cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.841466
title: (Table 2) Stable carbon and oxygen isotope record of benthic foraminifera of eastern Mediterranean Sea sediment cores

description: The paleoproductivity, paleo-oxygenation, and paleohydrographic configuration of the southeastern Mediterranean during the late Holocene was reconstructed on the basis of the isotopic composition of the epibenthic Heterolepa floridana, shallow-endobenthic Uvigerina mediterranea, and the deeper endobenthic Bulimina inflata from two high-resolution cores GA-112 (470 m) and GA-110 (670 m). The Delta d13C between H. floridana and U. mediterranea reveals four intervals of enhanced productivity, from 3.3-2.6, 2.3-1.9, 1.5-1.1, and 0.8-0.4 kyr BP, coinciding with increased nutrient supply by the Nile River. The entire basin was well aerated, with oxygen consumption varying between 1.0 and 3.5 mL O2/L. Oxygen consumption increases toward present day, probably because of higher accumulation of total organic carbon at 1.7 kyr BP, coinciding with the appearance of the mesotropic benthic species. The hydrographic configuration of the basin has changed during the course of the last 3.75 kyr. The Levantine Intermediate Water (LIW) deepens below 470 m between 3.3 and 2.0 kyr, and especially between 2.5 and 2.0 kyr. During the last 1.5 kyr, the LIW becomes shallower than 470 m, similar to the present day. The change in the hydrographic configuration reflects changes in evaporation/precipitation ratio and in temperature.
description: Supplement to: Schilman, Bettina; Almogi-Labin, Ahuva; Bar-Matthews, Miryam; Luz, Boaz (2003): Late Holocene productivity and hydrographic variability in the eastern Mediterranean inferred from benthic foraminiferal stable isotopes. Paleoceanography, 18(3), 1064
DOI: 10.1594/pangaea.847745
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-06)
DOI: 10.1594/pangaea.847325
title: Lithospheric thickness of Pangea

description: Surface wave tomography, using the fundamental Rayleigh wave velocities and those of higher modes between 1 and 4 and periods between 50 and 160 s, is used to image structures with a horizontal resolution of ~250 km and a vertical resolution of ~50 km to depths of ~300 km in the mantle. A new model, PM_v2_2012, obtained from 3×10**6 seismograms, agrees well with earlier lower resolution models. It is combined with temperature estimates from oceanic plate models and with pressure and temperature estimates from the mineral compositions of garnet peridotite nodules to generate a number of estimates of SV(P,T) based on geophysical and petrological observations alone. These are then used to estimate the unrelaxed shear modulus and its derivatives with respect to pressure and temperature, which agree reasonably with values from laboratory experiments. At high temperatures relaxation occurs, causing the shear wave velocity to depend on frequency. This behaviour is parameterised using a viscosity to obtain a Maxwell relaxation time. The relaxation behaviour is described using a dimensionless frequency, which depends on an activation energy E and volume Va. The values of E and Va obtained from the geophysical models agree with those from laboratory experiments on high temperature creep. The resulting expressions are then used to determine the lithospheric thickness from the shear wave velocity variations. The resolution is improved by about a factor of two with respect to earlier models, and clearly resolves the thick lithosphere beneath active intracontinental belts that are now being shortened. The same expressions allow the three dimensional variations of the shear wave attenuation and viscosity to be estimated.
description: Supplement to: Priestley, Keith; McKenzie, Dan (2013): The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle. Earth and Planetary Science Letters, 381, 78-91
DOI: 10.1594/pangaea.756711
title: (Table 12) Ranges of benthic foraminifers through the Miocene in ODP Hole 115-707A

description: Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because benthic foraminifers are not common in most samples, in many instances the numbers represent their true abundance in a sample. Only the bolivinids reached abundances of 6 or greater.
DOI: 10.1594/pangaea.784205
title: Radiosonde measurements from station Izaña (2012-05)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.499366
title: Physical oceanography from BT during cruise U90XX07115B_1957
DOI: 10.1594/pangaea.848030
title: Stratigraphy of the sedimentary sequence in hole GIK14356-1 Krummland, North Germany

