cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/6dm89f
title: (Table 10) Eocene-Oligocene diatom biostratigraphy of ODP Hole 120-748B
DOI: 10.15468/tfse6g
title: Distribution of Quinqueloculina sp. in sediment core 13077-023
DOI: 10.15468/5xm9wt
title: Sarcodine counts and carbon biomass at station TT011_6-CTD71
DOI: 10.15468/m77wcz
title: Phytoplankton abundance in surface water in June 1997, Callao, Peru
DOI: 10.15468/wtk8rq
title: Benthic macrofauna abundance of subcores of sediment core 13078-015
DOI: 10.15468/xrmr64
title: (Appendix F) Stratigraphic range and relative abundance of Paleogene planktonic foraminifera in ODP Hole 120-749C
DOI: 10.15468/4e6m2z
title: Planktic foraminifer Globorotalia menardii counts on sediment core GeoB5120-2
DOI: 10.15468/d8ghed
title: Microzooplankton abundance and biomass at station NBP97-03-12-2
DOI: 10.15468/7wzhxw
title: (Table 2) Distribution of selected planktonic foraminifer species at ODP Site 124-770
DOI: 10.15468/qsxr6u
title: (Table 7) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-709C
DOI: 10.15468/d3jyec
title: Planktic foraminifera abundance of Hole 94-611B
DOI: 10.15468/j7k5hs
title: Relative abundance of planktic foraminifera in sediment core GeoB1312-2
DOI: 10.15468/shbf7m
title: Nannofossil abundance of Hole 30-286
DOI: 10.15468/3kjh5k
title: Nannofossil abundance of Hole 7-63
DOI: 10.15468/3jqfst
title: Planktic foraminifera abundance of Hole 62-465
DOI: 10.15468/df6src
title: Planktic foraminifer Globorotalia menardii counts on sediment core GeoB5112-4
DOI: 10.15468/ytqrtn
title: (Table 2e) Nannofossil distribution chart of petroleum well Leeuwin-1
DOI: 10.15468/kfk3s5
title: Planktic foraminifera counts of sediment core RC14-7
DOI: 10.15468/ptx43g
title: Relative abundance of benthic foraminifera in sediment core M5/2_KL15
DOI: 10.15468/hhsphg
title: Distribution of Quinqueloculina sp. in sediment core 12930-065
DOI: 10.15468/yf84km
title: Planktic foraminifera abundance of Hole 19-184B
DOI: 10.15468/3pa9sr
title: (Appendix A) Abundances of planktonic foraminifera in mid-Pleistocene sediments of ODP Site 184-1144 in the South China Sea
DOI: 10.15468/4gk8f9
title: Dead benthic foraminifera from surface sediments of the Indian and Pakistan continental margin (Table 1)
DOI: 10.15468/6m64rx
title: (Table 3) Planktonic foraminifer abundance of ODP Hole 162-980A
DOI: 10.15468/2unhmv
title: (Table 1) Bottom fauna Metazoa in grab samples from the Namibia shelf in the area of Benguela upwelling
DOI: 10.15468/b3tcg8
title: Total living benthic foraminifera at station M33/1_MC-25 (EAST), size fraction &gt;30 µm
DOI: 10.15468/hf8s23
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 1984-1991. Part 3
DOI: 10.15468/ex8yc9
title: Benthic foraminifera abundance of Hole 56-435
DOI: 10.15468/warxzy
title: (Table 2) Distribution of silicoflagellates, actiniscidians, and ebridians in selected samples from ODP Hole 112-683A
DOI: 10.15468/k8ddbs
title: Range table from planktonic foraminifers in ODP Hole 169-1038H
DOI: 10.15468/g82bgs
title: Microzooplankton abundance measured on water bottle samples at station PS58/038-3
DOI: 10.15468/92s82q
title: (Figure 2) Distribution of dinoflagellate cysts in the mid-Cretaceous of ODP Hole 101-627B
DOI: 10.15468/7qm8qc
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 1995-1999. Part 1
DOI: 10.15468/a4ujgn
title: Benthic foraminifera abundance of Hole 42-381
DOI: 10.15468/vsvzeu
title: Nannofossil abundance of Hole 29-280
DOI: 10.15468/tgsuna
