cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/72br74
title: Apectodinium, age and percentage of endemic and bipolar dinoflagellate cysts of IODP Hole 318-U1356A
DOI: 10.15468/8w4jhz
title: Distribution of foraminifera of sediment core ENAM9321
DOI: 10.15468/qsaca3
title: Relative abundance of Neogene nannofossils at ODP Site 165-999 from the Caribbean
DOI: 10.15468/sy3p3m
title: Benthic foraminifera and algae abundance of Hole 81-552
DOI: 10.15468/pedv8a
title: (Table T3) Planktic foraminiferal assemblages in sediments of ODP Hole 198-1210A, Shatsky Rise, Pacific Ocean
DOI: 10.15468/r9a98r
title: Abundance and carbon biomass of phytoplankton at station TT007_12-CTD147
DOI: 10.15468/aqzmad
title: Occurrence of mammalia relicts at site Trafalgar Square
DOI: 10.15468/8mvszh
title: (Table 3) Occurrence of benthic foraminifera in the Ledyanaya section
DOI: 10.15468/7eqkuu
title: Benthic foraminiferal assemblage (dead) in MUC SC2-L, size fraction 63-150 µm
DOI: 10.15468/b2p8xg
title: (Table T1) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole 171B-1049A
DOI: 10.15468/7w37cd
title: Phytoplankton abundance at station Casma_2003-02-15_1, Casma, Peru
DOI: 10.15468/9rxa3v
title: Planktic foraminifera abundance of Hole 14-139
DOI: 10.15468/jnxc4u
title: Planktic foraminifera assemblage in sediment core GIK23256-1
DOI: 10.15468/yuuqcx
title: (Appendix Table 2) Percentages of benthic foraminiferal taxa, and number of specimens picked for each sample across the uppermost Maastrichtian and lower Danian at ODP Hole 198-1210A
DOI: 10.15468/h3bje5
title: Occurrence of mammalia relicts at site Felsdach Inzighofen
DOI: 10.15468/y2skys
title: Range table from benthic foraminifers in ODP Hole 198-1211B
DOI: 10.15468/fbpvmp
title: (Table 1) Distribution of Cretaceous-Tertiary benthic foraminifers in ODP Hole 129-802A

description: Reworked shallow-water larger and deep-water calcareous benthic foraminifers were recovered from foraminiferal packstones and nannofossil chalks in Hole 802A. The autochthonous zeolitic pelagic claystone is characterized by late Campanian abyssal agglutinated foraminifers that allow correlation with the North Atlantic and the adjacent Pigafetta Basin. Assemblages of DendrophryalRhizammina in graded beds within the zeolitic claystone indicate reworking through entrainment in the flocculent E layer of turbidites, rather than recolonization following a biosiliceous event. Background sedimentation of the claystone took place below the carbonate compensation depth. The nannofossil chalk contains reworked lower bathyal to abyssal calcareous foraminifers of late Paleocene to early Miocene age. The topmost bed of the nannofossil chalk unit commences with an algal foraminiferal packstone containing Lepidocyclina sumatrensis, Heterostegina borneensis, Amphistegina hauerina, Asterigerina marshallana, and A. tentoria, which indicate that the source area was a shallow-water reef and allow the bed to be dated as early Miocene. The absence of obviously younger planktonic microfossils in the graded bed indicates that the resedimentation event was generally contemporaneous with original deposition and took place during an early Miocene global sea-level highstand. An early Miocene shallow-water assemblage is also seen in the graded beds at the base of a volcaniclastic turbidite sequence overlying the nannofossil chalks. Resedimentation of this unit was associated with volcanic activity some distance away.