description: Project was supported by the German Research Foundation Project No. 1322/1-2.
DOI: 10.1594/pangaea.805077
title: Ozone measurements from station Izaña (2012-12)
DOI: 10.1594/pangaea.756226
title: Stable carbon and oxygen isotope ratios of Uvigerina mediterranea of sediment core MD99-2286
DOI: 10.1594/pangaea.848046
title: Basic measurements of radiation at station Kwajalein (2012-11)
DOI: 10.1594/pangaea.701634
title: Stable isotope composition of Holocene benthic foraminifers of sediment core GeoTu_SL123

description: Sapropel S1 (S1a: 114.5-133 cm; S1b: 96-110 cm)
DOI: 10.1594/pangaea.848048
title: Basic measurements of radiation at station Kwajalein (2012-12)
DOI: 10.1594/pangaea.701633
title: Stable isotope composition of Holocene benthic foraminifers of sediment core GeoTu_SL112

description: Sapropel S1: 220-273 cm
DOI: 10.1594/pangaea.726250
title: (Table 2) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core CHN115-89PC
DOI: 10.1594/pangaea.828318
title: Core summary for IODP Hole 323-U1341B
DOI: 10.1594/pangaea.847746
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-07)
DOI: 10.1594/pangaea.755942
title: Stable carbon and oxygen isotope ratios of planktonic and benthic foraminifera of ODP Hole 115-714B (Table 1)

description: Combined data on benthic foraminifers, siliceous fossils, and stable isotopes depict times of enhanced organic carbon oxidation in the sediments and high primary productivity in the southern Indian upwelling zone during the Miocene. Increased abundance of the diatom productivity index, the Thalassionema group, elevated diatom and uvigerinid abundances, and bolivinid diversity all suggest heightened primary productivity and the development of a mid-depth oxygen minimum between ~17 and 10 Ma.The abundance of bolivinids with large pores and crenulate chamber surfaces may indicate more aerated pore waters in the upper few centimeters of the partly siliceous sediments deposited during the episode of higher primary productivity and increased organic carbon flux around 10 Ma.
description: Supplement to: Boersma, Anne; Mikkelsen, Naja (1990): Miocene-Age primary productivity episodes and oxygen minima in the central equatorial Indian Ocean. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 589-609
DOI: 10.1594/pangaea.924239
title: Ultra-violet measurements from station Izaña (2020-09)
DOI: 10.1594/pangaea.848331
title: Basic measurements of radiation at station Xianghe (2015-01)
DOI: 10.1594/pangaea.815300
title: (Table 2) Distribution of calcareous nannofossil species at DSDP Hole 25-245A

description: Abundance - V = very abundant, (more than 10 specimens/field of view); A = abundant, (1 to 10 specimens/field of view); C = common, (1 specimen/2-10 fields of view); F = few, (1 specimen/11-100 fields of view); R = rare, (1 specimen/101-1000 fields of view); - = none found. Preservation - P = poor, M = moderate, G = good. Samples 25-245A-5-1,107-109; 25-245A-2-5,98-100; 25-245A-1-2,45-47; 25-245A-1-6,85-86 and 25-245A-2-1,75-77 were barren.
DOI: 10.1594/pangaea.848332
title: Basic measurements of radiation at station Xianghe (2015-05)
DOI: 10.1594/pangaea.676721
title: (Figure 4) Stable oxygen isotope ratios of benthic foraminifera from sediment core Alkor_159_225514 from the Skagerrak, North Sea

description: Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)
DOI: 10.1594/pangaea.847743
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-04)
DOI: 10.1594/pangaea.847747
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-08)
DOI: 10.1594/pangaea.884646
title: Benthic foraminiferal isotope ratios of IODP Site 339-U1390
DOI: 10.1594/pangaea.847748
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-09)
DOI: 10.1594/pangaea.847749
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-10)
DOI: 10.1594/pangaea.773168
title: Ultra-violet measurements from station Izaña (2011-11)
DOI: 10.1594/pangaea.847750
title: Continuous meteorological observations in high-resolution (1Hz) at University of Oldenburg (2014-11)
DOI: 10.1594/pangaea.464586
title: (Appendix 1) Benthic foraminiferal abundance and diversities of DSDP Hole 90-594

