cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/cz4ut3
title: (Table 6) Distribution of nannofossils in DSDP Hole 87-583G
DOI: 10.5066/p9n4wlc8
title: Southeast Texas Pilot National Topography Model (NTM), 1933 to 2021

description: The U.S. Geological Survey (USGS) 3D Elevation Program (3DEP) has initiated the development of a second pilot 3D National Topography Model (3DNTM) to generate 3-dimensional surface elevation models that integrate topographic bare-earth elevation surfaces with river channel bed and coastal bathymetry and topobathymetry. Detailed knowledge of integrated river system topography, bathymetry, and topobathymetry is essential for fisheries habitat restoration, hydrologic modeling, and other key science applications such as flood mapping and identification of fluvial geomorphic features. An integrated 1-meter topobathymetric digital elevation model (TBDEM) for Hardin, Orange, and Jefferson counties in Southeast Texas has been developed for this second pilot study. This pilot 3DNTM product supports the Southeast Texas Flood Coordination Study where flood planning and modeling are essential for resource management to minimize impacts from rainstorm and hurricane events. Within the pilot project area of interest, the following hydrographic features are included: reaches of the Neches and Sabine Rivers, Sabine-Neches Water Way (Sabine Channel), Lake Sabine, the Keith Lake-Salt Bayou, and the Intercoastal Waterway. The Southeast Texas TBDEM comprises the spatial integration of 12 different geospatial elevation sources, including topographic lidar data from USGS 3DEP and Texas Strategic Mapping (StratMap), single-beam acoustic data from Texas Water Development Board for the Keith-Lakes-Salt Bayou System, multiple single-beam acoustic surveys from the U.S. Army Corps of Engineers, and nearshore to offshore bathymetry from the National Oceanic and Atmospheric Administration (NOAA), National Centers for Environmental Information (NCEI). The integrated TBDEM will provide a fundamental geospatial baseline to support enhanced 2D/3D hydrologic, storm surge, and sediment-transport modeling. Geospatial data were integrated where the best available topography, topobathymetry, and bathymetry elevation data are sorted and prioritized based on survey date, accuracy, spatial distribution, and point density to develop a TBDEM. Every input data source in the TBDEM has been horizontally referenced to UTM Zone 15 N, NAD83 2011 and vertically referenced to the North American Vertical Datum of 1988 (NAVD88) Geoid12b. The spatial resolution is 1 meter with general elevations ranging from 100.05 meters on land to -34.43 meters offshore. The overall temporal range of the input topography, topobathymetry, and bathymetry is 1933 to 2021.
DOI: 10.15468/34jhnb
title: Benthic foraminifera abundance of ODP Site 184-1143
DOI: 10.15468/9m6c8m
title: Planktic foraminifera abundance of Hole 33-317B
DOI: 10.15468/qfgmvx
title: Nano and microzooplankton abundance and biomass at station NBP96-04A-10-12
DOI: 10.15468/u8ytdp
title: Analyses of the recent components of sediment core PS1402-2
DOI: 10.15468/g6cjb9
title: Relative abundance of deep-sea benthic foraminifera in surface sediments east of New Zealand
DOI: 10.15468/36jp2c
title: Sedimentological investigation on core V25-56
DOI: 10.15468/7uexnd
title: Occurrence of recent nannoplankton in sediment core M1_MULT242, Arabian Sea (Fig. 2)
DOI: 10.15468/ygq6hu
title: Distribution of planktic foraminifera of sediment core IK9373-10
DOI: 10.15468/3r5vds
title: Meiofauna abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/390-1c
DOI: 10.15468/v3esvj
title: (Figure 2d) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3245
DOI: 10.15468/3uwk8g
title: Total foraminifera counts from M35/1_MSN1050
DOI: 10.15468/6qj2we
title: Relative abundance of planktic foraminifera in sediment core GeoB2204-2
DOI: 10.15468/f6y76g
title: Abundance of broken diatom frustules measured on water bottle samples at station PS58/048-3
DOI: 10.15468/qwcvws
title: Range table from benthic foraminifers in ODP Hole 189-1168A
DOI: 10.15468/z2z5br
title: Phytoplankton abundance measured on water bottle samples during POLARSTERN cruise ANT-X/6
DOI: 10.15468/qe9tza
title: (Table 14B) Occurrences of planktonic foraminifers in DSDP Hole 592, samples 592-30-CC through 592-41-CC
DOI: 10.15468/vt5cgp
title: (Table 2) Population densities and biomass of surface sediments
DOI: 10.15468/mkw2k4
title: Neogene palynomorpha from site 93-603, part 1
DOI: 10.15468/atcf92
title: Occurrence of mammalia relicts at site Petnicka Pecina
DOI: 10.15468/vebjhx
title: Analyses of the recent components in the sand fraction of sediment core PS1215-2
DOI: 10.15468/r29wgw
title: Benthic foraminifera accumulation rate of sediment core MD01-2378 during marine isotope stage 3
DOI: 10.15468/6j78u4
title: Occurrence of ostracodes in ODP holes 101-627B and 101-635B (Table 1)