DOI: 10.15468/ucgkxa
title: Sarcodine counts and carbon biomass at station TT007_3-CTD29
DOI: 10.15468/t7g4jw
title: (Figure 7) Distribution of Cretaceous planktonic foraminifers and associated organisms from DSDP Hole 77-540
DOI: 10.15468/stg5ab
title: Benthic foraminifera abundance of Hole 76-533
DOI: 10.15468/tcyde5
title: Range table from benthic foraminifers in ODP Hole 149-897C
DOI: 10.15468/5yq5hk
title: Nannofossil abundance of Hole 31-300
DOI: 10.15468/acrn3q
title: Nano and microzooplankton abundance and biomass at station NBP97-01-08-9
DOI: 10.15468/sqrz8r
title: Nannofossil abundance of Hole 6-49A
DOI: 10.15468/p85p98
title: (Table 1) Stratigraphic distribution of new marine palynomorph species recorded for the Miocene and lowermost Pliocene of ODP Hole 105-646B

description: Three new dinocyst genera, 14 new dinocyst species, and one new acritarch species are described from the upper Miocene to lowermost Pliocene Site 646 in the Labrador Sea. The new genera described are Habibacysta, Cristadinium, and Muraticysta. The new dinocyst species described are Capillicysta gloriana, Cerebrocysta? namocensis, Corrudinium? labradori, Cristadinium cristatoserratum, Cristadinium diminutivum, Gongylodinium serratum, Habibacysta tectata, Impagidinium fenestroseptatum, Muraticysta microornata, Nematosphaeropsis major, Operculodinium? eirikianum, Operculodinium janduchenei, Selenopemphix dionaeacysta, and Selenopemphix? indentata. A new acritarch species, Cymatiosphaera? invaginata is also described.
DOI: 10.15468/u7xtxg
title: (Appendix H) Benthic foraminifera extinction group species in ODP Hole 172-1055B
DOI: 10.15468/9p4x32
title: (Appendix B5) Distribution of planktic foraminifera in DSDP Site 90-594 east of New Zealand
DOI: 10.15468/pyrmqh
title: Microfossil abundance of Hole 39-356
DOI: 10.15468/jfjyer
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station JANUARY-1995-D4
DOI: 10.15468/hbmcst
title: Microzooplankton (larger protists and small copepods) abundance measured on concentrated water bottle samples at station PS65/580-12
DOI: 10.15468/tnyv9s
title: Assemblage of living benthic foraminifera in sediment core SO117_MC468, 30-63 µm fraction
DOI: 10.15468/vd352m
title: Quantitative study of evolution in the Sphaeroidinella lineage in mid-Pleistocene sediment of ODP Hole 154-926A (Appendix A)

description: Morphological evolution in the late Neogene planktonic foraminifer Sphaeroidinella lineage involves a sudden increase of the percentage of specimens equipped with supplementary apertures (from &lt;30% to &gt;70%) in the mid-Pliocene (about 3.5 Ma). This evolutionary transition, marked by the first occurrence of specimens with large supplementary apertures in the lineage, is denoted the Sphaeroidinella event. Changes in the proportions of the supplementary apertures in the lineage were studied in 24 samples from ODP Hole 926A drilled in the equatorial Atlantic Ocean. In addition, detailed chronological models have been compiled for this section as well as for Pliocene sections from DSDP Holes 214, 502A, and 503B, where evolution in the lineage have been analyzed previously. Stratigraphic correlation of the studied sequences suggests that the Sphaeroidinella event took place at about 3.6 Ma in the eastern equatorial Pacific (Hole 503B) and at 3.5–3.6 Ma in the Caribbean (Hole 502A), while in the Atlantic Ocean (Hole 926A) and in the Indian Ocean (Hole 214) the event occurred after 3.5 Ma. The inferred diachrony of the mid-Pliocene Sphaeroidinella transition, which is considered to represent a prime example of punctuated anagenesis, suggests that this evolutionary modality may have an allopatric component. Its short duration (on average less than 50 kyr) and the detailed biochronology that could be established for this event qualifies it as a useful biostratigraphic tool in the low-latitude Pliocene oceans.
