cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/qud2wd
title: Distribution of foraminifera of sediment core GeoB1112-4
DOI: 10.15468/3rsd8y
title: (Table 6) Stratigraphic ranges and relative abundances of Paleogene planktonic foraminifers and other selected organisms in ODP Hole 114-703A
DOI: 10.15468/suat2e
title: Nannofossil abundance of Hole 74-528
DOI: 10.15468/2tndtt
title: Analyses of the recent components of sediment core PS1217-1
DOI: 10.15468/9f8fcq
title: Benthic macrofauna abundance of sediment core 12930-014
DOI: 10.15468/b3ugs3
title: (Table T1) Abundance of stratigraphically important planktonic foraminifera in ODP Site 186-1150 sediments
DOI: 10.15468/x83g6a
title: Nannofossil abundance of Hole 73-522
DOI: 10.15468/kx4n6f
title: (Table 3) Distribution of benthic foraminifers at DSDP Hole 21-206
DOI: 10.15468/2gz6p9
title: Abundance of benthos infauna at station PS1241-1
DOI: 10.15468/9pfsd3
title: Abundance of nematoda in sediment profile M3/1_035 from the Iberian deep sea basin (Table 5)
DOI: 10.15468/s7a5h8
title: Benthic macrofauna abundance of sediment core 13077-089
DOI: 10.15468/kyzp9s
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/091-4
DOI: 10.15468/v5fuvm
title: (Table 2) Quantitative parameters of the Emiliania huxleyi population at the section along 70 m isobath carried out on 26 and 27 August 2001
DOI: 10.15468/5asz2b
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V28-345
DOI: 10.15468/uyua5r
title: Smear slide analysis on sediment core GeoB4215-2
DOI: 10.15468/5vd8gt
title: Foraminifera distribution of sediment core MD81-BC15
DOI: 10.15468/r49ekr
title: (Table 5) Concentrations of organochlorine pesticides in adipose tissue of polar bears (Ursus maritimus) between 1991-2007
DOI: 10.15468/xafyjc
title: (Table 3) Occurrence of dinocyst species in ODP Hole 113-692B
DOI: 10.15468/echngv
title: Relative abundance of coccosphere-units of sediment core GIK23424-3
DOI: 10.15468/wganxg
title: Nannofossil abundance of Hole 7-62
DOI: 10.15468/d52u4a
title: Counts of recycled Pliocene foraminifera of sediment core CRP-1 (App. 1)
DOI: 10.15468/gr7vph
title: Nannofossil abundance of Hole 4-30
DOI: 10.15468/88fvb8
title: Occurrence of mammalia relicts at site la Grotte des Fees
DOI: 10.15468/rpax6g
title: Occurrence of mammalia relicts at site Prekonoska Pecina
DOI: 10.15468/tbdjcp
title: (Table 2) Ostracode assemblages and environment characteristica of modern surface sediment samples from Patagonia, Argentina
DOI: 10.15468/bn6gmt
title: Nannofossil abundance of Hole 3-19
DOI: 10.15468/2prjmb
title: Nannofossil abundance of Hole 9-83A
DOI: 10.15468/xm9xgv
title: Benthic foraminifera and algae abundance of Hole 81-554A
DOI: 10.15468/hpse53
title: Relative abundance of ostracods in sediment core Lz1120
DOI: 10.15468/vyh73u
title: Planktic foraminifera abundance of Hole 72-515B
DOI: 10.15468/pr45mt
title: Nannofossil abundance of Hole 64-475