title: Distribution of hydropolyp species in surface sediments of the Red Sea (Table 5)
DOI: 10.15468/w42652
title: (Table 6) Relative abundances of stratigraphically useful planktonic foraminifers from ODP Hole 167-1018A sediments
DOI: 10.15468/vpx9s6
title: Occurrence of mammalia relicts at site Roc de Combe
DOI: 10.15468/bkdxhh
title: (Table 4) Distribution of planktonic foraminifera in middle Miocene sediments of DSDP Hole 94-608 in the North Atlantic
DOI: 10.15468/wptypm
title: Plasm bearing foraminifera counts of multinet M42/3_MSN1362
DOI: 10.15468/6x2cct
title: Sarcodine counts and carbon biomass at station TT012_5-TM28
DOI: 10.15468/me6st2
title: (Table 2) Range chart of benthic and planktonic foraminifera of ODP Site 127-794
DOI: 10.15468/b59an3
title: (Tab. 10) Distribution of benthic foraminifera in Lower Cretaceous sediments of DSDP Hole 32-303A, Japanese Magnetic Lineations east of Japan
DOI: 10.15468/d3uubf
title: Abundance of living benthic foraminifera in sediment core CD86_09_BC1
DOI: 10.15468/mywekb
title: Coccolith counts of multinet SO119_MSN1301
DOI: 10.15468/nbeary
title: Microzooplankton (larger protists and small copepods) abundance measured on concentrated water bottle samples at station PS65/511-12
DOI: 10.15468/cpkgyu
title: Planktic foraminifera abundance of Hole 32-313
DOI: 10.15468/daxp2s
title: Occurrence of mammalia relicts at site Sainte-Eulalie
DOI: 10.15468/u8wbf8
title: Benthic foraminifera counts of sediment core GIK23342-6
DOI: 10.15468/2srqvx
title: Plasm bearing foraminifera counts of multinet M21/1_MSN607
DOI: 10.15468/tycjms
title: Microplankton counts and carbon biomass at station TT008_5-CTD61
DOI: 10.15468/b3k96k
title: Pollen profile 1 from Richland Creek
DOI: 10.15468/gjkafz
title: Planktic foraminifera counts of sediment core RC17-69
DOI: 10.15468/abnfb6
title: Range table from benthic foraminifers in ODP Hole 171-1052A
DOI: 10.15468/pufpbe
title: (Table 4) Distribution of planktonic foraminifers in ODP Site 126-792
DOI: 10.15468/ygkyaw
title: Nannofossil abundance of Hole 51-417B
DOI: 10.15468/zr2q3w
title: (Table 3) Occurrence of dinoflagellate cyst species in ODP Hole 113-696B
DOI: 10.15468/3qqzyv
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1372
DOI: 10.15468/x95ebv
title: Abundance of benthic foraminiferal taxa for the Lower Oligocene of section Poetschbichl in the Lower Inn Valley area
DOI: 10.15468/c3qpem
title: Phytoplankton abundance at station Casma_2003-01-30_1, Casma, Peru
DOI: 10.15468/c2bjw9
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 189-1170D
DOI: 10.15468/2tez6n
title: (Table 6) Relative abundance of dead foraminifers in surface sediment
DOI: 10.15468/gavszs
title: Biological data measured on water bottle sampels at station AT_II-119/5_35-4
DOI: 10.15468/cvgvn6
title: Occurrence of mammalia relicts at site Fohlenhaus-Höhlen
DOI: 10.15468/x9cgac
title: Nannofossil abundance of Hole 2-8A
DOI: 10.15468/zxxws7
title: Benthic foraminifera counts of sediment core PS1246-4 (GIK23246-4)
DOI: 10.15468/jchp5d
title: Range table from planktonic foraminifers in ODP Hole 143-865A
DOI: 10.15468/kgcgbm
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-04-4
DOI: 10.15468/beegtn
title: Ostracoda in sediment core PS51/135-4
DOI: 10.15468/kc9qmh
title: Microfossil abundance of Hole 29-277
DOI: 10.15468/9vjkux
title: Ostracode relative abundances and geochemistry in surface sediments from Lake Ohrid