DOI: 10.15468/tb5ruf
title: Distribution of Quinqueloculina sp. in sediment core 12930-028
DOI: 10.25934/pr00009141
title: Fatty Acid Metabolism, Oxidative phosphorylation, and cholesterol homeostasis pathways in endometrial cancer organoids

description: Obesity is a risk factor for many diseases, including at least 20 types of cancer. It is well known that obesity increases endometrial cancer (EC) risk more than any other cancer. American cancer society studies revealed that 70% of endometrial cancers are attributable to excess body weight. EC is the most common gynecologic cancer with incidence (~66,570 new cases/year) and deaths (~12,940 deaths/year) on the rise. Cancer survival has improved since the mid-1970s for all of the most common cancers except cervical and EC, which calls for major treatment advancements. The mechanisms of how obesity promote EC progression was not well understood and urgently needed. We wish to know the published data in this paper and understand Fatty Acid Metabolism, Oxidative phosphorylation, and cholesterol homeostasis pathways in EC organoids. The outstanding genes in those pathways will not only explain the mechanism of obesity driven EC, but also might serves as potential targets to prevent or inhibit obestiy driven EC, eventually leading to future treatments strategy to benefit EC patients.
DOI: 10.15468/dvce6a
title: Ostracoda abundance of Hole 34-319
DOI: 10.15468/ehj84w
title: Content of coarse fraction and G. menardii in sediment corev V25-42
DOI: 10.15468/9uxuqp
title: Total foraminifera counts of multinet M10/2_MSN251
DOI: 10.15468/nut43t
title: Occurrence of mammalia relicts at site Klausennische
DOI: 10.15468/6caacm
title: (Table 8C) Occurrences of planktonic foraminifers in selected samples of DSDP Hole 89-586B, Sections 8-5 through 15-3
DOI: 10.15468/kz6jmr
title: Effects of varying food-availability on ecology and distribution of smallest benthic organisms in sediments of the arctic Fram Strait during POLARSTERN cruise ARK-XV/2

description: With the aims of investigating the response of the smallest benthic biota to a strong ice-edge-related input of phytodetritus, and of registering supposed lateral transportation processes of phytodetrital matter with northerly direction under the ice, we analysed a number of abiotic and biotic parameters in surface sediments from the northern Fram Strait. Two transects of 14 stations in total were made. One transect, crossing the Fram Strait from the east to the west, followed mainly the ice edge. The second transect extended latitudinally in a northerly direction, starting in ice-free areas, passing the ice edge, and ending in heavy ice-covered areas, approximately 100 nm north of the ice edge. Stations along this transect were sampled at almost constant water depths to avoid depth-related influences in our investigations. Results showed the expected high phytodetritus concentrations in the ice-edge vicinity. Concentrations of sediment-bound plant pigments were approximately 5 times higher than in ice-covered areas, indicating a very strong phytodetritus input. With increasing distance from the highly productive areas at the ice edge, we found significantly decreasing concentrations of phytodetrital input to the seafloor in a northerly direction. Within the foraminiferans, generic diversity was clearly reduced in the area of strong phytodetritus deposition. Along the latitudinal transect, out of the direct ice-edge influence, foraminiferal diversities slowly increased within increasing distance from the ice edge. The integration of results from earlier foraminiferal investigations, from stations further to the north, indicates a once more decreasing diversity with continually decreasing food supply.
DOI: 10.15468/ewqknd
title: (Table 2) Stratigraphic ranges of selected Oligocene planktonic foraminifers in ODP Hole 115-706A
DOI: 10.15468/zukqye
title: Abundance of microplankton from bottle APRIL-2000-K4
DOI: 10.15468/kysdsb
title: Planktic foraminifera abundance of Hole 9-83A
DOI: 10.15468/gpybme
title: Range table from planktonic foraminifers in ODP Hole 171-1053B
DOI: 10.15468/urs3j4
title: (Table A5) Distribution of planktic foraminifera and sea surface temperature reconstruction of sediment core V30-97 in the North Atlantic
DOI: 10.15468/gwwypw
title: Total foraminifera counts of multinet POS247/2_MSN1379
DOI: 10.15468/u3a75k
title: (Appendix II) Foraminifera abundance in DSDP Hole 22-214
DOI: 10.15468/9afmfv
title: Range table from planktonic foraminifers in ODP Hole 155-931A
DOI: 10.15468/rbs7hy
title: Total foraminifera counts from multinet M31/3_MSN905
DOI: 10.15468/yy43rg
title: Occurrence of dinoflagellate cysts in ODP Hole 119-738C (Appendix)

description: Forty-one samples from the lower section (between approximately 370 and 495.5 mbsf) drilled at ODP Site 738 (southern Kerguelen Plateau) were analyzed for their palynomorph content. The majority proved to be palynologically barren. Twenty-one species and subspecies of dinoflagellate cysts were recorded, however, from the eight samples that proved productive. The irregular distribution of the cysts makes accurate age determinations difficult, particularly for the lower part of the succession. However, species recovered from Cores 119-738C-21R to 119-738C-23R indicate a latest Maastrichtian age.
