cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/vf4a62
title: Nematode abundance in cold seep sediments of the Darwin mud volcano

description: During the JC-10 cruise (2007), we sampled the Darwin mud volcano (MV) for meiofaunal community and trophic structure in relation of pore-water geochemistry along a 10 m transect from a seep site on the rim of the crater towards the MV slope. Sediment samples were retrieved by the ROV Isis using push cores. On board and after the pore water extraction, the top 10 cm of the cores were sliced into 1 cm sections and fixed them in 4% formaldehyde for meiofaunal community analysis. In the home laboratory, the formaldehyde-fixed samples were washed over a 32 µm mesh sieve and extracted the meiofauna from the sediment by Ludox centrifugation (Heip et al. 1985). Meiofauna was then sorted, enumerated and identified at coarse taxonomic level. From each slice, ca. 100 nematodes were identified to genus level. Afterwards, abundance of Nematoda were depth integrated over the top 5 cm to gain individual abundances per 10 cm**2. Overall, total nematode biomass in the top 5 cm of the seep sediment core was ~10x higher than that in the core taken 1100 m away. Nematode genus composition varied little among cores and was mainly dominated by Sabatieria.
DOI: 10.15468/dhe2d4
title: (Table 2) Relaticve abundances of Eocene to Oligocene planktonic foraminifera in ODP Hole 135-841B
DOI: 10.15468/nhmsag
title: (Table 1) Absolute abundances of Eocene to Oligocene planktonic foraminifera in ODP Hole 135-841B
DOI: 10.15468/qckypz
title: (Table 4) Composition of turbidite and background samples at ODP Site 166-1007
DOI: 10.15468/85htdc
title: (Table 3) Composition of turbidite and background samples at ODP Site 166-1003
DOI: 10.15468/xzy9en
title: Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological preparation data from the Miocene, Pliocene and Pleistocene of IODP Site 306-U1313
DOI: 10.15468/xdnav4
title: (Table 1) Benthic foraminifer stratigraphy of ODP Site 166-1006 sediments

description: Site 1006 provides a middle to late Miocene record of bathyal benthic foraminiferal abundance changes in the Straits of Florida. Benthic foraminifers indicate that sedimentation was primarily in situ at Site 1006, with periods of increased downslope transport of shallow-water material. Changes in the in situ faunas may have resulted from circulation changes. Dissolution indices identify a dissolution interval in the upper Miocene section at Site 1006 that may correspond to isotope event Mi5. The data presented here are intended to support a subsequent study (M.E. Katz, J.D. Wright, and K.G. Miller, unpubl. data) that integrates the benthic foraminiferal faunal record with the stable isotopic record, all within a sequence stratigraphic framework. The ultimate goal is to demonstrate that the Miocene faunal and isotopic changes at Site 1006 reflect global, regional, and local influences, and provide constraints on paleobathymetry, sediment provenance, and circulation changes that may reflect changing source regions and glacioeustatic changes.
DOI: 10.15468/nbezwc
title: Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological preparation data from the Miocene, Pliocene and Pleistocene of IODP Site 303-U1308
DOI: 10.15468/vj4n73
title: Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological preparation data from the Miocene, Pliocene and Pleistocene of DSDP Hole 94-610A
DOI: 10.15468/amtnbh
title: Record of 7 acritarch taxa, and palynological preparation data from the Miocene, Pliocene and Pleistocene of DSDP Hole 93-603C
DOI: 10.15468/9aqbwh
title: Record of 7 acritarch taxa from the Miocene, Pliocene and Pleistocene of ODP Hole 151-910C
DOI: 10.15468/7yb5kh
title: (Table 2) Planktonic foraminifer abundance in ODP Section 167-1021C-10H-2
DOI: 10.15468/seq89q
title: (Table 2) Distribution of Cretaceous redeposited benthic foraminifers at DSDP Hole 89-585A
DOI: 10.15468/h8xd8r
title: (Table 1) Distribution of Cretaceous redeposited benthic foraminifers at DSDP Hole 89-585
DOI: 10.6084/m9.figshare.14307881.v1
title: Survey Repository