description: Understanding the ecology of bioindicators such as ostracods is essential in order to reconstruct past environmental and climate change from analysis of fossil assemblages preserved in lake sediment cores. Knowledge of the ecology of ancient Lake Ohrid's ostracod fauna is very limited and open to debate. In advance of the Ohrid ICDP-Drilling project, which has potential to generate high-resolution long-term paleoenvironmental data of global importance in paleoclimate research, we sampled Lake Ohrid and a wide range of habitat types in its surroundings to assess 1) the composition of ostracod assemblages in lakes, springs, streams, and short-lived seasonal water bodies, 2) the geographical distribution of ostracods, and 3) the ecological characteristics of individual ostracod species. In total, 40 species were collected alive, and seven species were preserved as valves and empty carapaces. Of the 40 ostracod species, twelve were endemic to Lake Ohrid. The most common genus in the lake was Candona, represented by 13 living species, followed by Paralimnocythere, represented by five living species. The most frequent species was Cypria obliqua. Species with distinct distributions included Heterocypris incongruens, Candonopsis kingsleii, and Cypria lacustris. The most common species in shallow, flooded areas was H. incongruens, and the most prominent species in ditches was C. kingsleii. C. lacustris was widely distributed in channels, springs, lakes, and rivers. Statistical analyses were performed on a “Lake Ohrid” dataset, comprising the subset of samples from Lake Ohrid alone, and an “entire” dataset comprising all samples collected. The unweighted pair group mean average (UPGMA) clustering was mainly controlled by species-specific depth preferences. Canonical Correspondence Analysis (CCA) with forward selection identified water depth, water temperature, and pH as variables that best explained the ostracod distribution in Lake Ohrid. The lack of significance of conductivity and dissolved oxygen in CCA of Ohrid data highlight the uniformity across the lake of the well-mixed waters. In the entire area, CCA revealed that ostracod distribution was best explained by water depth, salinity, conductivity, pH, and dissolved oxygen. Salinity was probably selected by CCA due to the presence of Eucypris virens and Bradleystrandesia reticulata in short-lived seasonal water bodies. Water depth is an important, although indirect, influence on ostracod species distribution which is probably associated with other factors such as sediment texture and food supply. Some species appeared to be indicators for multiple environmental variables, such as lake level and water temperature.
DOI: 10.15468/tscf6g
title: Tab. 5: Artenzusammensetzung, mittlere Individuendichte, Diversität und Eveness der benthischen Gemeinschaft
DOI: 10.15468/yp2yan
title: Phytoplankton abundance in surface water in September 1997, Ilo, Peru
DOI: 10.15468/3hyrn2
title: (Table 5) Abundance, preservation, and distribution of calcareous nannofossils in ODP Hole 135-841A
DOI: 10.15468/yrf5ed
title: Microplankton abundance in the euphotic zone of the Aegean Sea at Station JUNE-94-GN3619940280200320
DOI: 10.15468/82a2pt
title: Occurrence of mammalia relicts at site Trebacki krs
DOI: 10.15468/npjhqb
title: (Table 1) Biometrics and lipid content of polar bear (Ursus maritimus) adipose tissue between 1991-2007
DOI: 10.15468/y32nch
title: Benthic macrofauna abundance of sediment core 13200-047
DOI: 10.15468/qgxdum
title: Planktic foraminifera abundance of Hole 28-265