DOI: 10.15468/mmpp87
title: Microzooplankton abundance and biomass at station TT043_15-1
DOI: 10.15468/vvz4sj
title: (Table 1) Distribution of planktonic and selected benthic foraminifers from DSDP Site 87-582
DOI: 10.15468/a6kf7q
title: Planktic foraminifera abundance of Hole 32-310
DOI: 10.15468/tn7p53
title: Nannofossil abundance of Hole 10-90
DOI: 10.15468/3mjf5w
title: (Table 1) Distribution of planktonic foraminifera in the upper Turonian-lower Campanian succession in ODP Hole 122-762C, Part I
DOI: 10.15468/zsk9h5
title: Phytoplankton abundance in surface water during cruise CD60
DOI: 10.15468/ffz7h8
title: Benthic macrofauna abundance of sediment core 13077-098
DOI: 10.15468/hukq7r
title: (Table 1) Some abiotic factors and distribution of benthic foraminifers in surface layer of bottom sediments from the littoral zone of the Kunashir Island (Sea of Okhotsk side)
DOI: 10.15468/xudztm
title: (Table 13) Ranges of benthic foraminifers through the early to middle Miocene in ODP Hole 115-715A
DOI: 10.15468/du49yc
title: Microplankton abundance at Station SEPT-1997-GN36199704606MNB02 in the euphotic zone of the Aegean Sea in September 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/m3f5ne
title: Planktic foraminifera counts of sediment core V28-56
DOI: 10.15468/zsv6p5
title: Distribution of planktonic foraminifera in surface sediments of the Mediterranean Sea

description: The Mediterranean Sea is a partillay isolated ocean where excess evaporation over precipitation results in large east to west gradients in temperature and salinity. Recent planktonic foraminiferal distributions have been examined in 66 surface sediment samples from the Mediterranean Sea. In addition to mapping the frequency distribution of 16 species, the faunal data has been subjected to cluster analysis, factor analysis and species diversity analysis. The clustering of species yields assemblages that are clearly temperature related. A warm assemblage contains both tropical and subtropical elements, while the cool assemblage can be subdivided into cool-subtropical, transitional and polar-subpolar groupings. Factor analysis is used to delineate the geographic distribution of four faunal assemblages. Factor 1 is a tropical-subtropical assemblage dominated by Globigerinoiden ruber. It has its highest values in the warmer eastern basin. Transitional species (Globorotalia inflata and Globigerina bulloides) dominate factor 2 with highest values occurring in the cooler western basin. Factor 3 reflects the distribution of Neogloboquadrina dutertrei and is considered to be salinity dependent. Subpolar species dominate factor 4 (Neoglobuquadrina pachyderma and G. bulloides), with highest values occurring in the northern part of the western basin where cold bottom water is presently being formed. The Shannon-Weiner index of species diversity shows that high diversity exists over much of the western basin and immediately east of the Strait of Sicily. This region is marked by equitable environmental conditions and relatively even distribution of individuals among the species. Conversely, in areas where temperature and salinity values are more extreme, diversity values are lower and the assemblages are dominated by one or two species.