description: Search queries and results of a literature survey on testing robots and autonomous systems.
DOI: 10.15468/nnmysr
title: (Table 1) Distribution of planktonic foraminifers at DSDP Hole 90-590A
DOI: 10.6084/m9.figshare.14307881
title: Survey Repository

description: Search queries and results of a literature survey on testing robots and autonomous systems.
DOI: 10.15468/g355yq
title: (Table 2) Relative abundance of selceted benthic foraminifera taxa of DSDP Hole 93-605
DOI: 10.15468/f6wr57
title: Pollen analysis of sediment core FEL2, Felchowsee, Germany
DOI: 10.15468/ujwqdm
title: (Table S1) Pb/U zircon ages of ODP Hole 118-735B
DOI: 10.15468/yx2tgj
title: (Table 1) Planktonic foraminiferal communities at DSDP Holes 94-609B and 94-609

description: The planktonic foraminifers in 124 samples from Holes 609 and 609B have been analyzed quantitatively to see whether oceanographic events in the late Miocene and early Pliocene (6.5-4.0 Ma) are reflected in the distribution of individual species. Major changes in sea-surface temperature and bottom-water circulation are postulated, mainly on the basis of the coiling-direction ratios in Neogloboquadrina pachyderma (Ehrenberg) and a dissolution index. A cool interval peaking at around 6.2 Ma was followed by climatic fluctuations, possibly indicative of glacial cycles, before a general warming in the Pliocene. Intense dissolution of CaCO3 at this site on both sides of the Miocene/Pliocene boundary is inferred to have resulted from the presence of Antarctic Bottom Water, and an influx of less aggressive North Atlantic Deep Water is indicated at the actual boundary. These climatic and oceanographic changes are tentatively linked to the Messinian salinity crisis in the Mediterranean.
DOI: 10.15468/jez88j
title: (Table 3) Minerals, and calcareous and siliceous fossil residues from DSDP Hole 93-603
DOI: 10.15468/9n4kkc
title: (Table 6) Benthic foraminiferal community at DSDP Hole 94-611C
DOI: 10.15468/8rktbm
title: (Table 5) Benthic foraminiferal community at DSDP Site 94-610
DOI: 10.15468/et4f3m
title: (Table 4) Benthic foraminiferal community at DSDP Hole 94-609B
DOI: 10.15468/3w5bku
title: (Table 1) Planktonic foraminiferal abundance at DSDP Site 94-606

description: A "total fauna" curve (Ruddiman, 1971; doi:10.1130/0016-7606(1971)82[283:PSITEA]2.0.CO;2) shows that surface water overlying DSDP Site 606 (central North Atlantic Ocean) cooled suddenly at 3.1 Ma, within the Mammoth paleomagnetic reversed interval. At that time, Globorotalia puncticulata, Neogloboquadrina pachyderma, and Globorotalia crassaformis increased and Globorotalia hirsuta, Globigerinoides sacculifer, and Sphaeroidinellopsis decreased in abundance. Oxygen isotope results for Globigerina bulloides do not indicate a "stepwise" cooling, but probably reflect small changes in continental ice volume. It is hypothesized that as annual average temperatures decreased, G. bulloides delayed its bloom from spring to summer to follow a preferred temperature habitat.
DOI: 10.6084/m9.figshare.18115940
title: updated_Data.zip

description: The dataset contains the xyt-coordinates of vehicular traffic simulations and the python code.
DOI: 10.6084/m9.figshare.18115940.v2
title: updated_Data.zip

description: The dataset contains the xyt-coordinates of vehicular traffic simulations and the python code.
DOI: 10.5519/qd.2nbtr8l6
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (2 records)
DOI: 10.6084/m9.figshare.18115940.v1
title: Data.zip