description: In Cores 101-627B-38X, -627B-39X, -627B-43X, -627B-46X, -627B-47X, and in Core 101-635B-14R, 10 species of ostracodes were found, all of which originally were described as being late Albian-Cenomanian from occurrences in the southeastern United States: Cytherella austinensis, Cythereis (Cytnereis) fredericksburgoides, Cythereis (C.) cf. pittensis, Cythereis (Rehacythereis) simunoluda, Cytheropteron (Eocytheropteron) jugosum (very rare), Isocythereis (?) sp., Protocythere alexanderi, Protocythere paratriplicata, Pterygocythereis cf. tokiana, and Schuleridea washitaensis. This assemblage indicates an outer neritic environment.
DOI: 10.15468/na4ntt
title: Meiofauna abundances at the Arctic Håkon Mosby Mud Volcano (HMMV) of sediment core PS64/363-1a
DOI: 10.15468/n5muw3
title: Benthic macrofauna abundance of sediment core 13200-078
DOI: 10.15468/5nx68q
title: (Table 2) Occurrences of ostracodes in ODP Hole 122-762C
DOI: 10.15468/batqkh
title: Large protozoa abundance measured on concentrated water bottle samples at station PS58/107-6
DOI: 10.15468/3tkub4
title: (Table 3) Relative abundances of benthic foraminifera in ODP Site 120-748
DOI: 10.15468/r7zvgm
title: Occurrence of mammalia relicts at site Pestera Hotilor
DOI: 10.15468/sh6q6f
title: Echinoderms in surface sediments off Sylt collected during HEINCKE cruise HE206
DOI: 10.15468/6efphn
title: Relative abundance of live benthic foraminifera of sediment core M5/2_107MC
DOI: 10.15468/rscr9c
title: Nannofossil abundance of Hole 77-540
DOI: 10.15468/wj3tu4
title: Nannofossil abundance of Hole 3-13
DOI: 10.15468/uf6j67
title: (Appendix A) Agglutinated foraminifers in ODP Hole 123-765C
DOI: 10.15468/khhqvg
title: Range table from planktonic foraminifers in ODP Hole 145-883B
DOI: 10.15468/xa47ys
title: Planktic foraminifera abundance of Hole 11-104
DOI: 10.15468/ubgdqk
title: Nannofossil abundance of Hole 5-34
DOI: 10.15468/7yafcw
title: Total foraminifera counts from multinet M31/3_MSN921
DOI: 10.15468/jbqtpc
title: (Table 2) Abundance of benthic foraminifers of sediment core PS2213-4
DOI: 10.15468/2amfv6
title: Petrography, carbonate mineralogy and texture of carbonate rocks of Meteor and Josephine Seamounts, eastern North Atlantic (Table 5)
DOI: 10.15468/rvg5b7
title: Range table from planktonic foraminifers in ODP Hole 159-960C
DOI: 10.15468/xcz4fz
title: (Table 3) Distribution of main species of planktonic foraminifers in Core AMK21-2259, Manus Basin
DOI: 10.15468/xpfc7g
title: Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 189-1168A
DOI: 10.15468/ymht8b
title: (Fig. 5c) Limacina dissolution index of sediment core GeoB2207-2
DOI: 10.15468/8kehmh
title: Occurrence of mammalia relicts at site Upton Warren
DOI: 10.15468/bxwhre
title: Microplankton abundance at Station MARCH-1998-GN36199804611MNB01 in the euphotic zone of the Aegean Sea in March 1998. Part 2 - dinoflagellates
DOI: 10.3886/e194892v1
title: COEP Replication Package for "Why College Majors and Selectivity Matter: Major Groupings, Occupation Specificity, and Job Skills"

