cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.785475
title: (Table 1) Biostratigraphic datums of ODP Leg 133 sites

description: We use benthic foraminifers to reconstruct the Neogene paleobathymetric history of the Marion Plateau, Queensland Plateau, Townsville Trough, and Queensland Trough on the northeastern Australian margin (Ocean Drilling Program Leg 133). Western Queensland Plateau Site 811/825 (present depth, ~938 m) deepened from the neritic zone (0-200 m) to the upper bathyal zone (200-600 m) during the middle Miocene (~13-14 Ma), with further deepening into the middle bathyal zone (600-1000 m) occurring during the late Miocene (~7 Ma). A depth transect across the southern Queensland Plateau shows that deepening from the outer neritic zone (100-200 m) to the upper bathyal zone began during the latest Miocene (~6 Ma) at the deepest location (Site 813, present depth, 539.1 m), whereas the shallower Sites 812 and 814 (present depths, 461.6 and 520.4 m, respectively) deepened during the late Pliocene (~2.7 and ~2.9 Ma). At Marion Plateau Site 815 (present depth, 465.5 m), water depth increased during the late Miocene (~6.7 Ma) from the outer neritic to the upper bathyal zone. Nearby Site 816 (present water depth, 437.3 m) contains Pliocene upper bathyal assemblages that directly overlie middle Miocene shallow neritic deposits; the timing of the deepening is uncertain because of a late Miocene hiatus. On the northern slope of the Townsville Trough (Site 817, present depth, 1015.8 m), benthic foraminifers and sponge spicules indicate deepening from the lower upper bathyal (400-600 m) to the middle bathyal zone in the late Miocene (by ~6.8 Ma). Benthic foraminiferal faunas at nearby Site 818 (present water depth, 752.1 m) do not show evidence of paleobathymetric change; however, a late Pliocene (~2-3 Ma) increase in downslope transport may have been related to the drowning of the Queensland Plateau. Site 822 (present depth, 955.2 m), at the base of the Great Barrier Reef slope, deepened from the upper bathyal to the middle bathyal zone during the late Pliocene (by ~2.3 Ma). Queensland Trough Site 823 (present depth, 1638.4 m) deepened from the middle bathyal to the lower bathyal (1000-2000 m) zone during the late Miocene (~6.5 Ma). Benthic foraminiferal faunal changes at these Leg 133 sites indicate that rapid deepening occurred duringthe middle Miocene (~13-14 Ma), late Miocene (6-7 Ma), and late Pliocene (2-3 Ma) along the northeastern Australian margin.
description: Supplement to: Katz, Miriam E; Miller, Kenneth G (1993): Neogene subsidence along the northeastern Australian Margin: benthic foraminiferal evidence. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 75-92
DOI: 10.1594/pangaea.724278
title: Other measurements at 10 m from station Southern Great Plains (2008-05)
DOI: 10.1594/pangaea.845095
title: Pore water chloride concentrations of sediment core GMMB01

description: Sample code GMMB01 = GMMB01 & 02
DOI: 10.1594/pangaea.886898
title: Empiric pollen record from lake Tiefer See for testing and illustrating the ROPES approach
DOI: 10.1594/pangaea.862293
title: GPS-derived precipitable water vapor content calculated for station KAT1
DOI: 10.1594/pangaea.886897
title: Pollen accumulation rates from lake Tiefer See for testing and illustrating the ROPES approach
DOI: 10.1594/pangaea.845104
title: Pore water chloride concentrations of sediment core GMMB05
DOI: 10.1594/pangaea.883642
title: Holocene inorganic geochemical data from Borreguil de la Caldera (S Spain)

description: This dataset includes bulk sediment inorganic data: Al, Si, S, K, Ca, Ti, Fe, Zr, Br, Rb, and Sr (measured using X-ray scanning fluorescence ? XRF core scanner), and Hg (analysed by means of a mercury analyser).
DOI: 10.1594/pangaea.901491
title: Beach profile data for the Elwha River Delta, 2011-05-16

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.883649
title: Holocene organic geochemical data from Laguna de Rio Seco (S Spain)

description: This dataset includes bulk sediment organic data: total organic carbon (TOC), total nitrogen (TN), atomic carbon - nitrogen ratio (C/N), carbon isotopic composition (13C), and nitrogen isotopic composition (15N). They were measured by means of isotope-ratio mass spectrometry (IRMS) with a coupled elemental analyser (EA).
DOI: 10.1594/pangaea.887040
title: Calcium carbonate and inorganic carbon in the western Arabian Gulf
DOI: 10.1594/pangaea.752770
title: Meteorological observations during Vrouwe Cornelia Hillegonda cruise from Batavia to Bengalen started at 1767-07-31
DOI: 10.1594/pangaea.901492
title: Beach profile data for the Elwha River Delta, 2011-05-17

