-1259
DOI: 10.15468/zfx989
title: Distribution of planktonic foraminifera of site GeoB1105
DOI: 10.15468/h32zgh
title: Total foraminifera counts of multinet M11/1_MSN526
DOI: 10.15468/haeusx
title: Phytoplankton abundance in surface water in June 1997, Pisco, Peru
DOI: 10.15468/3b8zpy
title: Range table from planktonic foraminifers in ODP Hole 145-883B
DOI: 10.15468/f3wkem
title: Total foraminifera counts of multinet POS247/2_MSN1374
DOI: 10.15468/79gdkv
title: (Table T8) Planktonic foraminifera stratigraphy of ODP Hole 198-1210A, Zone P4
DOI: 10.15468/ev3rqq
title: Benthic macrofauna abundance of subcores of sediment core 13200-045
DOI: 10.15468/w7vk93
title: Distribution of planktic foraminifers of core RC13-110
DOI: 10.15468/wa5ty7
title: (Table 4) Distribution of foraminifera in the Miocene section of ODP Hole 133-816C
DOI: 10.15468/kh95ej
title: Planktic foraminifera abundance of Hole 19-190
DOI: 10.15468/w2wcng
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1377
DOI: 10.15468/3qhyw8
title: (Table 8) Benthic foraminifera genera assemblage at DSDP Section 80-548A-28
DOI: 10.15468/cw98ep
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC13-205
DOI: 10.15468/2v79ff
title: (Figure 6) Range chart of planktonic foraminifers across the K/T boundary at ODP Hole 120-750A
DOI: 10.15468/udhq3r
title: Nannofossil abundance of Hole 60-455
DOI: 10.15468/h2t9zw
title: Size of planktic foraminifera at CTD station M39/4_381CTD-34