cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.928089
title: Phytoplankton biomass accumulation at Chatham Rise, east of New Zealand, measured during the SalpPOOP (TAN1810) campaign onboard the RV Tangaroa

description: Biomass accumulation was assessed by subtracting phytoplankton mortality (due to microzooplankton) from phytoplankton growth rates. Rates of phytoplankton growth and microzooplankton grazing were assessed daily with the dilution technique (Landry and Hassett 1982; doi:10.1007/BF00397668), following the two treatment approach (Landry, Haas et al. 1984 doi:10.3354/meps016127), at six depths within the euphotic zone. We implemented this mini-dilution approach to generate vertically resolved growth and grazing rates, but also conducted a full dilution experiment on the last day of each of the cycles (n = 5) to test linearity assumptions of the method. Seawater collected with the Niskin bottles attached to the CTD rosette at 02:00 h was used to fill a pair of 2.2-L polycarbonate bottles (100%, B and C) while a third bottle (A) was filled with 25% whole seawater diluted with 0.2-µm filtered seawater obtained immediately before by gravity filtration using an Acropak filter cartridge (Pall) directly from the same Niskin bottle. Nutrients (final concentrations in 2.2L bottles; nitrate 0.18 μM, ammonium 4.16 μM, phosphate 15.08, silicate 44.2 μM, and vitamins) were added to bottles A and B in order to ensure the assumption that the same phytoplankton intrinsic growth rate was occurring in WSW and FSW bottles despite dilution (Gutiérrez‐Rodríguez, Safi et al. 2020 doi:10.1029/2019JC015550). Bottles were then incubated in situ at the same six depths of collection using a drifting array. Rates were calculated from changes in Chl a concentration and picophytoplankton abundance between the beginning and end of the experiment assuming exponential growth of phytoplankton. Microzooplankton grazing rate was estimated from: µ = (kA – kB)/(1-x) where kA and kB are the observed net rates of change of chl a in bottles A and B, respectively, and x is the fraction of whole seawater in the diluted bottle A (0.25). Phytoplankton growth rate was estimated from µ =m+kB. Photoacclimation effects were corrected from changes in cell chl a fluorescence estimated by flow cytometry during incubations as a proxy of cell chl a content (Gutierrez-Rodriguez, Latasa et al. 2010 doi:10.1016/j.dsr.2009.12.013). These include estimating the photoacclimation index (Phi) from changes in FL3: FSC and calculating an average value from Phi index obtained for pico- and nanoeukaryotic populations weighted by their biomass contribution. Accumulation was calculated by subtracting the C-based estimates of microzooplankton grazing (from the dilution experiments) from the 14C-based NPP.
description: Empty cells = ndThis study was funded by the Ministry for Business, Innovation and Employment (MBIE) of New Zealand, NIWA core programmes Coast and Oceans Food Webs (COES- COES1901) and Ocean Flows (COOF-COOF1902), the Royal Society of New Zealand Marsden Fast-track award to Moira Décima, and NSF award #OCE-1756610 to Michael R. Stukel and Karen E. Selph.
DOI: 10.1594/pangaea.949292
title: Bayesian Modelling of the composite profile HZM19

description: Conducted using Bacon (version 4.1.1) for the R programming software. Model A: based on C-14 only; Model B: based on radiocarbon, parameter settings derived from information of the varve chronology (VT-99); Model C: based on radiocarbon dates and VT-99 as normal-distributed tie-points; Model D: segmented into four sections: section 1 and 3 are based on VT-99, sections 2 and 4 are based on Bacon models.
DOI: 10.1594/pangaea.759490
title: Expanded measurements from Neumayer Station (2011-01)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.748765
title: Meteorological observations during ECHO cruise from St. Eustatius to Paramaribo started at 1834-12-12
DOI: 10.1594/pangaea.834960
title: Pollen record of sediment core SONK_11_D

description: Sediment depth is given in composite depth (mcd).
DOI: 10.1594/pangaea.759468
title: Ozone measurements from Neumayer Station (2010-09)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.897151
title: Rock magnetic properties of sediment core GeoB18516-2
DOI: 10.1594/pangaea.834855
title: Maximum ingestion and maximum clearance rate of dinoflagellates determined experimentally
DOI: 10.1594/pangaea.858828
title: Radiosonde measurements from Neumayer Station (2015-07)
DOI: 10.1594/pangaea.749997
title: Meteorological observations during KOERIER cruise from Suriname to Curaçao started at 1832-10-04
DOI: 10.1594/pangaea.858913
title: Continuous meteorological observations at Neumayer station (2015-10)
DOI: 10.1594/pangaea.937635
title: List of specimens for geometric morphometric analyses of the wing venation of wasps (Vespinae, Vespidae, Hymenoptera, Insecta)