DOI: 10.15468/e59629
title: Benthic foraminifera abundance of Hole 42-373A
DOI: 10.15468/fqy3d8
title: Microplankton abundance in the euphotic zone of the Cretan Sea at Station MAY-1995-D4
DOI: 10.15468/ht8d9h
title: Planktic foraminifera abundance of Hole 32-313
DOI: 10.15468/vxw8mm
title: (Table 2) Abundance and biomass of the main phytoplankton groups in subsurface water samples collected in the southeastern Barents Sea in April 2000
DOI: 10.15468/xykzsc
title: (Table 5) Stratigraphic ranges of selected Oligocene to earliest Miocene planktonic foraminifers in ODP Hole 115-709A
DOI: 10.15468/jcpeuv
title: Nannofossil abundance of Hole 86-577
DOI: 10.15468/9pw9ge
title: Planktic foraminifera abundance of Hole 16-155
DOI: 10.15468/ue7xak
title: Plasm bearing foraminifera counts of multinet M21/2_MSN624
DOI: 10.15468/pt5set
title: Benthic foraminifera distribution of sediment core BP00-07/05
DOI: 10.15468/2dm3vn
title: Distribution of meiobenthos in sediment core M19_263 of the northeastern Atlantic (Table 1)
DOI: 10.15468/qqenms
title: Distribution of planktic foraminifers and SST of sediment core GIK15637-1
DOI: 10.15468/wgjzpb
title: Benthic and planktonic foraminifera in ODP Hole 123-766A (Table 1-4)

description: The distribution of 79 foraminiferal species is recorded among 23 samples taken from Cores 123-776A-16R through 123-766A-25R. The benthic species belong to the Ammodiscidae, Ammosphaeroidinidae, Spiroplectamminidae, Verneuilinidae, Tritaxiidae, Globotextulariidae, Eggerellidae, Ichthyolariidae, Nodosariidae, Vaginulinidae, Polymorphinidae, Glandulinidae, Bolivinidae, Turrilinidae, Fursenkoinidae, Pleurostomellidae, Patellinidae, Bagginidae, Quadrimorphinidae, Globorotalitidae, Osangulariidae, and Gavelinellidae families. The planktonic species belong to the Globigerinelloididae, Planomalinidae, Schackoinidae, Hedbergellidae, and Rotaliporidae families. On the basis of foraminiferal biostratigraphy, the interval from Sections 123-766A-16R-3 through 123-766A-17R-3 has been placed confidently in the uppermost Albian (equivalent of the Rotalipora appenninica Zone of Caron, 1985). Below this, correlations are tentative because of the absence of commonly used zonal index species. The interval from lower Core 123-766A-17R to upper Core 123-766A-18R has been placed in the upper Albian; that from lower Core 123-766A-18R to Core 123-766A-21R has been included in the lower to middle Albian; and Cores 123-766A-24R and 123-766A-25R have been correlated with the upper Aptian. The fauna is compared to that known from Aptian-Albian deposits in the Australian epeiric basins and at other sites along the western margin of the continent. These deposits were positioned at middle to high paleolatitudes in the Southern Hemisphere. The benthic assemblages from Site 766 belong to the Marssonella Association (of Haig, 1979) and are similar to those recorded elsewhere along the continental margin, but differ from those of the Ammobaculites Association (of Haig, 1979) within the epeiric basins. In overall aspect, the Australian fauna contains few genera not recorded elsewhere, but lacks many families present in Tethyan (low-latitude) faunas. Comparison of late Albian planktonic foraminifers known from along the continental margin indicates that assemblages from Site 766 are similar to those from the Papuan Basin at approximately the same paleolatitude, but are more diverse than those of the Naturaliste Plateau (approximately 10° of paleolatitude south of Site 766), where Rotalipora and Planomalina are absent. This suggests that a significant gradient in surface water temperature existed on the late Albian continental margin between Site 766 and the Naturaliste Plateau.