description: We provide new approaches to examining the returns to college majors and institutional selectivity. Using unique resume data, we devise new groupings of majors and use these to construct five measures that characterize majors. Applying these measures to the National Survey of College Graduates, we find that majors that lead to jobs that are math-intensive or writing-intensive have higher earnings and also a higher return to selectivity. Majors that are occupationally specific also have higher earnings but have a lower return to institutional selectivity. We find that the value of selectivity relative to major increases as selectivity rises.<br><br>This project contains material needed to use our new major groupings and the five major characteristics we examine.
DOI: 10.15468/7zx9hk
title: Total foraminifera counts of multinet M21/2_MSN638
DOI: 10.15468/gz7x8m
title: (Table 5) Distribution of calcareous nannoplankton in selected samples of ODP Hole 112-682A, Part I
DOI: 10.15468/r2zep9
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-V/1
DOI: 10.15468/33mmn9
title: (Table 6) Temporal variations of relative abundance of dead cells (in detritus, conglomerates and associated with Probocsia alata) of total number of living and dead cells of Emiliania huxleyi at Stations AH-2001-B3 and AH-2001-B3A
DOI: 10.15468/qjhrn7
title: Nekton and plankton counts from neuston net (300 µm) hauls of cruise GAE 1975/76
DOI: 10.15468/s29j8r
title: Abundance of empty diatom frustules measured on water bottle samples at station PS58/061-3
DOI: 10.15468/w562zk
title: (Table T4, T5, T6, T7) Percentage of agglutinated and calcareous benthic foraminiferal species in ODP Hole 178-1098C
DOI: 10.15468/me7df5
title: Occurrence of mammalia relicts at site Grabschütz
DOI: 10.15468/p276gj
title: Analyses of the recent components in the sand fraction of sediment core PS1279-1
DOI: 10.15468/5cjgnt
title: Nannofossil abundance of Hole 3-17
DOI: 10.15468/ztbkg9
title: Nannofossil abundance of Hole 85-573B
DOI: 10.15468/aps97u
title: (Table 2) Planktic foraminifera and their diversity indices of sediment surface samples from the Atlantic Ocean