description: A list of Vespinae specimens (Vespidae, Hymenoptera, Insecta) is given in this dataset. The information is related to data of wing landmark coordinates that are archived separately in PANGAEA (see Related to section, Abels & Wedmann 2021). The data were used in the geometric morphometric analyses of Abels & Wedmann (2022). This dataset includes 1025 Vespinae specimens analysed by Perrard et al. (2014, 2015). The following five specimens are added: Vespula rufa (photo "Rødveps Vespula rufa (Linnaeus, 1758)" by Arnstein Staverløkk CC BY-SA 4.0, https://www.artsdatabanken.no/Pages/F21128, accessed 21.02.2021), Vespula nursei (Kumar & Carpenter 2018: Fig. 5), Vespula pensylvanica (Snelling 1981: Fig. 66) and the fossil Palaeovespa socialis (Poinar 2005: Fig. 14) and the species Vespula? hassiaca described in Abels & Wedmann (2022).
DOI: 10.1594/pangaea.756458
title: (Table 1.2) Biogenic, terrigenous and authigenic components of ODP Hole 104-642D

description: Grain amount percentages, based on 500-700 grains.
DOI: 10.1594/pangaea.650348
title: Description of lithologic section units of Hole 310-M0009A

description: Abbreviations: encr=enrcusting, br=braching, rob=robust, tab=tabular, fol=foliaceous, mas=massive, frags/frag=fragments/fragmented, unident=unidentifies, CAB=coral-algal bindstone, ECR=encrustation, MB=microbiolite, HAL=Halimeda, IS=in situ, UK=unknown, gp=group; DEPTH applies to top depth of section unit
DOI: 10.1594/pangaea.890414
title: Geochemistry of La_Grande_coreL3T1C2 peat core
DOI: 10.1594/pangaea.875558
title: (Table 5, page 705) Chemical composition of layers out from the inner core of a fossil manganese nodule from DSDP Leg 81 (Holes 552A)
DOI: 10.1594/pangaea.495737
title: Water temperature MBT profiles from cruise U74X124280M_1972
DOI: 10.1594/pangaea.897158
title: Plainfin midshipman (Porichthys notatus) sperm to seminal fluid (SF) ratio
DOI: 10.1594/pangaea.748721
title: Meteorological observations during DUNKIRK cruise from Dunnoze to Plymouth started at 1757-12-09
DOI: 10.1594/pangaea.756460
title: (Table 1.3) Biogenic, terrigenous and authigenic components of ODP Hole 104-643A

description: Grain amount percentages, based on 500-700 grains. &lt;1 = traces.
DOI: 10.1594/pangaea.498215
title: Physical oceanography from BT during cruise U74EH08614B_1955
DOI: 10.1594/pangaea.861262
title: Sea surface temperature reconstruction for ODP Site130-806

description: Dataset was corrected on 2018-05-29, columns for TEX86- and UK'37-temperatures were switched in the old version.
DOI: 10.1594/pangaea.495313
title: Water temperature MBT profiles from cruise U31X006507M_1965
DOI: 10.1594/pangaea.834842
title: (Supplementary table 1) Characteristics of echolocation clicks of narwhal (Monodon monoceros) north of Disko Island, west Greenland
DOI: 10.1594/pangaea.694922
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-IR60

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.855397
title: (Table 1) Radiocarbon ages of ODP Hole 146-893A