DOI: 10.15468/7hxyw6
title: Phytoplankton abundance during G. M. Dannevig cruise GMD90/12
DOI: 10.15468/esm22q
title: Microzooplankton (larger protists and small copepods) abundance measured on concentrated water bottle samples at station PS65/544-6
DOI: 10.15468/6v6r2g
title: (Table 3) Distribution of planktonic foraminifers in ODP Hole 112-682A
DOI: 10.15468/62b9u8
title: Matter enrichment of the macrofauna community of MAC station 12930-005
DOI: 10.15468/98rsbg
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/038-3
DOI: 10.15468/prfeq6
title: Abundance of epibenthic echinoderms at seafloor photography station POS196_1017
DOI: 10.15468/fvrkmc
title: (Table 2) Occurrence of larger benthic foraminifers in ODP Hole 133-823C
DOI: 10.15468/whwdjh
title: Distribution of microorganisms in recent sediments of Kiel Bay

description: Die angewandte Mikropaläontologie bestimmt heute im wesentlichen das Alter eines Gesteins mit Hilfe von Faunenvergesellschaftungen. Aus der Zusammensetzung der Fauna, aus dem Einsatz oder Fehlen bestimmter Gattungen und Arten, aus den Mineralien, die das Gestein aufbauen, aus dem ganzen Bild, das eine aus einem Gestein herausgeschlämmte Fauna dem Bearbeiter gibt, läßt sich das Alter dieses Gesteins festlegen. Will man aber verschiedene Bohrungen, vor allem auch räumlich weit voneinander getrennter Gebiete, miteinander parallelisieren, so liegt das Kernproblem der Mikropaläontologie in der Frage, ob es sich bei verschiedenen Faunen tatsächlich um Alters- oder nur um Faziesunterschiede handelt. Da die Grundlagen der mikropaläontologischen Arbeitsweise zum weitaus größten Teil auf den Ergebnissen von Untersuchungen fossiler Faunen beruhen, müssen zu ihrer Unterbauung Untersuchungen an recentem Material folgen. Besonders spielt das Ineinandergreifen mariner und brackischer Sedimente in der angewandten Mikropaläontologie eine große Rolle. Auf Grund der Tatsache, daß ein großer Teil von Gattungen und Arten der Foraminiferen an der Wende Kreide/Tertiär ausstirbt und neue an ihre Stelle treten, stellt Glässner (1948) die Behauptung auf, daß die aktualistisch gewonnenen Ergebnisse für vortertiäre Faunen nur eine geringe Bedeutung besitzen. Auch seien vortertiäre, brackische Foraminiferen nicht bekannt (Glässner 1948, S. 191). Hiltermann (1948) konnte aber bereits im nordwestdeutschen Malm brackische, d. h. in Brackwasser eindringende Foraminiferen nachweisen. Auf jeden Fall behalten aktualistische Unterlagen ihren Wert für das Tertiär und Quartär. Die Faunen, die in recenten, brackischen Sedimenten nebeneinander auftreten, sind in einem Bohrprofil in einem Gestein übereinander zu erwarten. Gelingt es, die Beziehungen einer recenten Fauna zu ihrer Umwelt zu klären, dann können umgekehrt aus fossilen, ihnen gleichen oder ähnlichen Faunen Rückschlüsse auf die Entstehungsbedingungen von Gesteinen gezogen werden. Unter Umständen können der Verlauf einer Transgression, Küstennähe, die Höhe des Salzgehaltes des Meerwassers, die vorherrschenden Temperaturen u. a., aus ihnen abgelesen werden. Die Ostsee ist ein klassisches Brackwassergebiet der Erde. Ihr westlicher Teil, die Kieler Bucht, wurde erst in jüngster geologischer Zeit vom Meer überflutet. Nach Tapfer (1940) begann hier die flandrische Transgression erst etwa um 7500 v. d. Zw. mit dem Erreichen des heutigen Meeresniveaus. Seit dieser Zeit erst entstehen neue Küstenformen, wird der Meeresboden umgelagert und bilden sich marine und brackische Absätze in diesem Gebiet.