DOI: 10.15468/b285w7
title: Planktic foraminifera abundance of Hole 18-174A
DOI: 10.15468/ux524y
title: (Figure 3) Distribution of dinoflagellate cysts in the mid-Cretaceous of ODP Hole 101-635B
DOI: 10.15468/zswr5a
title: Diatom abundance measured on water bottle samples at station PS58/041-2
DOI: 10.15468/aph7jw
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V19-53
DOI: 10.15468/74twmp
title: Planktic foraminifera abundance of Hole 84-568
DOI: 10.15468/kp2w3k
title: Plasm bearing foraminifera counts of multinet POS247/2_MSN1390
DOI: 10.15468/xrk8cx
title: Nano and microzooplankton abundance and biomass at station NBP97-01-28-3
DOI: 10.15468/te5xqc
title: Living benthic foraminifera at station M33/1_MC-19 (CAST), size fraction 63-125 µm
DOI: 10.15468/ra5nhg
title: (Appendix D) Stable carbon and oxygen isotope composition of Globigerinoides sacculifera of ODP Hole 121-758A
DOI: 10.15468/v2wuc4
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 149-900A
DOI: 10.15468/fcagaa
title: (Table T1) Planktonic foraminifera stratigraphy of ODP Hole 198-1209C sediments
DOI: 10.15468/ke43av
title: Range table from planktonic foraminifers in ODP Hole 138-852B
DOI: 10.15468/8v73qr
title: (Appendix A1) Planktonic foraminifera of ODP Hole 157-951A
DOI: 10.15468/dyz3u6
title: (Table T2) Concentrations and accumulation rates of Globorotalia menardii at ODP Hole 175-1087A
DOI: 10.6084/m9.figshare.24498304.v1
title: Self-protective behaviour experiment code

description: The code for the statistical analyses and figures in the manuscript: "noxious stimulation induces self-protective behaviour in bumblebees"
DOI: 10.15468/ds4tch
title: Planktic foraminifera of sediment core GeoB1405-5
DOI: 10.15468/h8wcqx
title: Phytoplankton abundance at station Rigel_3_2005-08 in August 2005, Chipana, Chile
DOI: 10.15468/hjtjym
title: Microplankton abundance at Station MARCH-1998-GN36199804610MSB03 in the euphotic zone of the Aegean Sea in March 1998. Part 3 - coccolithophores and other groups
DOI: 10.15468/de99bg
title: Phytoplankton abundance during Professor Vodyanitskiy cruise PV5
DOI: 10.15468/znebqs
title: (Appendix 6) Benthic foraminifera at termination I in sediment core GIK23068-3 in the Norwegian Sea
DOI: 10.15468/6qa7kc
title: Planktic foraminifera counts of sediment core RC14-9
DOI: 10.7924/r4pr80j7f
title: Data and scripts from: Heterogenous biofilm mass-transport model replicates periphery sequestration of antibiotics in Pseudomonas aeruginosa PAO1 microcolonies

description: A model for antibiotic accumulation in bacterial biofilm microcolonies utilizing heterogenous porosity and attachment site profiles replicated the periphery sequestration reported in prior experimental studies on Pseudomonas aeruginosa PAO1 biofilm cell clusters. These P. aeruginosa cell clusters are in vitro models of the chronic P. aeruginosa infections in cystic fibrosis patients which display recalcitrance to antibiotic treatments, leading to exacerbated morbidity and mortality. This resistance has been partially attributed to periphery sequestration, where antibiotics fail to penetrate biofilm cell clusters. The physical phenomena driving this periphery sequestration have not been definitively established. This paper introduces mathematical models to account for two proposed physical phenomena driving periphery sequestration: biofilm matrix attachment and volume-exclusion due to variable biofilm porosity. An antibiotic accumulation model which incorporated these phenomena better fit observed periphery sequestration data compared to previous models.
DOI: 10.15468/vgscwf
title: (Table 2) Planktonic foraminifera community at DSDP Hole 94-610
DOI: 10.15468/b4bxrk
title: Total foraminifera counts from M35/1_MSN1054
DOI: 10.15468/f8h727
title: Dinoflagellates, pollen and spore abundance of Hole 29-283
DOI: 10.15468/66qbe7
title: Planktic foraminifera abundance of Hole 14-135
DOI: 10.15468/mt7gfh
title: Occurrence of mammalia relicts at site Overmere
DOI: 10.15468/whq87j
title: Fossil occurrence of calcareous nannofossils from IODP Hole 319-C0009A
DOI: 10.15468/76akmp
title: Benthic macrofauna abundance of sediment core 13200-051
DOI: 10.15468/cau4qb
title: Planktic foraminifera abundance of Hole 21-203
DOI: 10.15468/rcw2rq
title: Range table from nannofossils in ODP Hole 139-857A
DOI: 10.15468/p3sa4y
title: Occurrence of mammalia relicts at site Krapina
DOI: 10.15468/srmuec
title: (Table 4) Distribution of planktonic foraminifers in ODP Hole 108-658A
DOI: 10.15468/bkeqkw
title: Assemblage of living benthic foraminifera in sediment core CD145_55808#3, 63-150 µm