cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.788061
title: (Table A1) Species list of the high Antarctic Weddell Sea food web

description: Human-induced habitat destruction, overexploitation, introduction of alien species and climate change are causing species to go extinct at unprecedented rates, from local to global scales. There are growing concerns that these kinds of disturbances alter important functions of ecosystems. Our current understanding is that key parameters of a community (e.g. its functional diversity, species composition, and presence/absence of vulnerable species) reflect an ecological network's ability to resist or rebound from change in response to pressures and disturbances, such as species loss. If the food web structure is relatively simple, we can analyse the roles of different species interactions in determining how environmental impacts translate into species loss. However, when ecosystems harbour species-rich communities, as is the case in most natural systems, then the complex network of ecological interactions makes it a far more challenging task to perceive how species' functional roles influence the consequences of species loss. One approach to deal with such complexity is to focus on the functional traits of species in order to identify their respective roles: for instance, large species seem to be more susceptible to extinction than smaller species. Here, we introduce and analyse the marine food web from the high Antarctic Weddell Sea Shelf to illustrate the role of species traits in relation to network robustness of this complex food web. Our approach was threefold: firstly, we applied a new classification system to all species, grouping them by traits other than body size; secondly, we tested the relationship between body size and food web parameters within and across these groups and finally, we calculated food web robustness. We addressed questions regarding (i) patterns of species functional/trophic roles, (ii) relationships between species functional roles and body size and (iii) the role of species body size in terms of network robustness. Our results show that when analyzing relationships between trophic structure, body size and network structure, the diversity of predatory species types needs to be considered in future studies.
description: The species list that encompasses 488 consumer and resource species from the high Antarctic Weddell Sea was compiled by analyzing over 500 publications: for a full description of the methods used and a full list of these publications see Jacob (2005, http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000118684)
description: Supplement to: Jacob, Ute; Thierry, Aaron; Brose, Ulrich; Arntz, Wolf E; Berg, Sofia; Brey, Thomas; Fetzer, Ingo; Jonsson, Tomas; Mintenbeck, Katja; Möllmann, Christian; Petchey, Owen L; Riede, Jens O; Dunne, Jennifer A (2011): The role of body size in complex food webs: A cold case. Advances in Ecological Research, 45, 181-223
DOI: 10.1594/pangaea.666380
title: Atmospheric electric measurements during the Atlantic Expedition 1969 of RV "Meteor", balloon ascent M16_M39 (Table 1)

description: Cloud cover 2/8, measurement during ascent and descent. Burst level 11.2 km.
DOI: 10.1594/pangaea.887589
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2006403
DOI: 10.1594/pangaea.887603
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2008402
DOI: 10.1594/pangaea.746997
title: Meteorological observations during MAARSEVEEN cruise from Rotterdam to Batavia started at 1663-02-14
DOI: 10.1594/pangaea.759165
title: Physical oceanography during Bjarni Saemundsson cruise B16/99
DOI: 10.1594/pangaea.808310
title: Physical oceanography during John P. Tully cruise TUL96/38
DOI: 10.1594/pangaea.753394
title: (Table 1) P2O5 contents in diatom oozes from the shelf of the Southwest Africa and their sand-fine gravel size fractions

description: Available data on composition of sediments from the inner and outer continental shelves of the Southwest Africa, and on currents and variations of sea level in the Upper Quaternary are examined to elucidate the process of phosphate material concentration. Sand and gravel fractions in diatom oozes from the inner shelf have much higher phosphorus contents than adjoining sediments. This is due to presence of diagenetic phosphate nodules. As sea level varies, fine sediments are eroded by waves or currents that leads to formation of coarse-grained phosphate sediments.
description: Supplement to: Baturin, Gleb N (1971): Formation of phosphate sediments and water dynamics. Oceanology, 11, 372-376
DOI: 10.1594/pangaea.763797
title: (Table 7) Grain size composition of surface layer bottom sediments from the North Dvina mouth area