description: Species distribution patterns in planktonic foraminiferal assemblages are fundamental to the understanding of the determinants of their ecology. Until now, data used to identify such distribution patterns was mainly acquired using the standard &gt;150 µm sieve size. However, given that assemblage shell size-range in planktonic foraminifera is not constant, this data acquisition practice could introduce artefacts in the distributional data. Here, we investigated the link between assemblage shell size-range and diversity in Recent planktonic foraminifera by analysing multiple sieve-size fractions in 12 samples spanning all bioprovinces of the Atlantic Ocean. Using five diversity indices covering various aspects of community structure, we found that counts from the &gt;63 µm fraction in polar oceans and the &gt;125 µm elsewhere sufficiently approximate maximum diversity in all Recent assemblages. Diversity values based on counts from the &gt;150 µm fraction significantly underestimate maximum diversity in the polar and surprisingly also in the tropical provinces. Although the new methodology changes the shape of the diversity/sea-surface temperature (SST) relationship, its strength appears unaffected. Our analysis reveals that increasing diversity in planktonic foraminiferal assemblages is coupled with a progressive addition of larger species that have distinct, offset shell-size distributions. Thus, the previously documented increase in overall assemblage shell size-range towards lower latitudes is linked to an expanding shell-size disparity between species from the same locality. This observation supports the idea that diversity and shell size-range disparity in foraminiferal assemblages are the result of niche separation. Increasing SST leads to enhanced surface water stratification and results in vertical niche separation, which permits ecological specialisation. Specific deviations from the overall diversity and shell-size disparity latitudinal pattern are seen in regions of surface-water instability, indicating that coupled shell-size and diversity measurements could be used to reconstruct water column structures of past oceans.
DOI: 10.15468/jecjcr
title: (Table 3b) Distribution of planktonic foraminiferal tests in sediments from Core NKA-3T
DOI: 10.15468/n2p489
title: (Table 2) Numerical abundances of nannofossil taxa in ODP Hole 126-790A
DOI: 10.15468/3eu74c
title: Occurrence of mammalia relicts at site Grotte du Prince
DOI: 10.15468/3ky7h5
title: (Table A2) Sea surface temperature reconstruction of DSDP Site 94-607 in the North Atlantic
DOI: 10.15468/6tvcmj
title: Benthic macrofauna abundance of subcores of sediment core 13200-073
DOI: 10.15468/c4k4h3
title: Range table from planktonic foraminifers in ODP Hole 159-962B
DOI: 10.15468/ax6n7r
title: Pollen and spores in bottom sediments of the Mediterranean Sea

description: The paper presents results of palynological analysis of deposits from core VITYAZ4779 (length 6.5 m) that was collected from depth 3090 m in the eastern Mediterranean Sea. These palynological data reveal four distinct strata of sediments, each of which was accumulated under different physiographic conditions.
DOI: 10.15468/ebgcx2
title: Occurrence of mammalia relicts at site Nörre-Lyngby

description: Investigations at a Late Weichselian freshwater basin in northwestern Jutland, Denmark, yielded a fairly rich assemblage of vertebrate remains, mostly bones and teeth of small mammals. The remains are primarily allochthonous and the bones have been subjected to different taphonomic pathways and agents. AMS 14C-dates on terrestrial organic remains provided ages of Middle to Late Allerød time. Identifications revealed the first fossil record in Scandinavia of Rana arvalis, Sorex minutus, Ochotona cf. pusilla, Microtus gregalis, Microtus oeconomus, and Sicista cf. betulinu. Spermophilus cf. major and Desmana moschata, previously found only once and twice respectively, were retrieved, and Sorex araneus and Arvicola terrestris were recovered for the first time beyond the Atlantic chronozone. Ecologically, the Nørre Lyngby small mammal fauna can be characterized by its very high and almost equal proportions of boreal forest and steppe elements followed by a relatively high proportion of tundra elements. The fossil species share a modern area of sympatry north of the Caspian Sea from the river Volga in the west to the southern and western slopes of the Urals. If, however, the large Allerød mammals are added, the fauna is without modern analogues. The Nørre Lyngby fauna can be seen as a last expansion of the North European glacial fauna. Provided that an absolute chronology and a differentiated sea-level curve for the area can be established, the Nørre Lyngby fauna could become important for studies in mammalian dispersal and migration rates.
DOI: 10.15468/2gwq9g
title: (Table T1) Planktonic foraminifera stratigraphy of ODP Hole 198-1209A, Zones Palpha-P3b
DOI: 10.15468/43hnb3
title: Isotope tracer experiment: nematode abundance
DOI: 10.15468/wabeu5
title: (Fig. 3) Pollen analysis of the Bosque de Avicennia core
DOI: 10.15468/gjztk3
title: Range table from planktonic foraminifers in ODP Hole 141-859B
DOI: 10.15468/8d2xtm
title: Abundance of planktic foraminifera at CTD station M39/4_376CTD-29
DOI: 10.15468/wxnqef
title: (Appendix 2-6) Distribution of planktonic foraminifera in late Neogene sediments of DSDP Site 58-445 in the western Pacific Ocean
DOI: 10.15468/v4357a
title: (Table 4) Relative abundances of benthic foraminifera in ODP Hole 105-647B
DOI: 10.15468/efja9w
title: Phytoplankton abundance in surface water during Akademik Vernadsky cruise AV22
DOI: 10.15468/uadyvy
title: (List 1) Summary of fossil Mollusca found in Schleswig-Holstein, Germany
DOI: 10.15468/kkzxc5
title: Meiofauna abundance in sediment core 13200-046
DOI: 10.15468/x27f7j
title: Range table from planktonic foraminifers in ODP Hole 152-916A
DOI: 10.15468/7t5vv2
title: (Table 10) Occurrence of benthic foraminifera in ODP Hole 112-688E, Part I
DOI: 10.15468/7n3hmf
title: Range table from planktonic foraminifers in ODP Hole 183-1138A
DOI: 10.15468/eefmpa
title: Total foraminifera counts from multinet M31/2_MSN889
DOI: 10.15468/6zg8b9
title: Microfossil abundance of Hole 16-157
DOI: 10.15468/7dgczs
title: Planktic foraminifera abundance of Hole 68-502C
DOI: 10.15468/nc32pw
title: (Table 4) Relative abundances of planktonic foraminifera in Pliocene sediments of ODP Site 161-975 in the Mediterranean Sea
DOI: 10.15468/kfet6w
title: Planktic foraminifera abundance of Hole 1-1
DOI: 10.15468/t58f8j
title: Living benthic foraminifera at station M33/1_MC-13 (WAST-T), size fraction &gt;125 µm
DOI: 10.15468/ht6a5q
title: Benthic macrofauna abundance of sediment core 12930-052
DOI: 10.15468/qwb36s
title: Assemblage of living benthic foraminifera in sediment core CD146_55901#11, &gt;150 µm
DOI: 10.15468/j31fwo
title: Coleccion de helechos de la FML