DOI: 10.15468/xj95b7
title: Nannofossil abundance of Hole 2-11A
DOI: 10.15468/zcjby9
title: (Table T1) Distribution of selected calcareous nannofossils at the Paleocene/Eocene boundary, ODP Hole 208-1266C

description: Ocean Drilling Program Leg 208 Hole 1266C (28°32.55'S, 2°20.61'E) is located along the northwestern flank of Walvis Ridge (South Atlantic Ocean). The location of Site 1266, at 3.798 km water depth, corresponds to a mid-depth site of the Leg 208 transect. A stratigraphically continuous and expanded sequence of upper Paleocene and lower Eocene pelagic nannofossil ooze was recovered. Three holes were cored at Site 1266, and from Hole 1266C, an expanded and continuous Paleocene/Eocene (P/E) transition was recovered using the advanced piston corer system. The successful recovery and well-preserved nannofossil assemblages make Hole 1266C a reference section for improving the knowledge of the Paleocene/Eocene Thermal Maximum. The P/E transition is one of the most remarkable and intensively investigated time intervals. Significant and dramatic changes in climate and oceanography occurred at this transition. The P/E boundary is linked with an important turnover in benthic foraminifers and planktonic marine communities (Thomas and Shackleton, 1996, doi:10.1144/GSL.SP.1996.101.01.20; Kelly et al., 1998, doi:10.1016/S0031-0182(98)00017-0; Monechi et al., 2000, doi:10.2113/171.4.477; Bralower, 2002, doi:10.1029/2001PA000662). This report documents the calcareous nannofossil assemblage fluctuations at the P/E boundary in Hole 1266C based on semiquantitative and quantitative investigations.
DOI: 10.15468/hwsq2s
title: Range table from planktonic foraminifers in ODP Hole 175-1080A
DOI: 10.15468/b34k4s
title: (Table 4a) Range chart of benthic and planktonic foraminifera of ODP Hole 127-796A
DOI: 10.15468/uwweb7
title: Planktic foraminifera abundance of Hole 32-313
DOI: 10.15468/2ns3hz
title: (Table 3) Distribution of calcareous nannofossils from selected samples of ODP Hole 107-653A
DOI: 10.15468/sszqaf
title: (Table T1) Biogenic and mineral composition of sediments cored in Ratekau, Schleswig-Holstein
DOI: 10.15468/9dv2hh
title: Abundance of nematoda in sediment profile M3/1_021 from the Iberian deep sea basin (Table 5)
DOI: 10.15468/az5cna
title: Diatom abundance measured on water bottle samples at station PS58/090-4
DOI: 10.15468/fef432
title: Range table from planktonic foraminifers in ODP Hole 171-1050B
DOI: 10.15468/sad4jt
title: Distribution of Quinqueloculina sp. in sediment core 13077-059
DOI: 10.15468/9m9n67
title: Total foraminifera counts of multinet M21/5_MSN732
DOI: 10.15468/89gvdm
title: Microzooplankton abundance measured on water bottle samples at station PS58/046-3
DOI: 10.15468/wej2pm
title: (Table T10) Planktonic foraminifera stratigraphy of ODP Hole 198-1210A, Zones P8-P10
DOI: 10.15468/urr36u
title: Relative abundance of planktic foraminifera in sediment core TR126-23 from the 120 kyr time slice reconstruction
DOI: 10.15468/38zdtp
title: Planktic foraminifera abundance of Hole 67-500
DOI: 10.15468/szpuvz
title: Planktic foraminifera abundance of Hole 11-106B
DOI: 10.15468/7r3bw8
title: (Appendix B2) Distribution of planktic foraminifera in ODP Hole 181-1125A east of New Zealand
DOI: 10.15468/6du85z
title: Distribution of Quinqueloculina sp. in sediment core 13078-017