description: &gt;0 = traces.
DOI: 10.1594/pangaea.777311
title: Well-logging measurements from IODP Hole 314-C0004B

description: Geocode = [m, CMP] Top Depth DSF, MSF, WSF and CSF-B. MWD = measurement while drilling.
DOI: 10.1594/pangaea.777520
title: XRF-core logger measurements from IODP Hole 322-C0011B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.868253
title: Sediment characteristics and geochemistry of composite core ICDP5045-1 (386 sections) and Co1261 (2 sections) at Lake Ohrid (Macedonia, Albania) down to 247 meter sediment depth
DOI: 10.1594/pangaea.499465
title: Physical oceanography from BT during cruise U90XX08231B_1976
DOI: 10.1594/pangaea.755728
title: (Table 1b) Hydrocarbons in surface waters of the Atlantic and Indian Oceans
DOI: 10.1594/pangaea.706106
title: Age model of snow pit DML90S05_25
DOI: 10.1594/pangaea.887592
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2007406
DOI: 10.1594/pangaea.658973
title: Spicule dimensions of Siphonodictyon cf. coralliphagum Rützler, 1971; sample no. MNHN DT 2423

description: Sampled by M. Pruvot and originally identified by E. Topsent as 'Cliona labyrinthica', tentatively identified as S. coralliphagum by C. Schönberg. All measurements are of mature, fully formed oxeas to allow statistical comparison with other samples. Measurements conducted by C. Schönberg on preparation of acid-cleaned spicules made by E. Topsent. Data are sorted vertically by spicule width.; Topsent, Emile (1900) Étude monographique des spongiaires de France. 3. Monaxonida (Hadromerina). Archives de Zoologie Expérimentale et Générale(3)8: 1-331, pls. 1-8 (MNHN DT 2423: pp. 103-104). Schönberg, Christine H. L.; Desqueroux-Faúndez, Ruth (in review) A revision of the genus Aka (Demospongiae : Phloeodictyidae), with the proposal to rename it Siphonodictyon. Zootaxa. Schönberg, Christine H. L. (in review) Eight new descriptions and twenty-one redescriptions of Siphophonodictyon spp. (Demospongiae : Phloeodictyidae), with emphasis on their spicules. Zootaxa.
DOI: 10.1594/pangaea.788234
title: (Table 2) Contents of noble metals in phosphorites and bottom sediments
DOI: 10.1594/pangaea.744396
title: Physical oceanography during Thalassa cruise Thalassa97/2 to the North Sea
DOI: 10.1594/pangaea.914221
title: Biofouling abundance and type observed in marinas in the north-eastern Baltic Sea

description: In the present study, we collected data on biofouling in 17 marinas along the Baltic Sea coast during three consecutive boating seasons (May-October 2014, 2015 and 2016). In this context, we compared different monitoring strategies and developed a fouling index (FI) to characterise marinas according to the recorded biofouling abundance and type (defined according to the hardness and strength of attachment to the substrate). Lower FI values, i.e. softer and/or less abundant biofouling, were consistently observed in marinas in the north-eastern Baltic Sea. The decrease in FI from the south-western to the north-eastern Baltic Sea was partially explained by the concomitant decrease in salinity. Nevertheless, most of the observed changes in biofouling seemed to be determined by local factors and inter-annual variability, which emphasizes the necessity for systematic monitoring of biofouling by end-users and/or authorities for the effective implementation of non-toxic antifouling alternatives in marinas.
DOI: 10.1594/pangaea.876941
title: Continuous sediment temperature observations at station BEFmate_I3pio (2017-04)
DOI: 10.1594/pangaea.737612
title: Documentation of sediment core SO202-31-4
DOI: 10.1594/pangaea.788524
title: Radiosonde measurements from station Izaña (2012-08)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.762207
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0101