description: Plantas colectadas en Sudamérica, principalmente en Argentina y en Bolivia, Brasil, Perú, Uruguay, Paraguay, Colombia y Ecuador. En Centro América ejemplares colectados en Honduras por coleccionistas por coleccionistas de diversas nacionalidades. Las fechas de colección están comprendidas entre los años 1886 y 2011. La colección es curada actualmente por la Dra. Marcela A. Hernández en el Herbario Criptogámico de la Fundación Miguel Lillo
DOI: 10.15468/8qjpuf
title: Microplankton abundance at Station MARCH-1997-GN36199704601MSB01 in the euphotic zone of the Aegean Sea in spring 1997. Part 3 - coccolithophores and other groups
DOI: 10.15468/ps42ha
title: (Figure 3) Distribution chart of benthic foraminifers in ODP Site 126-790
DOI: 10.15468/qb4qeq
title: (Appendix B) Benthic foraminifera extinction group polpulation of ODP Hole 184-1146A
DOI: 10.15468/zccv6j
title: Total foraminifera counts from multinet SO119_MSN1284
DOI: 10.15468/5k5veb
title: (Table T3) Biogenic and mineral composition of sediments cored in Hamburg-Wulksfelde
DOI: 10.15468/rq456j
title: Mean abundance Ophiocten gracilis and sediment surface area covered by the ophiuroids according to total diameter of individuals at different stations on Vøring Plateau
DOI: 10.15468/edsxrn
title: Total fauna of benthic foraminifera of sediment core Kronsmoor, Late Cretaceous
DOI: 10.15468/s9hen4
title: Microplankton abundance in the euphotic zone of the Ionian Sea in October-November 1991
DOI: 10.5281/zenodo.10070238
title: Effects of tree species identity on soil microbial communities in Juglans nigra and Quercus rubra plantations.