DOI: 10.15468/gam6qz
title: Dinoflagellate abundance of Hole 71-511
DOI: 10.15468/z26n9c
title: (Table T14) Planktonic foraminifera stratigraphy of ODP Hole 198-1211A, Zones P4a-P6a
DOI: 10.15468/wth3mx
title: Nannofossil abundance of Hole 29-280A
DOI: 10.15468/ks3227
title: Nannofossil abundance of Hole 8-75
DOI: 10.15468/4ax4ax
title: Microzooplankton abundance and biomass at station NBP97-03-16-1
DOI: 10.15468/nkgn3v
title: Range table from benthic foraminifers in ODP Hole 178-1099B
DOI: 10.15468/7v52s6
title: Benthic foraminiferal assemblage (Rose Bengal stained) in MUC OB10-K, turbidite sequence 3
DOI: 10.15468/r2gf3k
title: Nannofossil abundance of Hole 27-262
DOI: 10.15468/hhkfjb
title: Microzooplankton abundance measured on water bottle samples at station PS58/092-3
DOI: 10.15468/y6rbpu
title: Nannofossil abundance of Hole 38-349
DOI: 10.15468/s69tre
title: Faunal assemblage of sediment core GS7603-11
DOI: 10.15468/g2g2b6
title: Total foraminifera counts of multinet M21/6_MSN786
DOI: 10.15468/tfs7sy
title: Planktic foraminifera abundance of Hole 37-335
DOI: 10.15468/ajfrtn
title: Total foraminifera counts of multinet SO118_MSN1266
DOI: 10.15468/hsvcfw
title: Occurrence of mammalia relicts at site Lehringen
DOI: 10.15468/64d7g8
title: (Table 9) Distribution of planktonic foraminifera in the early Pliocene to Holocene section of ODP Hole 149-900A
DOI: 10.15468/7sc42p
title: Assemblage of living benthic foraminifera in sediment core SO129_MC-03, 30-63 µm fraction
DOI: 10.15468/n78u2k
title: Microplankton abundance at Station MARCH-1997-GN36199704603MNB02 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/6v5nqk
title: Abundance of organic-walled dinoflagellate cysts in surface sediments from the Northwest African upwelling area
DOI: 10.15468/k7ma9b
title: Plasm bearing foraminifera counts of multinet M21/1_MSN610
DOI: 10.15468/xvnsbb
title: (Table 11) Distribution of Pleistocene to early Pliocene nannofossils in ODP Hole 108-665A
DOI: 10.15468/2auf22
title: (Table 2) Distribution and relative abundance of planktonic foraminifers in ODP Hole 114-703A
DOI: 10.15468/rcksxk
title: (Table 7) Distribution of planktonic foraminifera in the early Miocene to late Pliocene section of ODP Hole 149-899A
DOI: 10.15468/23b5xg
title: Foraminifera distribution of sediment core SDSE192
DOI: 10.15468/dnyb9d
title: Foraminifera abundance of sediment core C1960.199
DOI: 10.15468/s3ffjv
title: Ostracoda abundance of Hole 42-371
DOI: 10.15468/9s3pkd
title: Planktic foraminifera assemblage in sediment core GIK17051-3
DOI: 10.15468/68mgv5
title: Total foraminifera counts of multinet M21/4_MSN717
DOI: 10.15468/bg2mav
title: Lower Albian Moriez core (Niveau Paquier) individuals per gram sediment of benthic foraminifera, in SE France
DOI: 10.15468/m7rssu
title: Nannofossil abundance of Hole 60-459B
DOI: 10.5281/zenodo.7949096
title: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark