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.887590
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2006408
DOI: 10.1594/pangaea.788399
title: (Table T1) Calcareous nannofossil abundance of ODP Site 170-1039 sediments

description: Sediment depth is given in mbsf. Abundance estimates as follows: HA = highly abundant, VA = very abundant, A = abundant, C = common, F = few, f = few reworked, R = rare, r = rare reworked, - = not found.
DOI: 10.1594/pangaea.759988
title: (Table 2) Phosphatase activity in the photic layer of the Kuril region

description: Specific activity - for 1 mg of protein.
DOI: 10.1594/pangaea.762284
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0593

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.744454
title: Physical oceanography during Walther Herwig II cruise WH104/1 to the North Sea
DOI: 10.1594/pangaea.876893
title: Continuous sediment temperature observations at station BEFmate_I3low (2015-11)
DOI: 10.1594/pangaea.876947
title: Continuous sediment temperature observations at station BEFmate_I3upp (2015-02)
DOI: 10.1594/pangaea.498239
title: Physical oceanography from BT during cruise U74X000709B_1957
DOI: 10.1594/pangaea.763161
title: (Table A3) Carbon and nitrogen isotope measurements of cores St-11, DR-16 and DR-13 from the Bering Sea

description: d13C and d15N are based on total organic and total nitrogen values
DOI: 10.1594/pangaea.760355
title: (Table 4) Relative contribution of different sources to REE composition in phosphorites from Pacific seamounts

description: Calculations have been made for two vertical profiles and for ten REE.
DOI: 10.1594/pangaea.776880
title: CNS-analysis from IODP Hole 331-C0017A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.477114
title: Hydrochemistry measured on water bottle samples at station NPac_1974_RY_136E/4442

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.744370
title: (Table 4) Composition of ilmenite and titanomagnetite in hypabyssal rocks from the Omgon Range, Western Kamchatka coastal area

description: 0 = below detection limit.
DOI: 10.1594/pangaea.737617
title: Documentation of sediment core SO202-40-1TC
DOI: 10.1594/pangaea.747135
title: Meteorological observations during Vrouwe Johanna Cores cruise from Middelburg to Gulf of Guinea started at 1753-04-09
DOI: 10.1594/pangaea.751153
title: Meteorological observations during PERSEUS cruise from Charles Town to Antigua started at 1777-01-26
DOI: 10.1594/pangaea.777007
title: MSCL measurements from IODP Hole 331-C0017D

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.845236
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE382/1, Bremerhaven - Cuxhaven, 2012-06-15 - 2012-06-20
DOI: 10.1594/pangaea.776878
title: Core summary for IODP Hole 331-C0017A
DOI: 10.1594/pangaea.817761
title: (Table 6) Abundance of triterpenoid ketones in DSDP Sections 66-487-2-3 and 66-491-1-5

description: Sections 66-487-2-3 and 66-491-1-5: + + =0.2 ng/g; + = &lt;0.1 ng/g. Empty cells = not detected.
DOI: 10.1594/pangaea.762290
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0793

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.733205
title: Physical oceanography during Moana Wave cruise HOT-63 on section PRS2
DOI: 10.1594/pangaea.860460
title: Age model of sediment core MD76-131

description: after Globigerinoides ruber stable isotope data from J-C Duplessy
DOI: 10.1594/pangaea.859279
title: (Table 1) Core top sediment composition and SST reconstruction
DOI: 10.1594/pangaea.712740
title: (Table A4) Composition of coarse fraction of sediment core POS158/1_0021/1

description: Components of coarse fraction (125-500 µm) in grain percentages
DOI: 10.1594/pangaea.816776
title: (Table 2) Soil texture of cryosols from two sites on King George Island in 2008
DOI: 10.1594/pangaea.776899
title: CNS-analysis from IODP Hole 331-C0017B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.743303
title: (Table 13) Chemical composition of Fe-Mn crusts between the Bogdanov Fault and the Sierra Leone Tectonic Zone
DOI: 10.1594/pangaea.756477
title: (Table 1) Heat flow measurements in the Gulf of Aden