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
description: Portions of these data have been published previously, including in Gelfenbaum et al. 2015.
DOI: 10.1594/pangaea.878051
title: Loss on ignition of Lake Verney sediment core
DOI: 10.1594/pangaea.761490
title: Meteorological synoptical observations from station Lindenberg (2006-12)
DOI: 10.1594/pangaea.907022
title: Caesium 137 liquid releases from La Hague nuclear plant

description: Liquid caesium 137 releases from La Hague nuclear plant reaching the north-west European seas since the beginning of operation. Releases are given annually.
DOI: 10.1594/pangaea.747511
title: Meteorological observations during ASIA cruise from Madras to Madagascar started at 1780-04-25
DOI: 10.1594/pangaea.912473
title: Radiosonde measurements from station Budapest (2019-06)
DOI: 10.1594/pangaea.664224
title: Oceanography at CTD/bottle station IFREMER_1065
DOI: 10.1594/pangaea.913960
title: Radiosonde measurements from station Payerne (2020-01)
DOI: 10.1594/pangaea.750710
title: Meteorological observations during MENTOR cruise from Batavia to Ierland started at 1795-01-13
DOI: 10.1594/pangaea.870036
title: Links to master tracks in different resolutions from POLAR 2 flight EMAGE-IV_06
DOI: 10.1594/pangaea.722399
title: Other measurements at 10 m from station Goodwin Creek (2002-08)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.664028
title: Oceanography at CTD/bottle station IFREMER_0869
DOI: 10.1594/pangaea.748812
title: Meteorological observations during El Aguila cruise from Montevideo to Islas Malvinas started at 1768-01-02
DOI: 10.1594/pangaea.664794
title: Oceanography at CTD/bottle station IFREMER_1634
DOI: 10.1594/pangaea.736379
title: Ozone measurements from Neumayer Station (2009-04)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.603894
title: Hydrographic and chemical measurements at anchor station M8_065-2b of the eastern North Atlantic (Table 1)
DOI: 10.1594/pangaea.868906
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 14 (Sites 14-135, 14-136, 14-137, 14-141)

description: Leg 14 of the Deep Sea Drilling Project completed 9 holes; 7 were located off NW Africa, 1 in Ceara Abyssal Plain, and 1 on Demerara Rise. Quaternary and Pliocene sediments consist of nanno chalk oozes and brown clay. The facies boundary (CCD) is near 5000 meters. Sedimentation rates are between 10 and 30 meters/million years (m/My) for chalk ooze and 2 to 4 m/My for pelagic clay. Redeposition off the Amazon produces terrigenous and bioclastic turbidite sequences with rates increasing, on the average, from 50 to 150 m/My. Small manganese nodules (coarse sand and small pebbles) are common in sediments associated with hiatuses at Sites 135 (Eocene-Miocene, Core SW1), 136 (Late Cretaceous- Miocene, Cores 3 to 6), and to a lesser extent at 141 (Middle Miocene-Pliocene, Core 7). Additional occurrences were noted in the pelagic clays at Site 137 (Late Cretaceous to Miocene). At 135-8 (Cenomanian) micro-nodules occur within a mixture of siltstone fragments, compressed planktonic foraminifera, fish debris, as well as chert pebbles and other redeposited components. Manganese concretions are generally younger than Turonian and are restricted to the predominantly oxidized part of the sequences, that is, where sediments are mostly red, brown, or yellow-colored.
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.
description: Supplement to: Berger, Wolfgang H; von Rad, Ulrich (1972): Cretaceous and Cenozoic Sediments from the Atlantic Ocean. In: Hayes, D.E.; Pimm, A.C.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIV, 787-954
DOI: 10.1594/pangaea.494803
title: Physical oceanography during cruise U06X008038C
DOI: 10.1594/pangaea.733187
title: Physical oceanography during cruise HOT-45 on section PRS2
DOI: 10.1594/pangaea.793156
title: (Table 2) Nd and Sm isotopic composition and model ages of garnet-biotite gneisses in the Ol'khon Group and Anginskaya and Talanchanskaya formations
DOI: 10.1594/pangaea.747406
title: Meteorological observations during ANTELOPE cruise from Lizard to Cruising started at 1760-03-01
DOI: 10.1594/pangaea.752434
title: Meteorological observations during TEMPEL cruise from Texel to Kasseraijen started at 1776-01-02
DOI: 10.1594/pangaea.712796
title: Main and trace element geochemistry of sediment core POS158/1_0016/2
DOI: 10.1594/pangaea.687728
title: Time series of temperature in 2006, Ancón Bay, Peru
DOI: 10.1594/pangaea.810956
title: Basic measurements of radiation at station Nauru Island (2006-06)