description: High-resolution planktonic foraminiferal census data from Santa Barbara Basin (Ocean Drilling Program hole 893A) demonstrate major assemblage switches between 25 and 60 ka that were associated with Dansgaard-Oeschger cycles. Stadials dominated by Neogloboquadrina pachyderma (sinistral), and Globigerinoides glutinata suggest a strong subpolar California Current influence, while interstadials marked by abundant N. pachyderma (dextral) and G. bulloides indicate a relative increase in subtropical countercurrent influence. Modern analog technique and transfer function (F-20RSC) temperature reconstructions support d18O evidence of large rapid (70 years or less) sea surface temperature shifts (3° to 5°C) between stadials and interstadials. Changes in the vertical temperature gradient and water column structure (thermocline depth) are recorded by planktonic faunal oscillations suggest bimodal stability in the organization of North Pacific surface ocean circulation. Santa Barbara Basin surface water demonstrates the rapid response of the California Current System to reorganization of North Pacific atmospheric circulation during rapid climate change.
description: Sample data were taken from Ingram and Kennet (1995).
description: Supplement to: Hendy, Ingrid L; Kennett, James P (2000): Dansgaard-Oeschger Cycles and the California Current System: Planktonic foraminiferal response to rapid climate change in Santa Barbara Basin, Ocean Drilling Program Hole 893A. Paleoceanography, 15(1), 30-42
DOI: 10.1594/pangaea.834310
title: Growth rate of Dolioletta gegenbauri and Thalia democratica determined experimentally
DOI: 10.1594/pangaea.845431
title: Continuous meteorological observations at Neumayer station (2014-02)
DOI: 10.1594/pangaea.858840
title: Expanded measurements from Neumayer Station (2015-09)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.749583
title: Meteorological observations during HEUREUX cruise from West Indies to Coastal started at 1801-05-02
DOI: 10.1594/pangaea.834562
title: Growth rate of Paraphysomonas imperforata and Euphausia pacifica determined experimentally
DOI: 10.1594/pangaea.834861
title: Maximum ingestion and maximum clearance rate of Favella ehrenbergii and Favella taraikaensis determined experimentally
DOI: 10.1594/pangaea.834642
title: Stick and slip measurements from ODP Leg 170 and Leg 205
DOI: 10.1594/pangaea.834563
title: Growth rate of Oithona similis determined experimentally
DOI: 10.1594/pangaea.858850
title: Expanded measurements from Neumayer Station (2015-11)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.834443
title: Growth rate of Eurytemora affinis determined experimentally
DOI: 10.1594/pangaea.858853
title: Radiosonde measurements from Neumayer Station (2015-12)
DOI: 10.1594/pangaea.845469
title: Basic and other measurements of radiation at Neumayer Station (2014-06)
DOI: 10.1594/pangaea.937651
title: Data for geometric morphometric analyses of the wing venation of wasps (Vespinae, Vespidae, Hymenoptera, Insecta)

description: This dataset includes wing landmark coordinates for Vespinae specimens (Vespidae, Hymenoptera, Insecta). The data were used in the geometric morphometric analyses of Abels & Wedmann (2022). Information on the different Vespinae specimens are archived separately in PANGAEA (see Related to section, Abels & Wedmann 2021). Perrard et al. (2014, 2015) provided data of 19 landmark coordinates of 1025 measured Vespinae wings, of which 17 landmarks are resorted and reproduced in this data set. The following five specimens and their wing landmarks are added: Vespula rufa (photo "Rødveps Vespula rufa (Linnaeus, 1758)" by Arnstein Staverløkk CC BY-SA 4.0, https://www.artsdatabanken.no/Pages/F21128, accessed 21.02.2021), Vespula nursei (Kumar & Carpenter 2018: Fig. 5), Vespula pensylvanica (Snelling 1981: Fig. 66), the fossil Palaeovespa socialis (Poinar 2005: Fig. 14) and the species Vespula? hassiaca described in Abels & Wedmann (2022). For details on data acquisition and analysis see Abels & Wedmann (2022).
DOI: 10.1594/pangaea.822915
title: Meteorological measurements in the upper air at station Peshawar, 1929-01-03 to 1935-12-15, ERA-CLIM ID 5819

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.858844
title: Ozone measurements from Neumayer Station (2015-10)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.858642
title: (Appendix 9) Characteristics of Pokhodsk cores and pits

description: Ice content is the amount of ice contained in frozen or partially frozen soil or rock.- absolute ice content: the ratio of the mass of the ice in a sample to the mass of the frozen sample- gravimetric ice content: the ratio of the mass of the ice in a sample to the mass of the dry sample (the gravimetric ice content can greatly exceed 100 percent)
DOI: 10.1594/pangaea.743905
title: Grain size analysis on Site 208-1266
DOI: 10.1594/pangaea.858843
title: Radiosonde measurements from Neumayer Station (2015-10)
DOI: 10.1594/pangaea.715047
title: (Appendix Table 1) Sr/Ca ratios of Coccoliths from ODP Hole 198-1209C
DOI: 10.1594/pangaea.858814
title: Ozone measurements from Neumayer Station (2015-04)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.717969
title: Other measurements at 10 m from station Boulder, SURFRAD (2005-10)
DOI: 10.1594/pangaea.834598
title: Growth rate of Pseudodiaptomus marinus determined experimentally
DOI: 10.1594/pangaea.834713
title: Maximum ingestion and maximum clearance rate of Euphausia superba determined experimentally
DOI: 10.1594/pangaea.858909
title: Continuous meteorological observations at Neumayer station (2015-08)
DOI: 10.1594/pangaea.748261
title: Hydrography on standard level calculated from water bottle samples of RV Skif from 1969 to 1980
DOI: 10.1594/pangaea.834603
title: Growth rate of Calanus pacificus and Pseudocalanus sp. determined experimentally
DOI: 10.1594/pangaea.750872
title: Meteorological observations during NAUTILUS cruise from Plymouth to Cape Henry started at 1762-12-14
DOI: 10.1594/pangaea.776735
title: Structure description (VCD) from IODP Hole 331-C0014D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.915117
title: Radiosonde raw data from tandem soundings at Neumayer Station (2019-06), links to files