description: Heat fllow in the Tadjoura rift ranges from 158 to 348 mW/m**2. Under these conditions convection rate with intrinsic liquid temperature of 60°C is 2.5 m/yr. A body producing heat flow anomaly is a plate inclined toward the Arabian plate at an angle of 10° to vertical. The upper edge of the plate locates at depth of 6 km and its base locates at 45 km. 1300°C isotherm locates at depth of 30 km at distance of 160 km from the constructive boundary.
description: Supplement to: Zolotarev, Vladimir G (1986): Geothermal model of the Aden Rift. Oceanology, 26(6), 717-720
DOI: 10.1594/pangaea.759154
title: Physical oceanography during ARANDA cruise ARA-12-3/97
DOI: 10.1594/pangaea.759889
title: (Table 2) Data on tagging and recapturing of mature cod in 1946-1949

description: Parameters: ''Latitude'', ''Longitude'', and ''Date/Time of event'' show positions and dates of tag points; parameters: ''Latitude of event 2'', ''Longitude of event 2'', and ''Date/Time of event 2'' show positions and dates of recaptures.
DOI: 10.1594/pangaea.887611
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2011408
DOI: 10.1594/pangaea.771869
title: Sedimentation rate and calculated sea surface temperature of sediment core NBP05-05_JPC-42
DOI: 10.1594/pangaea.859274
title: (Table 1, page 153) Location, stratigraphic position, and sample mass for Fe-Mn micronodules from the Alpha Ridge, Central Arctic Ocean

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.845777
title: Meteorological synoptical observations from station Ny-Ålesund (2014-09)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset and a decimal was added to the atmospheric pressure value. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.733150
title: Physical oceanography during Moana Wave cruise HOT-100 on section PRS2
DOI: 10.1594/pangaea.855336
title: (Table 3) Foraminiferal abundances in sediment cores from the Ulleung Basin
DOI: 10.1594/pangaea.887167
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2000403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.747149
title: Meteorological observations during ACTIVE cruise from Jersey to Nova Scotia started at 1777-04-06
DOI: 10.1594/pangaea.887613
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2014405
DOI: 10.1594/pangaea.776945
title: MSCL measurements from IODP Hole 331-C0015B

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.677775
title: Ozone measurements from station South Pole (1998-07)
DOI: 10.1594/pangaea.735736
title: (Table 3) Composition of quenching glasses from the Mid-Atlantic Ridge 5-7°N

description: Analyses have been carried out in the United Institute of Geology, Goeophysics and Mineralogy (Novosibirsk), Siberian Branch of the Russian Academy of Sciences.
DOI: 10.1594/pangaea.782546
title: (Table 1) Composition of basic rocks from the Predmaysky area of the Bol'shoy Lyakhovsky Island
DOI: 10.1594/pangaea.735809
title: (Table 2) Concentration of long chained alkenones and alkenes in seawater samples
DOI: 10.1594/pangaea.887607
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2010402
DOI: 10.1594/pangaea.887608
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2010406
DOI: 10.1594/pangaea.759193
title: Physical oceanography during LANCE cruise LA97/1
DOI: 10.1594/pangaea.776908
title: Thermal conductivity of IODP Hole 331-C0017B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.776580
title: Moisture and density (MAD) measured on IODP Hole 331-C0014E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.681846
title: Meteorological synoptical observations from station Sede Boqer (2006-03)
DOI: 10.1594/pangaea.822995
title: Meteorological measurements in the upper air at station Buhta Providenia, 1949-07-01 to 1949-12-30, ERA-CLIM ID 6008
DOI: 10.1594/pangaea.776720
title: Core-section summary from IODP Hole 331-C0014D
DOI: 10.1594/pangaea.776726
title: Description and distribution of lithologic units (VCD) from IODP Hole 331-C0014D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.787736
title: (Table 1) Tie points used to create ages and distances to the Paleocene-Eocene boundary by the research of ODP Holes 113-689B and 113-690B

description: Sediment depth is given in mbsf. / = PEB and tie-point "c" both assigned an age of 0.00 ka at Site 689. # = interpolated ages for biostratigraphic datums. *0.999 = not recovered or not recognized in the Site 689 record. PEB = delimited by CIE onset (tie-point "c") has been set to 0.00 ka. MA* = morozovellid acme. PAR* = post-CIE acarininid recovery.
DOI: 10.1594/pangaea.477750
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_43S/46