description: Version 2, 2013-04-30.
DOI: 10.1594/pangaea.751798
title: Meteorological observations during ROTTERDAM cruise from Rotterdam to Batavia started at 1840-02-18
DOI: 10.1594/pangaea.737276
title: Sea surface temperature reconstruction from sediment core SU81-18 using alkenones
DOI: 10.1594/pangaea.499687
title: Physical oceanography from BT during cruise UXXXX00420B_1975
DOI: 10.1594/pangaea.701089
title: Hydrochemistry measured on water bottle samples during DISCOVERY cruise D285 (74E320041103)
DOI: 10.1594/pangaea.809045
title: (Table 12) Dry-bulk density and CaCO3 content for sediment core V28-153
DOI: 10.1594/pangaea.863363
title: Daily mean meteorology at station IMS, 2001-2012
DOI: 10.1594/pangaea.495917
title: Water temperature MBT profiles from cruise U90M_1957
DOI: 10.1594/pangaea.901272
title: Apatite fission track (AFT) length analyses of sample MAU-11 from a Precambrian crystalline basement in Mauretania
DOI: 10.1594/pangaea.495394
title: Water temperature XBT profiles from cruise U31X107860_1988
DOI: 10.1594/pangaea.747145
title: Meteorological observations during ACTIVE cruise from Madeira to Barbados started at 1763-11-28
DOI: 10.1594/pangaea.808251
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 2012
DOI: 10.1594/pangaea.864643
title: Ultra-violet measurements from station Goodwin Creek (2011-12)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.747696
title: Meteorological observations during BOSTON cruise from Madeira to Hampton Road started at 1770-01-20
DOI: 10.1594/pangaea.476326
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/179

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.750671
title: Meteorological observations during MEDWAY cruise from St. Helena to Spithead started at 1782-08-06
DOI: 10.1594/pangaea.712516
title: Calculation of paleoproductivity during the Eocene-Oligocene transition of ODP Site 113-689

description: High-resolution records of carbon and oxygen isotopes and benthic foraminiferal accumulation rates for the Eocene-Oligocene section at Ocean Drilling Program Site 689 (Maud Rise, Weddell Sea; paleodepth about 1500 m) were used to infer variations in paleoproductivity in relation to changes in climate and ventilation of the deeper-water column. The benthic foraminiferal abundance and isotope records show short-term fluctuations at periodicities of 100 and 400 ka, implying orbitally driven climatic variations. Both records suggest that intermediate-depth water chemistry and primary productivity changed in response to climate. During the Eocene, productivity increased during cold periods and during cold-to-warm transitions, possibly as a result of increased upwelling of nutrient-rich waters. In the Oligocene, in contrast, productivity maxima occurred during intervals of low delta18O values (presumably warmer periods), when a proto–polar front moved to the south of the location of Site 689. This profound transition in climate-productivity patterns occurred around 37 Ma, coeval with rapid changes toward increasing variability of the oxygen and carbon isotope and benthic abundance records and toward larger-amplitude delta18O fluctuations. Therefore, we infer that, at this time, temperature fluctuations increased and a proto–polar front formed in conjunction with the first distinct pulsations in size of the Antarctic ice sheet. We speculate that this major change might have resulted from an initial opening of the Drake Passage at 37 Ma, at least for surface- and intermediate-water circulation.
description: Supplement to: Diester-Haass, Lieselotte; Zahn, Rainer (1996): Eocene-Oligocene transition in the Southern Ocean: History of water mass circulation and biological productivity. Geology, 24(2), 163-166
DOI: 10.1594/pangaea.779009
title: (Table T11) Chemical composition of galena in ODP Hole 193-1189B
DOI: 10.1594/pangaea.668377
title: Physical oceanography of CTD station T8 off Independencia Bay, 2003, Peru
DOI: 10.1594/pangaea.499143
title: Physical oceanography from BT during cruise U90X008338B_1986
DOI: 10.1594/pangaea.901249
title: Apatite fission track (AFT) age analyses of sample MAU-02 from a Precambrian crystalline basement in Mauretania

description: Zeta: Traditional zeta: 348.18sig zeta: 6.5rho-d (N/cm**2): 1.16E+06Nd: 3480
DOI: 10.1594/pangaea.901261
title: Apatite fission track (AFT) age analyses of sample MAU-22 from a Precambrian crystalline basement in Mauretania

description: Zeta: Traditionalzeta: 348.18sig zeta: 6.5rho-d (N/cm**2): 1160000Nd: 3471
DOI: 10.1594/pangaea.808852
title: Measured water discharges, suspended supply and morphometric parameters of cross-sections in the Lena River Delta during summer period 2012
DOI: 10.1594/pangaea.761896
title: (Table 6) U, Th, 234U/238U and 230Th/234U values in metal-rich deposits from DSDP Hole 31-294
DOI: 10.1594/pangaea.829049
title: Magnetic remanence from IODP Hole 339-U1391B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.808701
title: Physical oceanography during HEINCKE cruise HE392
DOI: 10.1594/pangaea.720113
title: Radiosonde measurements from station Desert Rock (2001-10)