DOI: 10.15468/buc7t2
title: Nannofossil abundance of Hole 67-495
DOI: 10.15468/4sb23a
title: Nannofossil abundance of Hole 26-258
DOI: 10.15468/6rdjrp
title: Distribution of meiobenthos in sediment core M19_193-2 of the northeastern Atlantic (Table 1)
DOI: 10.15468/hyamy5
title: Benthic foraminiferal assemblage (Rose Bengal stained) in MUC OB10-K, size fraction 63-150 µm
DOI: 10.15468/5rzntc
title: (Table 7) Relative abundance of benthic foraminifera in ODP Site 112-683
DOI: 10.15468/z8hdgh
title: Range table from benthic foraminifers in ODP Hole 182-1130A
DOI: 10.15468/b29n48
title: Total foraminifera counts of multinet M21/4_MSN707
DOI: 10.15468/3jqnsw
title: Total foraminifera counts of multinet M42/3_MSN1360
DOI: 10.15468/ymksey
title: Foraminifera abundance of Hole 22-215
DOI: 10.15468/57n2bj
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/041-5
DOI: 10.15468/my35ex
title: Foraminifera abundance of sediment core IN68-21
DOI: 10.15468/z27jhz
title: Abundance of dead benthic foraminifera in sediment core CD86_07_BC4
DOI: 10.15468/b7vy7q
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 2005-2006. Part 2
DOI: 10.15468/ewxca4
title: Planktic foraminifera abundance of Hole 26-250
DOI: 10.15468/mb5rga
title: Dinoflagellate abundance in sediment core JM06-WP-04-MCB
DOI: 10.15468/b5md9x
title: (Table 15C) Occurrences of planktonic foraminifers in Hole 90-593A
DOI: 10.15468/dyzfkr
title: Smear slide analysis on sediment core GeoB4223-2
DOI: 10.15468/q67mny
title: (Table T16) Planktonic foraminifera stratigraphy of ODP Hole 198-1211A, Zones P9-P12
DOI: 10.15468/4c2nfh
title: Planktic foraminifera abundance of Hole 14-136
DOI: 10.15468/rej2y3
title: Total foraminifera counts of multinet M21/4_MSN697
DOI: 10.15468/2ph2ps
title: Plasm bearing foraminifera counts of multinet M12/3_MSN559
DOI: 10.15468/7nynd9
title: Crustacea in surface sediments off Sylt collected during HEINCKE cruise HE278
DOI: 10.15468/7qr3vt
title: Distribution of Quinqueloculina sp. in sediment core 13200-039
DOI: 10.15468/vn8swk
title: Nannofossil abundance of Hole 67-497
DOI: 10.15468/gatrna
title: Content of coarse fraction and G. menardii in sediment corev V26-101
DOI: 10.15468/mg4kww
title: Benthic macrofauna abundance of sediment core 13200-075
DOI: 10.15468/j3czbg
title: Microplankton counts and carbon biomass at station TT011_5-CTD64
DOI: 10.15468/nmtwkv
title: Absolute abundance of dead benthic foraminifera of sediment core M5/2_91MC
DOI: 10.15468/r6qhme
title: Benthic foraminifers of sediment core Svanic90_9004
DOI: 10.15468/y2af6h
title: (Table 8) Sample mass, sand fraction and relative abundances of planktonic foraminifera in ODP Holes 127-794A and 127-197B
DOI: 10.15468/ywc77n
title: Planktic foraminifera counts during POLARSTERN cruise ARK-XIII/2
DOI: 10.15468/9cxjvb
title: Total foraminifera counts of multinet M26/1_MSN843
DOI: 10.15468/mdcasz
title: (Tab. 4) Occurence of microfossils in Late Jurassic sediments of DSDP Hole 11-105, Bahama Lower Continental Rise Hill
DOI: 10.15468/r6zats
title: (Table 3) Quantitative parameters of the Emiliania huxleyi population along the section from the Pribilofs Islands to the Nunivak Island carried out on 24 and 25 August 2001
DOI: 10.15468/yr6dqx
title: (Table T9) Planktonic foraminifera stratigraphy of ODP Hole 198-1210A, Zones P5-P7
DOI: 10.15468/j24xtv