description: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark
DOI: 10.5281/zenodo.8218018
title: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark

description: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark
DOI: 10.15468/6zrgju
title: Phytoplankton abundance during G. M. Dannevig cruise GMD91/10
DOI: 10.5281/zenodo.10070476
title: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark

description: Simulated BCRseq data for the nf-core/airrflow pipeline benchmark
DOI: 10.15468/wyjxnn
title: Benthic macrofauna abundance of sediment core 13200-073
DOI: 10.15468/49atgz
title: Benthic foraminifera abundance of Hole 48-400A
DOI: 10.15468/ydmphg
title: Analyses of the recent components of sediment core PS1279-1
DOI: 10.15468/9r8w5p
title: Abundance of megabenthic species in trawl catches per station in addition to table 2 during POLARSTERN cruise ARK-VIII/2 (EPOS)
DOI: 10.15468/g85xxt
title: (Table 2) Abundance of benthic foraminifers of sediment core PS2161-1
DOI: 10.15468/aeauyb
title: Planktic foraminifera counts of sediment core RC14-29
DOI: 10.15468/zzyskp
title: Total foraminifera counts from multinet M31/3_MSN918
DOI: 10.15468/3jynu3
title: Sarcodine counts and carbon biomass at station TT011_8-CTD96
DOI: 10.15468/nsyu7s
title: (Table 1) Distribution of Lower Cretaceous calcareous nannofossils in ODP Hole 113-692B
DOI: 10.15468/2wtbwj
title: Range table from planktonic foraminifers in ODP Hole 180-1116A
DOI: 10.15468/x4nazv
title: Range table from nannofossils in ODP Hole 199-1217B
DOI: 10.15468/q2xh26
title: Range table from planktonic foraminifers in ODP Hole 180-1111A
DOI: 10.15468/vacqfn
title: Plasm bearing foraminifera counts of multinet M21/5_MSN742
DOI: 10.15468/ywf8mu
title: Phytoplankton abundance at station Rigel_2_2005-02 in Febraury 2005, Chipana, Chile
DOI: 10.15468/jhg9sv
title: (4) Assemblages of planktic foraminifera and Sea Surface Temperature (SST) reconstructed from the Modern Analogue Technique in sediment core MD02-2488 during the Last Interglacial
DOI: 10.15468/vpn32w
title: Total foraminifera counts of multinet FCA97C_MSN1346
DOI: 10.15468/ut26qh
title: Planktic foraminifera counts of sediment core V29-219
DOI: 10.15468/nfrrbk
title: Abundance of living benthic foraminifera in sediment core CD86_10_BC4
DOI: 10.15468/sznauy
title: Planktic foraminifera abundance of Hole 94-610C
DOI: 10.15468/tfhkkk
title: Nannofossil abundance of Hole 47-397
DOI: 10.15468/4a4uxu
title: Phytoplankton long-term time-series at the fixed coastal station in the Gulf of Naples, data for the years 2000-2004. Part 1
DOI: 10.15468/3gswz9
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V22-182
DOI: 10.15468/czpnvg
title: (Table 13) Benthic foraminifera in early-mid Miocene sediments of DSDP Hole 90-592
DOI: 10.15468/dvd45c
title: Total foraminifera counts of multinet M42/3_MSN1367
DOI: 10.15468/rwsj9c
title: Range table from planktonic foraminifers in ODP Hole 171-1049A
DOI: 10.15468/6faavt
title: Benthic foraminifera and algae abundance of Hole 81-553A
DOI: 10.15468/ju3jet
title: Crustacea in surface sediments off Sylt collected during HEINCKE cruise HE241
DOI: 10.15468/xkmn63
title: Abundance and carbon biomass of phytoplankton at station TT007_1-CTD14
DOI: 10.15468/t68e2n
title: Assemblage of living benthic foraminifera in sediment core CD146_55916#1, 63-150 µm
DOI: 10.6084/m9.figshare.23269007
title: Common evolutionary origins of bacGlyRS and AlaRS

description: <b>CLANS input files</b>Files in special ‘CLANS’ format (.clans file) can be loaded into CLANS for visualization of the relationship between proteins based on their all-against-all pairwise sequence similarities.<i>Closest sequence matches to each of the domains of bacGlyRS:</i> catalytic_cluster.CLANS; body-tail_cluster.CLANS; HD_cluster.CLANS; ATL_cluster.CLANS; and ABD_cluster.CLANS.<i>Similarity of bacGlyRS catalytic and ATL domains to archaeal and bacterial uniAlaRS sequences:</i> catalytic_bacGlyRS-AlaRS.CLANS; and ATL_bacGlyRS-AlaRS.CLANS.<b>MSA files</b>Files in FASTA format (.fasta) contain multiple sequence alignments (MSAs) of bacGlyRS and AlaRS sequences that were calculated for a representative set of archaea and bacteria.<b>Spreadsheet file</b>bacGlyRS alpha and beta subunits GenBank identifiers and exact base pair locations of the genes.
DOI: 10.6084/m9.figshare.23269007.v3
title: Common evolutionary origins of bacGlyRS and AlaRS

description: <b>CLANS input files</b>Files in special ‘CLANS’ format (.clans file) can be loaded into CLANS for visualization of the relationship between proteins based on their all-against-all pairwise sequence similarities.<i>Closest sequence matches to each of the domains of bacGlyRS:</i> catalytic_cluster.CLANS; body-tail_cluster.CLANS; HD_cluster.CLANS; ATL_cluster.CLANS; and ABD_cluster.CLANS.<i>Similarity of bacGlyRS catalytic and ATL domains to archaeal and bacterial uniAlaRS sequences:</i> catalytic_bacGlyRS-AlaRS.CLANS; and ATL_bacGlyRS-AlaRS.CLANS.<b>MSA files</b>Files in FASTA format (.fasta) contain multiple sequence alignments (MSAs) of bacGlyRS and AlaRS sequences that were calculated for a representative set of archaea and bacteria.<b>Spreadsheet file</b>bacGlyRS alpha and beta subunits GenBank identifiers and exact base pair locations of the genes.
DOI: 10.15468/wjqp8w
title: Living benthic foraminifera at station M33/1_MC-03 (NAST), size fraction &gt;125 µm
DOI: 10.6084/m9.figshare.23269007.v2
title: Common evolutionary origins of bacGlyRS and AlaRS