description: Black walnut (Juglans nigra L.) forestry within the Central Hardwoods Region (CHR) has progressed primarily based on studies of trial and error among plantations. Although J. nigra wood has been used for everything from gunstocks in the Revolutionary War to the artfully crafted furniture of today, gaps exist in our knowledge base regarding the impact of this hardwood species on the soil. We aim to evaluate and analyze how J. nigra modified soil bacterial and fungal structure in conjunction with soil properties after 10 years of establishment. Additionally, we used another hardwood tree Northern red oak (Quercus rubra L.) for contrast. Our results showed soil microbial structure is influenced primarily by plant species; then by season, and lastly depth. The alpha-diversity index was increased in J. nigra compared to bulk soil values, whereas Q. rubra decreased the index. The most significant disparities in microbiomes were observed between plant species with J. nigra displaying greater enrichment in Nitrospira, Geobacter, Steroidobacter, Bacillus, and Perlucidibaca while Q. rubra more enriched in Acidobacteria (GP1, GP2, and GP3) and ectomycorrhizal fungi (Tuber, Inocybe, Amanita, and Russula). Finally, the co-occurrence networks showed that J. nigra increased node numbers while Q. rubra increased connection (edge) numbers. Additionally, the Q. rubra network displayed the highest mean degree, density, and clustering coefficient while J. nigra exhibited the highest modularity and average connectivity. In conclusion, our findings highlight the intricate interplay between CHR tree species and soil microbiota.
DOI: 10.15468/ya5fw5
title: Range table from benthic foraminifers in ODP Hole 160-967A
DOI: 10.5281/zenodo.10070239
title: Effects of tree species identity on soil microbial communities in Juglans nigra and Quercus rubra plantations.

description: Black walnut (Juglans nigra L.) forestry within the Central Hardwoods Region (CHR) has progressed primarily based on studies of trial and error among plantations. Although J. nigra wood has been used for everything from gunstocks in the Revolutionary War to the artfully crafted furniture of today, gaps exist in our knowledge base regarding the impact of this hardwood species on the soil. We aim to evaluate and analyze how J. nigra modified soil bacterial and fungal structure in conjunction with soil properties after 10 years of establishment. Additionally, we used another hardwood tree Northern red oak (Quercus rubra L.) for contrast. Our results showed soil microbial structure is influenced primarily by plant species; then by season, and lastly depth. The alpha-diversity index was increased in J. nigra compared to bulk soil values, whereas Q. rubra decreased the index. The most significant disparities in microbiomes were observed between plant species with J. nigra displaying greater enrichment in Nitrospira, Geobacter, Steroidobacter, Bacillus, and Perlucidibaca while Q. rubra more enriched in Acidobacteria (GP1, GP2, and GP3) and ectomycorrhizal fungi (Tuber, Inocybe, Amanita, and Russula). Finally, the co-occurrence networks showed that J. nigra increased node numbers while Q. rubra increased connection (edge) numbers. Additionally, the Q. rubra network displayed the highest mean degree, density, and clustering coefficient while J. nigra exhibited the highest modularity and average connectivity. In conclusion, our findings highlight the intricate interplay between CHR tree species and soil microbiota.
DOI: 10.5281/zenodo.8411209
title: Earthquake catalog for California and Nevada

description: Earthquake catalog combining events from California and Nevada from 1980 through September 2023. A concerted effort has been made to only list unique events (i.e., no duplicates across data sources) but it is impossible to guarantee that this has been accomplished perfectly. Similarly, we rely on hypocentral and magnitude efforts from each data center and do not attempt to relocate events or otherwise unify/homogenize the data in any way. The columns in the text file are space delimited: Origin time (UTC) Catalog magnitude Latitude Longitude Depth [km] Data source: Northern California (nc), Southern California (sc), or Nevada (nv)
DOI: 10.15468/u42pt6
title: (Table 7) Relative abundance of benthic foraminifera in ODP Hole 112-683B
DOI: 10.5281/zenodo.10065410
title: Earthquake catalog for California and Nevada

description: Earthquake catalog combining events from California and Nevada from 1980 through September 2023. A concerted effort has been made to only list unique events (i.e., no duplicates across data sources) but it is impossible to guarantee that this has been accomplished perfectly. Similarly, we rely on hypocentral and magnitude estimates from each data center and do not attempt to relocate events or otherwise unify/homogenize the data in any way.
The columns in the text file are space delimited:

Origin time (UTC)
Catalog magnitude
Magnitude type
Latitude
Longitude
Depth [km]
Data source: Northern California (nc), Southern California (sc), or Nevada (nv)