description: The dataset contains the xyt-coordinates of vehicular traffic simulations and the python code.
DOI: 10.15468/sw9vkk
title: (Table 2) Ostracoda community from DSDP Hole 95-613
DOI: 10.15468/hk5g9p
title: (Table 1) Ostracoda community from DSDP Hole 95-612
DOI: 10.15468/hugcpt
title: (Table T2) Benthic foraminfera stratigraphy of ODP Hole 199-1220B sediments
DOI: 10.15468/4n45zj
title: (Table T1) Benthic foraminfera stratigraphy of ODP Hole 199-1218A and 199-1219A sediments

description: We investigated benthic foraminiferal assemblages from Sites 1218 and 1219, Ocean Drilling Program Leg 199, to understand the abyssal response of the eastern equatorial Pacific to the Oligocene climate. Globocassidulina subglobosa, Oridorsalis umbonatus, Gyroidinoides spp., Cibicidoides spp., and Pullenia spp. are common in the lower Oligocene, whereas Nuttallides umbonifer, a dominant species in carbonate corrosive deep water, often dominates the upper Oligocene assemblage at both sites.
DOI: 10.15468/kc2xpe
title: (Table T1) Benthic foraminfera stratigraphy of ODP Hole 199-1215A sediments
DOI: 10.15468/4evyjz
title: (Table T3) Benthic foraminfera stratigraphy of ODP Hole 199-1221C sediments
DOI: 10.15468/gsywae
title: (Table 3) Middle Eocene silicoflagellates from DSDP Hole 95-613
DOI: 10.15468/a2zm3f
title: (Table 2) Upper Eocene silicoflagellates from DSDP Hole 95-612
DOI: 10.15468/yfcgpa
title: (Table 1) Middle Eocene silicoflagellates from DSDP Hole 95-612
DOI: 10.15468/ahrmeh
title: (Table 2) Benthic foraminiferal species observed in the Quaternary samples from DSDP Hole 95-613
DOI: 10.15468/x9f6sb
title: (Table 1) Benthic foraminifera species observed in the Quaternary samples from DSDP Hole 95-612
DOI: 10.15468/3wckcp
title: (Table T5) Planktonic foraminifera abundance of ODP Hole 170-1043A sediments
DOI: 10.15468/35pa8e
title: (Table T4) Planktonic foraminifera abundance of ODP Site 170-1042 sediments
DOI: 10.15468/ry3s6w
title: (Table T3) Planktonic foraminifera abundance of ODP Site 170-1041 sediments
DOI: 10.15468/vfh9pk
title: (Table T2) Planktonic foraminifera abundance of ODP Site 170-1040 sediments
DOI: 10.15468/zyqwm9
title: (Table 3) Neogene relative abundances of Uvigerina spp. at DSDP Hole 95-613
DOI: 10.15468/3xdnvx
title: (Table T1) Planktonic foraminifera abundance of ODP Site 170-1039 sediments
DOI: 10.15468/ak58xn
title: (Table 2) Neogene benthic foraminiferal community at DSDP Hole 95-613
DOI: 10.15468/2ndgjp
title: (Table 1) Neogene benthic foraminiferal community at DSDP Hole 95-612
DOI: 10.15468/63pb6a
title: (Table 2) Eocene benthic foraminiferal community of DSDP Holes 95-613 and 11-108
DOI: 10.15468/vmzgjz
title: (Table T2) Calcareous nannofossil abundance of ODP Hole 171B-1052A sediments
DOI: 10.15468/rxgzkv
title: (Table 1) Eocene benthic foraminiferal community of DSDP Hole 95-612
DOI: 10.15468/naksnr
title: (Table T1) Calcareous nannofossil abundance of ODP Hole 171B-1051A sediments
DOI: 10.15468/hqbmuf
title: (Table T1) Dinoflagellate cyst abundance in ODP Hole 171B-1053A sediments