description: Further relevant data sets: Nelson et al. (1986) doi:10.1594/PANGAEA.688744, Dersch and Stein (1991) doi:10.1594/PANGAEA.667464, Dudley and Nelson (1994) doi:10.1594/PANGAEA.688785, Kowalski and Meyers (1997) doi:10.1594/PANGAEA.696438, Wells and Okada (1997) doi:10.1594/PANGAEA.681280, Weaver et al. (1998) doi:10.1594/PANGAEA.691461
DOI: 10.1594/pangaea.848349
title: Zooplankton egg counts from METEOR cruise M87/1 in April 2012

description: Zooplankton samples were taken in five depth strata using a Multinet type Midi, with 50 µm nets. The samples were taken during the second leg only, three times at station 1, two times at station 2 and once at station 3. Zooplankton were identified to species / genus and life-stage, and at least 300 individuals were counted per sample. 10 individuals of each stage / species were measured and the numbers of eggs counted.
DOI: 10.1594/pangaea.884654
title: Salinity reconstruction based on Mg/Ca ratios for IODP Site 339-U1390
DOI: 10.1594/pangaea.879500
title: Daily mean stream temperatures at station Piron3, Central Spain
DOI: 10.1594/pangaea.806032
title: Rock magnetic properties of sediment core ROD11-1
DOI: 10.1594/pangaea.826435
title: P-Wave velocity (PWL) from IODP Hole 329-U1367C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.848204
title: Basic measurements of radiation at station Camborne (2008-05)
DOI: 10.1594/pangaea.676736
title: (Appendix III.3) Stable oxygen isotope ratios of benthic foraminifera from sediment core Alkor_159_225510 from the Skagerrak, North Sea

description: Further relevant data sets: Brückner and Mackensen (2007) doi:10.1594/PANGAEA.676719. Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)
DOI: 10.1594/pangaea.757159
title: (Table 3) Organic carbon and reduced sulfur in sediments of DSDP Hole 117-722A
DOI: 10.1594/pangaea.789403
title: Ozone measurements from station Izaña (2012-09)
DOI: 10.1594/pangaea.682701
title: (Appendix 3, Table 4) Relative abundances of benthic foraminifera in Late Quaternary sediments of core BMR96GC21 in the southeast Indian Ocean
DOI: 10.1594/pangaea.848658
title: Extensive management of field margins enhances their potential to mitigate soil erosion

description: Soil erosion is a widespread problem in agricultural landscapes, particularly in regions with strong rainfall events. Vegetated field margins can mitigate negative impacts of soil erosion by trapping eroded material. In this data set, we present data of sediment trapped by 12 field margins during the monsoon season of 2013 in an agricultural landscape in the Haean-myun catchment in South Korea. Prior to the beginning of monsoon season, we equipped a total of 12 sites representing three replicates for each of four different types of field margins ("managed flat", "managed steep", "natural flat" and "natural steep") with Astroturf mats with a size of 34 cm x 25 cm (850 cm**2). The mats (n = 15 / site) were installed at three levels: upslope, immediately before the field margin to quantify the sediments that reach it, in the middle of the field margin to quantify the locally trapped sediments, and after the field margin at the downslope edge to quantify the sediments that leave the field margin to the next field or to the stream. Sediment was collected after each rain event until the end of the monsoon season.
description: Supplement to: Ali, Hamada E; Reineking, Björn (2016): Extensive management of field margins enhances their potential for off-site soil erosion mitigation. Journal of Environmental Management, 169, 202-209
DOI: 10.1594/pangaea.676726
title: (Appendix III.1) Relative abundance of benthic foraminifera in sediment core Alkor_159_225510 from the Skagerrak, North Sea

description: Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)
DOI: 10.1594/pangaea.858633
title: Table 1. Living foraminiferal taxa in the box core PO287-26-1B (no/86cc)
DOI: 10.1594/pangaea.874630
title: (Tables 5, page 8) Beryllium10-Beryllium9 study of layers inside a manganese nodule of the South China Sea

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.848322
title: Basic measurements of radiation at station Xianghe (2014-11)
DOI: 10.1594/pangaea.806333
title: (Table 2b) Relative abundance of diatoms (Chaetoceros spp. resting spore-free) in sediment core MD03-2597

description: Slides were prepared in a beaker with a diameter of 10 cm and the area of the microscope field of view used during counting was 0.000356 cm. The Hyalochaete Chaetoceros spp. resting spore (CRS)-free count allows trends of less common, but ecologically important, species to be revealed.
DOI: 10.1594/pangaea.815219
title: (Table 2) Spores and pollen in Jurassic sediments at DSDP Hole 36-330
DOI: 10.1594/pangaea.694829
title: Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station FEBR-1999-IR16