description: Version 2, 2009-06-16; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.901101
title: Other measurements at 10 m from station Rock Springs (2018-08)
DOI: 10.1594/pangaea.497315
title: Physical oceanography from BT during cruise M90Z6B_1987
DOI: 10.1594/pangaea.819993
title: (Table 9) Minerals of bulk and fine-grained (2 µm) samples from DSDP Site 60-461

description: Sediment depth is given in mbsf. &lt;1 = trace. Carbonate, alkaline feldspar, clinoptilolite, phillipsite, analcime, opal CT, Fe-Mg chlorite, attapulgite and serpentine also looked for but not found.
DOI: 10.1594/pangaea.901265
title: Apatite fission track (AFT) length analyses of sample MAU-03 from a Precambrian crystalline basement in Mauretania
DOI: 10.1594/pangaea.690712
title: Concentrations of chlorophyll-alpha combined with different size fractions of microplankton in sea water from the euphotic zone of the Aegean Sea at Station MARCH-1997-GN36199704603MNB01

description: Samples from 2 l of sea water were size fractionated by filtration through polycarbonate Millipore filters with pores 0.2 µm, 1.2 µm, and 3.0 µm. 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.695093
title: Ciliate abundance in water samples collected at Station MAY-1997-MNB1 in the Aegean Sea

description: For sample preservation borax-buffered formalin (final concentration 2% formaldehyde) has been used. Samples were stored at 4°C in the dark until observation. 100 ml samples have been transferred into Utermohl chambers for settling during 24 hours and finally examined by means of an inverted microscope.
DOI: 10.1594/pangaea.901269
title: Apatite fission track (AFT) length analyses of sample MAU-08 from a Precambrian crystalline basement in Mauretania
DOI: 10.1594/pangaea.747357
title: Meteorological observations during AMPHITRITE cruise from Coastal to Gulf of Guinee started at 1838-07-10
DOI: 10.1594/pangaea.754301
title: Milankovitch frequency peaks of ODP Site 113-693 (Table 3)

description: The first well logs collected below the Antarctic circle were obtained during Leg 113 at Site 693 on the Dronning Maud Land Margin (Antarctica) in the Weddell Sea. Gamma-ray, resistivity, and sonic logs were collected between 108.0 and 439.0 mbsf. The downhole logs show good agreement with the data collected from cores and provide a continuous measurement of the sedimentary record. These continuous log records show that the rather uniform Tertiary lithology seen in cores is characterized by high-frequency variability in the log data. Several thin hard streaks are identified, the largest of which coincides with a major Miocene hiatus. Associated with this hiatus is a change to lower illite content (and correspondingly lower gamma-ray counts) and to a significant increase in diatom content.Spectral analysis of the logs was performed on the lower Pliocene through upper Oligocene interval (108.0-343.0 mbsf). Between 108.0 and 245.0 mbsf, average sedimentation rates (50 and 26 m/m.y.) are high enough to show that variance is present in the orbital eccentricity (~95 k.y.) and obliquity (~41 k.y.) bands. Between 253.0 and 343.0 mbsf, the sedimentation rate (8 m/m.y.) is too low to resolve high frequency variations. The Milankovitch frequencies are best developed in the resistivity logs. Resistivity is responding to changes in porosity, which in these sediments is controlled by the abundance of biosiliceous sediments, particularly diatoms. The orbital forcing suggested by the Milankovitch frequencies may be influencing diatom productivity by inducing oscillations in upwelling, ice coverage, pack ice, and/or polynya. Although variations in diatom abundance were observed in the cores, they were not attributed to a Milankovitch signal, and therefore in this environment, downhole logs are an important contribution to the detection and understanding of orbitally influenced changes in sedimentation.
description: Quality of interval frequency is determined by the presence or absence of the top or near top of an amplitude peak within ± 0.5 m.y. of the predicted frequency. Correlation: G = good, M = moderate, P = poor.
description: Supplement to: Golovchenko, Xenia; O'Connell, Suzanne B; Jarrard, Richard D (1990): Sedimentary response to paleoclimate from downhole logs at Site 693, Antarctic Continental Margin. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 239-251
DOI: 10.1594/pangaea.495261
title: Water temperature MBT profiles from cruise U3190214M_1953
DOI: 10.1594/pangaea.752643
title: Meteorological observations during Van Oldenbarneveld cruise from Rotterdam to Batavia started at 1849-03-20