description: Site 1053 is located at the top of an escarpment cut into the upper part of Blake Nose (29°59.5385'N, 76°31.4135'W). The total core recovery was 189.5 m of upper middle to upper Eocene deposits. An exceptionally thick upper Eocene section was recovered, consisting mainly of siliceous nannofossil ooze (Norris, Kroon, Klaus, et al., 1998, doi:10.2973/odp.proc.ir.171B.1998). These Eocene sediments are unconsolidated as they were not buried by younger deposits. This chapter discusses the distribution of organic walled dinoflagellate cysts (dinocysts) at Hole 1053A. Bio(chrono)stratigraphic divisions cited here follow the initial assignment by the Leg 171B Shipboard Scientific Party (Norris, Kroon, Klaus, et al., 1998, doi:10.2973/odp.proc.ir.171B.1998).
DOI: 10.15468/j74wh5
title: Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C

description: Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most extensively used tool (e.g. [1] for a review), as they are easy to extract from the sediment and can also be used for coupled geochemical (e.g; d18O, d13C, Mg/Ca) and paleo-ecological investigations. Planktonic foraminifera are marine protists, which build a calcareous shell made of several chambers which reflect in their chemistry the properties of the ambient water-masses. Planktonic foraminifera are known to thrive in various habitats, distributed not only along a latitudinal gradient, but also along different water-depth intervals within surface waters (0-1000 m). Regarding their biogeographical distribution, planktonic foraminifera assemblages therefore mirror different water-masses properties, such as temperature, salinity and nutrient content of the surface water in which they live. The investigation of the specific composition of a fossil assemblage (relative abundances) is therefore a way to empirically obtain (paleo)information on past variations of sea-surface hydrological parameters. This paper focuses on the planktonic foraminifera record from the Arctic domain. This polar region records peculiar sea-surface conditions, with the influence of nearly perennial sea-ice cover development. This has strong impact on living foraminifera populations and on the preservation of their shells in the underlying sediments.
DOI: 10.6084/m9.figshare.19245843
title: The source data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.

description: The raw data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.
DOI: 10.6084/m9.figshare.19245843.v2
title: The source data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.

description: The raw data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.
DOI: 10.6084/m9.figshare.19245843.v1
title: The raw data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.

description: The raw data for all results, organized by figures and supplementary figures, are all available. The Mathematica codes used to fit Figure 2b and simulate supplementary figure 4 are also available.
DOI: 10.5281/zenodo.6320520
title: Data supporting the publication "Non-Hermitian chiral phononics through optomechanically-induced squeezing"

description: Data supporting the publication "Non-Hermitian chiral phononics through optomechanically-induced squeezing"
DOI: 10.15468/umjzzp
title: (Table 5) Distribution of benthic foraminifers from ODP Site 134-832
DOI: 10.15468/ekapp3
title: (Table 4) Distribution of benthic foraminifers from ODP Hole 134-829A
DOI: 10.15468/pb9mqa
title: (Table 3) Distribution of benthic foraminifers from ODP Hole 134-828A
DOI: 10.15468/an25ph
title: (Table T3) Stable isotope ratios and abundances of foraminifera from ODP Hole 172-1063D
DOI: 10.15468/fgmp5z
title: (Table 2) Distribution of benthic foraminifers from ODP Hole 134-827A
DOI: 10.15468/bnp8fc
title: (Appendix B) Planktic foraminiferal assemblages from ODP Holes 113-689B and 113-690B
DOI: 10.15468/f9w5x4
title: Calcareous nanofossils in late Pliocene sediments of ODP Site 162-982
DOI: 10.15468/jc7cpe
title: (Table 6) Live benthic foraminifera in sediment core SO130-291MC
DOI: 10.15468/fz2n7k
title: (Table 5) Live benthic foraminifera in sediment core SO130-236MC
DOI: 10.15468/yjet3z
title: (Table 3) Oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A
DOI: 10.15468/n5k63v
title: (Table 4) Live benthic foraminifera in sediment core SO130-242MC
DOI: 10.6084/m9.figshare.18482603
title: Dentists’ Perceptions on the present and future dental practice during the COVID-19 Pandemic