description: CLANS input files: Files in special ‘CLANS’ format (.clans file) can be loaded into CLANS for visualization of the relationship between proteins based on their all-against-all pairwise sequence similarities. MSA files: Files in FASTA format (.fasta) contain multiple sequence alignments (MSAs) of bacGlyRS and AlaRS sequences that were calculated for a representative set of archaea and bacteria.
DOI: 10.15468/tgeq4x
title: Range table from planktonic foraminifers in ODP Hole 175-1076A
DOI: 10.15468/zgqdxj
title: Occurrence of mammalia relicts at site Burgtonna
DOI: 10.15468/huh94e
title: (Tables 1,2) Site characteristics and phenotypic attributes of King Penguins (Aptenodytes patagonicus) on Possession Island

description: In colonial species, it is often assumed that locations in the center of the colony are of highest quality and provide highest breeding success. We tested this prediction, known as the "central-periphery model," in a King Penguin colony in the subantarctic Crozet Archipelago. Breeding activity and survival of 150 penguins, fitted with transponder tags, were monitored over an entire breeding season. Among these 150 birds, 50 bred on the slope at the upper periphery of the colony, where the rates of predation and parasitism by ticks were high. Fifty birds bred in the center of the colony, where rates of predation and tick parasitism were low, and 50 bred at the lower end of the colony, where the rate of tick parasitism was low but predation and flooding were important risks. We predicted that the center of the colony should provide the safest breeding place and consequently be characterized by the highest breeding success and be used by the highest-quality individuals. Yet we found that penguins breeding in the center of the colony had the same breeding success as those at both peripheral locations. In addition, penguins breeding on the upper slope had a higher survival rate than penguins breeding at the center or bottom of the slope and were likely of higher quality. Our study does not support the central-periphery model and emphasizes the complexity behind the relationships among breeding site, breeding success, and individual quality.
DOI: 10.15468/jvpdu6
title: Assemblage of total living benthic foraminifera in sediment core SO118_MC-43
DOI: 10.15468/9xs43j
title: Range table from planktonic foraminifers in ODP Hole 170-1042A
DOI: 10.15468/burz3w
title: (Table 1d) Principal petrographic characteristics and K-Ar isotope-geochronological data on samples from the Late Neopleistocene - Holocene activity phase of the Keli Volcanic Highland
DOI: 10.15468/wktbb5
title: Composition of the coarse silt fraction in surface sediments of the northwest African continental margin (Appendix Tab. 4)
DOI: 10.15468/mr355b
title: Pollen analysis of surface samples from Germany and Austria
DOI: 10.15468/6qp6cy
title: Nannofossil abundance of Hole 10-92
DOI: 10.15468/ejcz5t
title: Abundance of Globorotalia menardii of sediment core GeoB2822-2
DOI: 10.15468/e6tkp3
title: Abundance of benthos infauna at station GIK23038-1
DOI: 10.15468/ck4y93
title: Planktic foraminifera counts of sediment core V19-188
DOI: 10.15468/td87ts
title: (Appendix 2) Distribution of planktonic foraminifera in the last 70 kyr of sediment core MD95-2043 from the western Mediterranean Sea
DOI: 10.15468/q8x7x2
title: Analyses of the recent components in the sand fraction of sediment core PS1401-2
DOI: 10.15468/f292a7
title: (Table AT1) Grain size distribution and stable isotope record of benthic foraminifera of ODP Hole 175-1085A