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.884651
title: Clumped salinity reconstruction for IODP Site 339-U1390
DOI: 10.1594/pangaea.810704
title: (Table 22) Benthic foraminifera in Pliocene sediments of DSDP Hole 90-594

description: Abundances: X = present, A = very abundant, - = absent.
DOI: 10.1594/pangaea.704768
title: (Table 1) Chemical and isotope compositions of interstitial water in sediments from Mediterranean basin at DSDP Site 42-374
DOI: 10.1594/pangaea.857984
title: Stable isotope record of benthic foraminifera of sediment core Vi-37GC
DOI: 10.1594/pangaea.701202
title: (Table A4) Stacked stable isotope record of sediment cores from the North Atlantic

description: Stacked isotope signals of sediment core V30-97 (Latitude 41, Longitude -32.93, water depth 3371 m) and CHN82-24-4 (Latitude 43, Longitude -30, water depth 3070 m). Oxygen isotope signal adjusted to Uvigerina, carbon isotope signal adjusted to Cibicidoides
DOI: 10.1594/pangaea.755338
title: (Table 7) Absolute abundance of silicoflagellates from ODP Hole 114-703A

description: &lt;1 = very rare, found only after completion of census count of 300 specimens.
DOI: 10.1594/pangaea.920945
title: Organic matter composition of the water column in mesocosm study (Svalbard 2010)

description: During the ocean acidification study in Svalbard (2010) we measured concentrations of dissolved organic carbon (DOC) and nitrogen (DON) as well as concentrations of total and dissolved amino acids and carbohydrates including individual compounds in mesocosms.
DOI: 10.1594/pangaea.756707
title: (Table 9) Ranges of benthic foraminifers through the Oligocene in ODP Hole 115-710A

description: Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because benthic foraminifers are not common in most samples, in many instances the numbers represent their true abundance in a sample. Only the bolivinids reached abundances of 6 or greater.
DOI: 10.1594/pangaea.860881
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE457, Kiel - Kiel, 2016-02-26 - 2016-03-10
DOI: 10.1594/pangaea.815206
title: (Appendix S2 Table 1) Species list of lichen, bryophytes and vascular plants around Abisko, Sweden and Toolik lake, Alaska

description: + = found, - = not found.
DOI: 10.1594/pangaea.848428
title: Basic measurements of radiation at station Camborne (2008-10)
DOI: 10.1594/pangaea.903353
title: Calcareous nannofossils absolute abundance and accumulation rates from Holywell Pinnacle, England
DOI: 10.1594/pangaea.825475
title: (Table S1) Foraminiferal trace element ratios from ODP 177-1090D and sediment core TTN057-6-PC4

description: Sediment depth is given in mcd, age is tuned to the LR04 benthic d18O stack.
DOI: 10.1594/pangaea.727105
title: Radiosonde measurements from station Izaña (2009-08)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.924896
title: Daily mean water discharge in Algedonda river in the Grønfjorden area
DOI: 10.1594/pangaea.924899
title: Daily mean water discharge in Bryde river in the Grønfjorden area
DOI: 10.1594/pangaea.903383
title: Calcareous nannofossils absolute abundance and accumulation rates from Punta Grande/Punta Piccola, Italy
DOI: 10.1594/pangaea.860346
title: Ultra-violet measurements from station Izaña (2016-04)
DOI: 10.1594/pangaea.924904
title: Daily mean water discharge in Vasstak river in the Grønfjorden area
DOI: 10.1594/pangaea.924830
title: Median iGDGT fractional abudances in modern peats, modern peats above 15ºC and Paleogene lignites
DOI: 10.1594/pangaea.752579
title: Meteorological observations during UNKNOWN-06 cruise from Soerabaija to Rotterdam started at 1848-06-27
DOI: 10.1594/pangaea.810305
title: (Table 2) Toxaphene, chlorobornane and chlorobornane congener content in blubber of minke whales (Balaenoptera acutorostrata)

description: DATE/TIME to Date/Time end is the sampling period. Concentrations given per g lipid weight.
DOI: 10.1594/pangaea.924900
title: Daily mean water discharge in Grøndalen river in the Grønfjorden area
DOI: 10.1594/pangaea.924901
title: Daily mean water discharge in Grønfjorddalen river in the Grønfjorden area
DOI: 10.1594/pangaea.924902
title: Daily mean water discharge in Kongress river in the Grønfjorden area
DOI: 10.1594/pangaea.925155
title: Diatom isotopes of ODP Site 145-887 (Table S2)
DOI: 10.15468/dl.t4kbub
title: Occurrence Download

description: A dataset containing 2845 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is South America",
 "TaxonKey is Meteoridium remotifolium (Müll.Hal.) Manuel"
 ]
}