description: The emergence of the COVID-19 pandemic has placed a significant burden on everyone in the worst possible manner. Though dental professionals are at an increased risk for COVID-9 infection, currently, very little is known about how oral health professionals and their professions could be affected by the pandemic. We conducted an embedded mixed-methods study to investigate dentists' perceptions on present and future dental practice because of the COVID-19 pandemic with Indian dentists. A total of 976 responded dentists responded to an online survey. Of them, 61% were females, 32% were 40 years of age or younger. Nearly half of the respondents (54%) acknowledged that the lockdown measures caused them a severe financial burden, and 56% were seriously concerned about being a source of infection to their family, friends, and community. Though 79% felt very comfortable or somewhat comfortable going back to work, they were all worried that Personal Protective Equipment (PPE) use would increase their financial burden and impact the number of patients seeking care. Even though a vast majority received the necessary information concerning returning to practice from their concerning dental regulatory bodies, some were unsure about the reuse of the PPEs because of the conflicting information they received. Our study concluded that, the COVID-19 pandemic affected participants' professional lives negatively. Their major concerns were being a source of infection to their families and community. Providing information to dental professionals in a timely manner may prepare the dentists to provide safe care to their patients while protecting themselves and their families.
DOI: 10.15468/4dsg7e
title: (Appendix) Abundance of Discoaster brouweri and Coccolithus pelagicus in ODP Site 180-1115 sediments
DOI: 10.6084/m9.figshare.18482603.v1
title: Dentists’ Perceptions on the present and future dental practice during the COVID-19 Pandemic

description: The emergence of the COVID-19 pandemic has placed a significant burden on everyone in the worst possible manner. Though dental professionals are at an increased risk for COVID-9 infection, currently, very little is known about how oral health professionals and their professions could be affected by the pandemic. We conducted an embedded mixed-methods study to investigate dentists' perceptions on present and future dental practice because of the COVID-19 pandemic with Indian dentists. A total of 976 responded dentists responded to an online survey. Of them, 61% were females, 32% were 40 years of age or younger. Nearly half of the respondents (54%) acknowledged that the lockdown measures caused them a severe financial burden, and 56% were seriously concerned about being a source of infection to their family, friends, and community. Though 79% felt very comfortable or somewhat comfortable going back to work, they were all worried that Personal Protective Equipment (PPE) use would increase their financial burden and impact the number of patients seeking care. Even though a vast majority received the necessary information concerning returning to practice from their concerning dental regulatory bodies, some were unsure about the reuse of the PPEs because of the conflicting information they received. Our study concluded that, the COVID-19 pandemic affected participants' professional lives negatively. Their major concerns were being a source of infection to their families and community. Providing information to dental professionals in a timely manner may prepare the dentists to provide safe care to their patients while protecting themselves and their families.
DOI: 10.15468/7knvr5
title: (Table 4) Thecosomata in ODP Hole 134-831A
DOI: 10.15468/y43ahx
title: (Table 4) Abundance of under-ice amphipods on flat ice and ice ridges sampled during the 2005 Hidden Ocean expedition
DOI: 10.15468/8xfpe8
title: (Table 2) Abundance of metazoan ice meiofauna in the bottom 30 cm of level sea ice obatined during the 2005 Hidden Ocean expedition
DOI: 10.15468/p6kuhz
title: (Table 3) Relative abundances of benthic foraminifera in chosen time-slices from cores obtained in the Nordic and Barents Seas
DOI: 10.15468/vtusrh
title: (Table 3) Dead benthic foraminifera in surface sediments from the eastern South Atlantic Polar Front region
DOI: 10.15468/mzvp86
title: (Table 2) Osmium isotope ratios and Re-Os element content for cleaned and uncleande foraminifera of ODP Hole 121-758A
DOI: 10.15468/24ya96
title: (Table 2) Live benthic foraminifera in surface sediments from the eastern South Atlantic Polar Front region
DOI: 10.15468/7sbq93
title: (Table 1) Osmium isotope ratios and Re-Os element content in bulk sediments of ODP Hole 121-758A
DOI: 10.15468/5m4v4m
title: (Table 1) Trawled distance, Isopoda per 1000 m haul length, expected number of species, evenness, and the Shannon-Wiener index during POLARSTERN cruise ANT-XXII/3 (ANDEEP III)
DOI: 10.15468/fns5em
title: (Table 1) Trawled distance, Isopoda per 1000 m haul length, expected number of species, evenness, and the Shannon-Wiener index during POLARSTERN cruise ANT-XIX/4 (ANDEEP II)
DOI: 10.15468/mnqp9a
title: (Table 1) Trawled distance, Isopoda per 1000 m haul length, expected number of species, evenness, and the Shannon-Wiener index during POLARSTERN cruise ANT-XIX/3 (ANDEEP I)
DOI: 10.15468/chhhu4
title: (Table 1) Sulphur chemistry of ODP Site 206-1256 volcanic section
DOI: 10.15468/kj6s6k
title: (Table 2) Relative abundances of shallow-water foraminifera in ODP Hole 133-821A
DOI: 10.15468/rcuj2s
title: (Table 2) Abundance of Miocene to Pleistocene dinoflagellate cysts in ODP Site 133-823
DOI: 10.15468/rha4b8
title: (Table 1) Abundance of Miocene to Pleistocene dinoflagellate cysts in ODP Hole 133-815A
DOI: 10.15468/x3fgnm
title: (Table 1) Abundance of Pleistocene dinoflagellate cysts in ODP Site 133-820