description: The Walvis Paradox states that opal accumulation fluctuates in counterphase to general productivity on Walvis Ridge, off northern Namibia. Sediments of early Quaternary age from Site 1085 (Cores 175-1085A-7H to 10H, off South Africa) were studied to check the phase relationships of general productivity and opal deposition in the region off the Oranje River, near the southern end of the Namibia upwelling system. The proxies used are delta18O of Cibicidoides wuellerstorfi, delta13C of C. wuellerstorfi, benthic foraminifers per gram (BF/g), Uvigerina spp. per gram (U/g), estimated diatom abundance (EDA) and sulfide and oxide aggregates (SOA) in the coarse fraction. EDA and BF/g are taken to indicate diatom and organic matter productivity, respectively. Oxygen isotopes were used to determine phase within the glacial-interglacial cycles. The phase relationships between the different proxies emerge when applying internal stacking methods. For Core 175-1085A-7H, five prescribed 41-k.y. cycles were combined into an average 41-k.y. cycle for the different indices. Productivity indices (BF/g and U/g) tend to follow delta18O in the accustomed manner (with glacial periods showing maximum productivity), but not EDA, whose maximum appears closer to interglacials, offset toward cooling. Thus, phase relationships are similar to those on Walvis Ridge, extending the Walvis Paradox to the southern end of the Namibia upwelling system for the early Quaternary. A tentative reconstruction of the phase of intensity of mixing is given, based on the two productivity indicators EDA and BF/g. Mixing is strongest during the glacial maximum.
DOI: 10.15468/p8sbmv
title: (Table 1) Distribution of silicoflagellates, actiniscidians, and ebridians in selected samples from ODP Hole 112-682A
DOI: 10.15468/mq3wts
title: Total foraminifera counts of multinet M33/1_MSN1030
DOI: 10.15468/9ec695
title: (Table 1) Distribution of planktic foraminifera in sediments from Core AMK4-410GC

description: Sediments in 36 cores recovered from the rift zone of the Reykjanes Ridge were dated on the basis of planktic foraminifera. Their ratios in samples were used to determine temperature of the water surface layer during the last glaciation. Benthic foraminifera were studied in 12 samples of surface sediments and in five cores, and conclusions made on changes in the bottom water layer from changes in composition of these benthic foraminifera.
DOI: 10.15468/u3yyqx
title: (Table 12) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-714A
DOI: 10.15468/cv2jj6
title: Abundance of radiolaria at station LV28-55-2
DOI: 10.15468/wpght4
title: Total foraminifera counts of multinet SO118_MSN1251
DOI: 10.15468/jqtnbs
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station APRIL-1995-D4
DOI: 10.15468/h5ph47
title: (Table 10) Benthic foraminifera in late Miocene sediments of DSDP Hole 90-591
DOI: 10.15468/uax68m
title: Total foraminifera counts of multinet M6/7_MSN150
DOI: 10.15468/5dcjmw
title: (Appendix 2a) Foraminiferal analyses of research borehole Sonder Vium
DOI: 10.15468/d64haa
title: Fig. 3. Pollen record of profile PG1228 from lake Levinson-Lessing
DOI: 10.15468/h9fubr
title: (Table 16) Distribution of planktonic foraminifers in ODP Hole 108-667A
DOI: 10.15468/7dfykn
title: Abundance of radiolaria at station LV28-41-2
DOI: 10.15468/cxtptz
title: Relative abundance of coccosphere-units of sediment core GIK23400-3
DOI: 10.15468/t69g9m
title: Planktic foraminifera abundance of Hole 32-310
DOI: 10.15468/veus6f
title: (Table S1) Palynology of IODP Hole 302-M0004A