 The dataset includes 2845 records from 113 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031290-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.847297
title: Bottom water data time series at benthic lander NuSOB station HE395/38-2

description: The datasets were obtained by a CTD (Sea & Sun) mounted 1 meter above the seafloor on the lander frame.
DOI: 10.1594/pangaea.875598
title: (Table 4A) Porewater and sediment geochemistry of sediment core Trout_Creek
DOI: 10.1594/pangaea.925156
title: Salinity reconstructions of ODP Site 145-887 (Table S3)
DOI: 10.1594/pangaea.897293
title: Inorganic nutrient measured during Maria S. Merian cruise MSM21/3 (ARCHEMHAB)
DOI: 10.1594/pangaea.806335
title: (Table 4) Description of visually conspicuous diatom species in laminae of sediment core MD03-2597

description: RS: resting spores; CRS: Hyalochaete Chaetoceros spp. resting spores; veg: vegetative. BSEI = backscattered electron imagery and SEI = secondary electron imagery scanning electron microscopy.
DOI: 10.1594/pangaea.907155
title: Environmental data layers and R script for estimating giant panda distribution

description: Included is the R script used in the analyses done in the paper. The environmental data layers used in these analyses are available upon request - they are publically available but we can save you time in the download/processing. The files are very large and cannot be uploaded here, however. Giant panda presence data is restricted due to their threatened status. Get in touch with us to see if we can get you access to some or all.
DOI: 10.1594/pangaea.889194
title: Documentation of sediment core GeoB17721-1
DOI: 10.1594/pangaea.914257
title: Petrographic observations and phase properties for sample sets from Wadi Somerah (OM10-Sam) and Wadi Wariyah (OM10-War), Oman

description: As largest and best-exposed paleo-fast-spread oceanic crust on land, the Samail ophiolite in the Sultanate of Oman represents an ideal natural laboratory for investigating processes at fast-spreading mid-ocean ridges. We studied two layered gabbro sequences from different stratigraphic depths: one from the middle of the plutonic crust showing dm-scale modal layering with olivine abundance gradually decreasing from layer base to top (Wadi Somerah, Sumail block) and one located near the crust-mantle boundary showing mm-scale layers being enriched in olivine (Wadi Wariyah, Wadi Tayin block). Petrographic analyses were performed at the Institut für Mineralogie (Leibniz Universität Hannover, Germany) for thin-section description. Plagioclase and Clinopyroxene are present in all samples, most of the samples also include olivine as primary phase and are therefore described as olivine gabbro. The olivine content increases per layer towards the layer base. Grain sizes of the three primary phases olivine, plagioclase and clinopyroxene vary between 0.2 and 5 mm. Olivine usually forms the largest grains, plagioclase the smallest ones. The grain shapes are generally subhedral, their habit is prismatic or, occasionally, irregular or elongated. Some olivine grains show reaction rims or contain plagioclase chadacrysts. Poikilitic clinopyroxene also containing plagioclase as chadacrysts is very common. The described phases are only the primary minerals not taking the low to medium degree of alteration and therefore presence of secondary phases into account.
description: OM10-Sam: layer 6= 0-8 cm, layer 5= 8-57 cm, layer 4= 57-95 cm, layer 3= 95-136 cm, layer 2= 136-205 cm, layer 1= 205-285 cmOM10-War: layer 1= 0-0.7 cm, layer 2= 0.7-1.5 cm, layer 3= 1.5-2.1 cm, layer 4= 2.1-2.6 cm, layer 5= 2.6-3.2 cm, layer 6= 3.2-3.9 cm, layer 7= 3.9-4.3cm, layer 8= 4.3-5 cm, layer 9= 5-5.8 cm, layer 10= 5.8- 6.3 cm, layer 11= 6.3-7.2 cm