description: Compared with other Australian marine Quaternary locations, Site 820's dinoflagellate cyst assemblages are low in both abundance and diversity. Abundances are between &lt; 1 and 14 cysts/cm3 , and the number of species is between 7 and 14 per sample. The dominant species are Operculodinium israelianum, Spiniferites bulloideus, Spiniferites hyperacanthus and Tuberculodinium vancampoae, which together usually make up more than 75% of the assemblage. The rareness of Protoperidinium spp., taxa usually associated with nutrient enrichment, suggests that upwelling was not a regular feature of this region during the Quaternary. The relative dinoflagellate abundance, which indicates changes in the position of the coastline, shows the presence of several sea-level events, particularly near the base of the sequence. Here, they parallel at least two upward-coarsening cycles in the sediment record. Further comparison is hindered by too large a sampling interval.
DOI: 10.15468/n7rp2v
title: (Table AT9) Planktonic foraminiferal stratigraphy of ODP Hole 182-1134B
DOI: 10.15468/tngn8y
title: (Table AT8) Planktonic foraminiferal stratigraphy of ODP Hole 182-1134A
DOI: 10.15468/d4w84y
title: (Table AT5) Planktonic foraminiferal stratigraphy of ODP Hole 182-1130A
DOI: 10.15468/wnajgh
title: (Table AT6) Planktonic foraminiferal stratigraphy of ODP Hole 182-1130B
DOI: 10.15468/ypyzqv
title: (Table AT4) Planktonic foraminiferal stratigraphy of ODP Hole 182-1128C
DOI: 10.15468/fq3sm2
title: (Table AT3) Planktonic foraminiferal stratigraphy of ODP Hole 182-1128B
DOI: 10.15468/fp4pb3
title: (Table AT2) Planktonic foraminiferal stratigraphy of ODP Hole 182-1126C
DOI: 10.15468/xxcspx
title: (Figure 6) Dinoflagellate cyst measured on sediment core AI07-12G
DOI: 10.15468/ndsr32
title: (Figure 4) Dinoflagellate cyst measured on sediment core AI07-03G
DOI: 10.15468/mytd76
title: (Table AT1) Planktonic foraminiferal stratigraphy of ODP Hole 182-1126B
DOI: 10.15468/bjpd3d
title: (Figure 4) Dinoflagellate measurements from sediment core DA06-139G during DANA cruise in 2006
DOI: 10.15468/umqp2g
title: Meiobenthic taxon counts from deep-sea in situ recolonization experiment II deployed at station PS64/475-1 during ARK-XIX/3c
DOI: 10.15468/hq2kar
title: Meiobenthic taxon counts from deep-sea in situ recolonization experiment I deployed at station PS64/474-1 during ARK-XIX/3c
DOI: 10.15468/4yjz89
title: (Supplementary data 1) Count data of the observed dinoflagellate cyst species from sediment core GeoB10709-5