description: At Neumayer station the transition of sonde type from Vaisala RS92-SGP to RS41-SGP is controlled by tandem soundings starting in July 2018. Each file in this dataset was acquired together with the corresponding data file in doi:10.1594/PANGAEA.915086.
DOI: 10.1594/pangaea.834734
title: (Table S2) Stable carbon isotopic values of sugars and glycerol of the 2G-GDGT fraction purified from ODP Hole 201-1229A

description: Subsurface sample from the Peru Marin spiked or not spiked with the TLE of [99%-13C]S. platensis. Results are the means and standard errors of duplicate analyses.
DOI: 10.1594/pangaea.897192
title: Meteorological synoptical observations from station Fukuoka (2018-11)
DOI: 10.1594/pangaea.859762
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE396
DOI: 10.1594/pangaea.495267
title: Water temperature MBT profiles from cruise U3190215M_1954
DOI: 10.1594/pangaea.663556
title: Oceanography at CTD/bottle station IFREMER_0396
DOI: 10.1594/pangaea.707840
title: (Appendix 3) TOC concentrations and accumulation of ODP Site 184-1143

description: Sediment depth (m) is composite depth (mcd)
DOI: 10.1594/pangaea.833706
title: Supplementary table 1: Raw X-ray fluorescence (XRF) core scanning data (Al, Ca, Ti, Fe) of DSDP Site 48-401
DOI: 10.1594/pangaea.611365
title: Composition, abundance and biomass of the main groups of benthic organisms in the flood-plain lake on Samoylov Island
DOI: 10.1594/pangaea.776608
title: A 1.2.3. Data of the batch experiments with the fine fraction of harbour sediments - trace elements
DOI: 10.1594/pangaea.833635
title: Taxonomic lists and abundances of the Lower Miocene bivalve assemblages of the Vives quarry (Meilhan, SW France)

description: Biodiversity estimates through geological times are difficult because of taphonomic perturbations that affect sedimentary records. Pristine shell assemblages, however, allow for calibration of past diversity. Diversity structures of two exceptionally preserved Miocene bivalve assemblages are quantitatively determined, compared with recent communities and used as paleoenvironmental proxy. The extremely rich assemblages were collected in Aquitanian (Early Miocene) carbonate sands of the Vives Quarry (Meilhan, SW France). Both paleontological and sedimentological data indicate a coral patch-reef environment, which deposits were affected by transport processes. Among two samples more than 28.000 shells were counted and 135 species identified. Sample Vives 1 is interpreted as a proximal debris flow and Sample Vives 2 as a sandy shoreface/foreshore environment influenced by storms. The two Vives assemblages have a similar diversity structure despite facies differences. Rarefaction curves level off at ~600 shells. The rare species account for more than 80 % of the species pool. The high values of PIE diversity index suggest a relatively high species richness and an even distribution of abundance of the most common species within the assemblages.The fossil data are compared to death shell assemblages (family level) of a modern reefal setting (Touho area, New Caledonia). The shape of the rarefaction curves and PIE indices of Meilhan fossil assemblages compare well to modern data, especially those of deep (&gt;10 m water depth), sandy depositional environments found downward the reef slope (slope and pass settings). In addition to primary ecological signals, the similarity of the Vives samples and the Recent deep samples derives from taphonomic processes. This assumption is supported by sedimentological and paleontological observations. Sediment transports gather allochthonous and in situ materials leading to mixing of various ecological niches. Such taphonomic processes are recorded in the diversity metrics. Environmental mixing and time-averaging of the shell assemblages disturb the preservation of local-scale diversity properties but favour the sampling of the regional-scale diversity.
DOI: 10.1594/pangaea.861253
title: Sea surface temperature reconstruction for sediment core GeoB7926-2

description: Dataset was corrected on 2018-05-29, columns for TEX86- and UK'37-temperatures were switched in the old version.
DOI: 10.1594/pangaea.901254
title: Apatite fission track (AFT) age analyses of sample MAU-08 from a Precambrian crystalline basement in Mauretania