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.776497
title: Description and distribution of lithologic units (VCD) from IODP Hole 331-C0014C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.749210
title: Meteorological observations during EMERALD cruise from Cadiz to Spithead started at 1771-03-28
DOI: 10.1594/pangaea.705665
title: Documentation of sediment core GIK12880-2
DOI: 10.1594/pangaea.733241
title: Physical oceanography during Moana Wave cruise HOT-99 on section PRS2
DOI: 10.1594/pangaea.615803
title: Paleontological research on the Bykovsky Peninsula (Table 5-5)

description: In 1998, we were able to collect at the Bykovsky Peninsula more than 600 bones. Typically for permafrost regions, where fossil bones in summer rapidly emerge from frozen sediment and are delivered to the cliff foot by mud flows, most bones come from the shore and shallow coastal bars, mainly in the area of the Mamontovy Khayata cliff, and another site NW of it, provisionally called ”the Holocene Shore”. However, rather large amount of bones (145) was collected at the Mamontovy Khayata exposure itself. Among them, about 20 bones (location group ”a”) were discovered strictly in situ in the frozen silts and sands, and about 80 bones were found in the mud flows; the initial stratigraphic posi-tion of the latter could be reconstructed more or less precisely (location group ”b”). About 30 bones, listed under the last group, were found on the surface of fresh mud flows evidently related to certain baidzherakhs, or their closely ar-ranged groups, so the original position of these bones can be estimated within 2-4 meters of the baidzherakh height. The other bones, listed under the group ”b”, were found (sometimes in rather high concentrations) on the mud flows related to large exposed parts of the cliff, usually at the base of its upper steep part. The areas of these concentrations are labelled here as ”bone fields”; the possible altitude range of the original position of bones was usually estimated between the height of their occurrence (minimum) and the height of the cliff in this particular area (maximum). The bones referred to the location type ”c” have been found within the Mamontovy Khayata cliff, but their exact position remains unknown. Nearly 300 bones (group ”d”) were collected at the Mamontovy Khayata shore and on the more or less adjacent shallow bars emerging during the lower sea level conditions. About 150 bones were picked up at the ”Holocene Shore” (group ”e”). Finally, a few dozens of bones come from the other sites on the Bykovsky Peninsula (mostly NW from the Mamontovy Khayata), and a few specimens have been delivered from other locations in the Lena Delta (group ”f”).
DOI: 10.1594/pangaea.776572
title: Headspace-gas measurements from IODP Hole 331-C0014E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.776504
title: Structure description (VCD) from IODP Hole 331-C0014C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.733207
title: Physical oceanography during Moana Wave cruise HOT-65 on section PRS2
DOI: 10.1594/pangaea.776264
title: Thermal conductivity of IODP Hole 331-C0014B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.776362
title: Electrical conductivity from IODP Hole 331-C0013F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.776575
title: Description and distribution of lithologic units (VCD) from IODP Hole 331-C0014E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.785443
title: (Table 1) Soil physical parameters of sediments obtained in the Lüchow-Dannenberg district, Lower Saxony

description: The mobility of the radionuclides of the elements Sr, I, Cs and Ce were investigated for three typical sands of Northern Germany under simulated natural, undersaturated flow conditions. The laboratory experiments include the determination of the flow parameters of the seepwater movement as well as the transport velocities of the radionuclides in the sands. For the three selected sands, the following mobility sequence/order has been established for the radionuclides: I &lt; Sr &lt; Cs &lt; Ce
description: Anzahl der Tracerversuche pro Säule N = 19.
description: Supplement to: Klotz, Dietmar; Moser, Heribert (1982): Verhalten von Radionukliden in drei typischen Sanden Norddeutschlands bei wasserungesättigtem Fließen. Meyniana, 34, 95-123
DOI: 10.1594/pangaea.887235
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2008403

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.