title: Pollen profile from Pittsburg Basin
DOI: 10.15468/dwy9cp
title: Range table from benthic foraminifers in ODP Hole 139-858B
DOI: 10.15468/9tyneh
title: Microzooplankton abundance and biomass at station TT043_6-1
DOI: 10.15468/6jt5p2
title: Percentages of planktonic foraminifera species in sediment core V29-144
DOI: 10.15468/bsupb2
title: (Table 5) Oligocene to Pleistocene nannofossil range chart for ODP Hole 134-829A
DOI: 10.15468/cx469w
title: Distribution of benthic foraminifera on sediment core sediment core PS1290-4
DOI: 10.15468/tq9rqa
title: Nano and microzooplankton abundance and biomass at station NBP97-01-05-9
DOI: 10.15468/k58buw
title: Abundance of radiolaria at station UT99-19-2
DOI: 10.15468/w2a66d
title: Nannofossil abundance of Hole 20-199
DOI: 10.15468/bvytez
title: Planktic foraminifera abundance of Hole 14-140
DOI: 10.15468/y7z6jd
title: Total foraminifera counts from M35/1_MSN1043
DOI: 10.15468/npxz7p
title: Counts of Quaternary foraminifera of sediment core CRP-1 (App. 1)
DOI: 10.15468/5239n3
title: Range table from benthic foraminifers in ODP Hole 144-874A
DOI: 10.15468/pnhjr2
title: (Table 6) Distribution of live benthic foraminifera in deep-sea surface sediments of the Scotia Sea, part 1
DOI: 10.15468/g6zcfw
title: Microzooplankton abundance and biomass at station TT045_11-2
DOI: 10.15468/dp9b83
title: Total foraminifera counts of multinet M10/2_MSN229
DOI: 10.15468/emp9j7
title: Relative abundance of planktonic foraminifera in sediment core MK-316
DOI: 10.15468/hkby88
title: Planktic foraminifera abundance of Hole 94-611D
DOI: 10.15468/rnn8hr
title: Plasm bearing foraminifera counts of multinet M42/3_MSN1363
DOI: 10.15468/z8c5u9
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V22-196
DOI: 10.15468/5jaarh
title: (Table 1) Distribution and relative abundance of mid-Cretaceous planktonic foraminifers at DSDP Hole 79-545
DOI: 10.15468/sdsx3v
title: Benthic foraminifera and algae abundance of Hole 81-552A
DOI: 10.15468/52cr5m
title: Range table from benthic foraminifers in ODP Hole 192-1183A
DOI: 10.15468/hkeyeg
title: Total foraminifera counts of multinet M21/2_MSN640
DOI: 10.15468/46ejzt
title: Range table from benthic foraminifers in ODP Hole 161-975B
DOI: 10.15468/nsrxmc
title: Globigerinita spp. in sediment core MSM05/5_712-2
DOI: 10.15468/9hfe89
title: Relative abundance of coccosphere-units of sediment core GIK23071-3
DOI: 10.15468/7w52ur
title: (Table 2) Calcareous nannofossil distribution and relative abundance in ODP Hole 114-703A
DOI: 10.15468/uqyjvy
title: Relative abundances of benthic foraminifera in surface sediments (Table A3)
DOI: 10.15468/svehdx
title: Occurrence of mammalia relicts at site Rotselaar
DOI: 10.15468/bvxv8g
title: Analyses of the recent components in the sand fraction of sediment core PS1422-1
DOI: 10.15468/gq8n74
title: Nannofossil abundance of Hole 11-106B
DOI: 10.15468/8svg26
title: Size of planktic foraminifera at CTD station M39/4_366CTD-22
DOI: 10.15468/b6p2gn
title: Range table from planktonic foraminifers in ODP Hole 180-1114A
DOI: 10.15468/cw6ath
title: Assemblage of living benthic foraminifera in sediment core CD146_55918#7, 63-150 µm
DOI: 10.15468/tqt8na
title: (Table 6) Pleistocene nannofossil range chart for ODP Hole 134-830A
DOI: 10.15468/gq9cu2
title: (Table 4b) Abundances of Globorotalia menardii in sediment core INMD-115BX