description: Zeta: Traditionalzeta: 348.18sig zeta: 6.5rho-d (N/cm**2): 1150000Nd: 3462
DOI: 10.1594/pangaea.855331
title: Chemical composition of a P2O5 rich concretion from the Challenger expedition, Station 143 off Cape of Good Hope

description: Among the geological discoveries of the end of the 19th century, one of the most remarkable and certainly most important from the economic point of view, is that lime phosphate deposits have been recorded at various levels in a great many fields. The subsequent development given to the phosphate industry by that of agriculture needs have attracted a great interest in phosphate deposits. This, interest quickly developed for the phosphatic concretions dredged durin the Challenger expedition in the vicinity the Cape of Good Hope and in the Indian Ocean in a line drawn South from Africa to Marion Island. This paper describes the sedimentary environment of these finds and measurements of their chemical contents.
description: Samples have been dessicated at 110 °C and futher ignited at about 1000 °C. Acid insoluble part has been seperated using nitric acid.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.
description: Supplement to: Renard, A F (1889): Les concrétions de phosphate de chaux draguées au large du Cap de Bonne-Espérance. Bulletin de l'Académie Royale de Belgique, 3éme Série, 18(12), 641-665
DOI: 10.1594/pangaea.741392
title: Lithology of sediment core ILMEN, Ilmen Lake, Russia

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.833080
title: Stable isotope ratios on bolboforma from Hole 104-642C

description: Specimens picked by Dorothee Spiegler. Isotope data measured by Kyaw Winn in 1986-1988 with the CARBO KIEL Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University, Kiel, Germany.
DOI: 10.1594/pangaea.897514
title: Magnesium/Calcium ratio of Globigerinoides ruber from a long-running sediment trap time series from the northern Gulf of Mexico
DOI: 10.1594/pangaea.901256
title: Apatite fission track (AFT) age analyses of sample MAU-10 from a Precambrian crystalline basement in Mauretania

description: Zeta: Traditionalzeta: 348.18sig zeta: 6.5rho-d (N/cm**2): 1160000Nd: 3490
DOI: 10.1594/pangaea.833298
title: Geochemistry for sediment core MD02-2496

description: Variations in chalcophile and redox-sensitive trace elements are examined at high-resolution intervals from a ~50 kyr long sediment core (MD02-2496) from the Vancouver Island margin. Enrichments of Ag, Cd, Re, U, and Mo above lithogenous levels, signifying sedimentary suboxia and anoxia, occurred during the early Holocene and Bølling/Allerød, and during warm interstadial events of Marine Isotope Stage (MIS) 3. Down-core trace element profiles co-vary with productivity proxy records (opal, CaCO3, and marine organic carbon), and with sedimentary nitrogen isotope ratios, which reflect variably enriched nitrate upwelled from intermediate waters that were transported northward from the Eastern Tropical North Pacific. The similarity of the MD02-2496 record with records from the southern portion of the California Current System (CCS), and to the Greenland ice core oxygen isotope record during warm climate intervals, suggests that sedimentary redox conditions along the California Current responded to local productivity, to North Atlantic climate change and to tropical Pacific surface water processes via long-distance teleconnections. Concentrations of trace elements and productivity proxies were relatively depleted during the Younger Dryas, cool stadial events of MIS 3, and in two episodes of glaciomarine sedimentation from ~14.7 to 30.5 kyr BP (last glacial maximum, LGM), and from 44 to 50.4 kyr BP. Cordilleran Ice Sheet advancement onto the Vancouver Island continental shelf during the LGM led to intervals of increased terrigenous sedimentation and greatly reduced productivity not seen in the southern portion of the CCS, and along with ventilation of North Pacific Intermediate Waters, resulted in brief sedimentary oxic conditions.
description: Age is based on calibrated and interpolated radiocarbon ages. PI of Age and corrected depth is Ingrid Hendy (ihendy@umich.edu).
description: Supplement to: Chang, Alice S; Pedersen, Thomas F; Hendy, Ingrid L (2014): Effects of productivity, glaciation, and ventilation on late Quaternary sedimentary redox and trace element accumulation on the Vancouver Island margin, western Canada. Paleoceanography, 29(7), 730-746
DOI: 10.1594/pangaea.897554
title: Mineral accumulations during the retreat of the Smith Sound ice stream in the early Holocene from sediment core 2001LSSL-014TC
DOI: 10.1594/pangaea.495159
title: Water temperature XBT profiles from cruise K99_1995