description: The Palaeocene/Eocene thermal maximum, 55 million years ago, was a brief period of widespread, extreme climatic warming (Zachos et al., 2003; Kennett and Stott, 1991, doi:10.1038/353225a0; Tripati and Elderfield, 2005, doi:10.1126/science.1109202), that was associated with massive atmospheric greenhouse gas input (Dickens et al., 1995, doi:10.1029/95PA02087). Although aspects of the resulting environmental changes are well documented at low latitudes, no data were available to quantify simultaneous changes in the Arctic region. Here we identify the Palaeocene/Eocene thermal maximum in a marine sedimentary sequence obtained during the Arctic Coring Expedition (Backman et al., 2006, doi:10.2204/iodp.proc.302.2006). We show that sea surface temperatures near the North Pole increased from 18 °C to over 23 °C during this event. Such warm values imply the absence of ice and thus exclude the influence of ice-albedo feedbacks on this Arctic warming. At the same time, sea level rose while anoxic and euxinic conditions developed in the ocean's bottom waters and photic zone, respectively. Increasing temperature and sea level match expectations based on palaeoclimate model simulations (Shellito et al., 2003, doi:10.1016/S0031-0182(02)00718-6), but the absolute polar temperatures that we derive before, during and after the event are more than 10 °C warmer than those model-predicted. This suggests that higher-than-modern greenhouse gas concentrations must have operated in conjunction with other feedback mechanisms -perhaps polar stratospheric clouds (Sloan and Pollard, 1998, doi:10.1029/98GL02492) or hurricane-induced ocean mixing (Emanuel et al., 2004, doi:10.1175/1520-0469(2004)061&lt;0843:ECOTCI&gt;2.0.CO;2)- to amplify early Palaeogene polar temperatures.
DOI: 10.15468/cuufc5
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/042-5
DOI: 10.15468/32494d
title: (Appendix B) Nannofossil abundance in ODP Hole 165-998A sediments
DOI: 10.15468/ru4njf
title: Planktic foraminifera counts of sediment core V14-102
DOI: 10.15468/nsy98j
title: Faunal composition of sediment core MD01-2416
DOI: 10.15468/t7u6n7
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/012-4
DOI: 10.15468/xsb9w8
title: Nannofossil abundance of Hole 10-88
DOI: 10.15468/v9trw7
title: Total foraminifera counts of multinet M27/2_MSN882
DOI: 10.15468/85ycp5
title: (Appendix A5) Planktonic foraminifera of ODP Hole 172-1063A
DOI: 10.15468/bwepn3
title: Benthic foraminifera abundance of Hole 32-308
DOI: 10.15468/5wt46y
title: (Table 3) Distribution of foraminifera in the Miocene section of ODP Hole 133-816B
DOI: 10.15468/yxxe76
title: (Table 2) Stratigraphic ranges and relative abundances of Paleogene planktonic foraminifers and other selected organisms in ODP Hole 114-698A
DOI: 10.15468/kqjmq8
title: Distribution of meiobenthos in sediment core M19_238-2 of the northeastern Atlantic (Table 1)
DOI: 10.15468/fvkdwj
title: Microplankton abundance at Station MARCH-1997-GN36199704601MSB02 in the euphotic zone of the Aegean Sea in spring 1997. Part 2 - dinoflagellates
DOI: 10.15468/suhdwh
title: Plasm bearing foraminifera counts of multinet M27/2_MSN882
DOI: 10.15468/be9ay5
title: Total foraminifera counts of multinet M21/6_MSN767
DOI: 10.15468/we8ugc
title: Abundance of mesozooplankton in the Mediterranean Sea during PELMED 1995 and PELMED 1996

description: The PELMED-ECOPEL dataset contains mesozooplankton data collected in 1995-1996 in the Gulf of Lion (North Western Mediterranean Sea) between 43°35' N, 2°50' E and 42°15' N, 6°15' E. Zooplankton taxonomy-related abundance per unit volume of the water column.
DOI: 10.15468/kq7q2f
title: Range table from planktonic foraminifers in ODP Hole 159-959A
DOI: 10.15468/yj7ntr
title: Abundance of nematoda in sediment profile M3/1_031 from the Iberian deep sea basin (Table 5)
DOI: 10.15468/qk2f7r
title: Assemblage of living benthic foraminifera in sediment core SO117_MC469, &gt;125 µm fraction
DOI: 10.15468/fawxbs
title: (Fig. 2) Occurrence of calcareous dinoflagellate species in ODP Hole 113-689B
DOI: 10.15468/4e3e2z
title: Abundance of benthos infauna at station GIK23024-1
DOI: 10.15468/xsn4ak
title: Microplankton abundance measured on water bottle samples during AEGAEO cruise LIA-7
DOI: 10.15468/z98mgp
title: (Table 3) Distribution of benthic foraminifera in Neogene sediments of DSDP Site 90-590 in the southwest Pacific
DOI: 10.15468/3yw5bp
title: Nematode genera abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/390-1a
DOI: 10.15468/g73fc4
title: Plasm bearing foraminifera counts of multinet M21/2_MSN643
DOI: 10.15468/f28ge8
title: Occurrence of mammalia relicts at site la Grotte Maldidier
DOI: 10.15468/jpp45r
title: (Table 1) Stable oxygen and carbon isotopes, and relative abundances, of selected planktonic foraminiferal species together with biogenic compounds in the surface sediment samples retrieved during the SO-184 cruise off Wand SW Indonesia
DOI: 10.15468/2gju77
title: (Table 2) Planktic foraminiferal abundance in Eocene to Oligocene sediments of ODP Hole 177-1090B on the Agulhas Ridge, South Atlantic
DOI: 10.15468/xuee5g
title: hygromidae

description: Datos de todos los lotes de material seco depositados en la colección del Instituto de Invertebrados, área Zoología de la Fundación Miguel Lillo. Incluyen datos de colecta, numero de ejemplares por lote y sistemática.
DOI: 10.15468/3mvhqk
title: Planktic foraminifera assemblage in sediment core Q208
DOI: 10.15468/fwfsws
title: Microzooplankton abundance and biomass at station TT043_2-1