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  • PANGAEA  (247)
  • 2020-2024  (247)
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  • 1
    Publication Date: 2023-12-12
    Description: 14C and 210Pb age determination of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
    Keywords: Age; Age, 14C uncalibrated; Age, dated; Age, dated material; Age, uncertainty; BLL; Borralleiras_da_Cal_Grande; calculated, 1 sigma; Comment; C-PEAT; DEPTH, sediment/rock; Laboratory code/label; PAGES_C-PEAT; Past Global Changes - Carbon in Peat on EArth through Time; PEATC; Peat corer; Peatland; Sample thickness; Spain
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 2
    Publication Date: 2023-12-12
    Description: Calibrated ages of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
    Keywords: Age, 14C calibrated, Bacon 2.2 (Blaauw and Christen, 2011); Age, 14C calibrated, OxCal 4.2.4, P sequence deposition model; BLL; Borralleiras_da_Cal_Grande; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; C-PEAT; DEPTH, sediment/rock; PAGES_C-PEAT; Past Global Changes - Carbon in Peat on EArth through Time; PEATC; Peat corer; Peatland; Spain
    Type: Dataset
    Format: text/tab-separated-values, 366 data points
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  • 3
  • 4
    Publication Date: 2023-03-14
    Description: In this work we used controlled microcosms to study the effect of temperature and pH on brGDGTs in lake water. We collected surface water from Kennedy Lake, Tucson, AZ, a shallow eutrophic artificial reservoir previously described by Martínez-Sosa & Tierney (2019). From the collected samples we set up a series of microcosms, consisting of 1L glass flasks filled with lake water, and manipulated single environmental factors including temperature and pH. For our temperature incubations, we selected four conditions (9C, 18C, 27C and 35C) and incubated 3 1L flasks under each condition for two periods of time (4 or 6 weeks). For the pH incubations, we used commercially available freshwater aquarium non-phosphate buffers (Proprietary composition, Seachem, Madison, GA, USA) to manipulate the pH of the microcosms. For these experiments we targeted four pH conditions (4, 5, 6 and 7), and included two control samples: one where we added enough buffer to maintain the initial pH (Control + Buffer), and another to which we added no buffer (Control - Buffer). GDGTs were analyzed on an Agilent 1260 Infinity HPLC coupled to an Agilent 6120 single quadrupole mass spectrometer using two BEH HILIC silica columns (2.1 x 150 mm, 1.7 um; Waters) and the methodology of Hopmans et al. (2016). We calculated peak areas using the MATLAB package software ORIGAmI (Fleming et al. 2016) and estimated the concentration of brGDGTs by comparing the obtained peaks with a C46 internal standard (Huguet et al. 2006) normalized to the volume of each sample.
    Keywords: Branched glycerol dialkyl glycerol tetraether; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIa'; Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIb'; Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIa'; brGDGTs; Calculated; Cyclization ratio of branched tetraethers; Degree of cyclisation; Experiment; Incubation duration; Isomer ratio; Kennedy_Lake_water_microcosm; Laboratory experiment; lakes; Methylation index of 5-methyl branched glycerol dialkyl glycerol tetraether; microcosms; pH; Sample ID; Standard deviation; Temperature; Temperature, water; Tucson, Arizona, USA
    Type: Dataset
    Format: text/tab-separated-values, 528 data points
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  • 5
    Publication Date: 2023-03-14
    Description: A high-resolution carbonate C-isotope (δ13Ccarb) stratigraphy for the Aptian is presented for the Cau core from Alicante, Spain. The studied succession, lower to upper Aptian, embraces the record of the Early Aptian OAE 1a. The data provided includes δ13Ccarb, δ18O isotopes, Total Organic Carbon (TOC) and CaCO3. Four overlapping cores (D1 to D4) were drilled with an almost 100% recovery of a total (corrected for dip) thickness of 143 m. The cores were split in two parts. One half was described, photographed and scanned, and then sampled with a drill to obtain powdered samples for geochemical analyses. Also, small solid samples were taken from the drill for biostratigraphic characterization of the nannofossil and planktonic foraminifera associations. Second half was stored for archive and future research.
    Keywords: Almadich formation; Aptian; Automatic calcimeter (DREAM Électronique SAS , Pessac, France); Calcium carbonate; C and O isotopes; Carbon, organic, total; Cau_Core-D1; Cau_Core-D2; Cau_Core-D3; Cau_Core-D4; Cau-core; CO3Ca; DEPTH, sediment/rock; Event label; Hemipelagic sedimentation; Mass spectrometer, Finnigan, MAT 253; coupled with Carbonate preparation device, Finnigan, KIEL IV; OAE 1a; RDC; Rock drill core; Sample ID; Shimadzu TOC-V CSH total organic carbon analyzer; TOC; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 3121 data points
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  • 6
    Publication Date: 2023-01-30
    Description: Supplementary material for Martínez Fontaine et al., 2021: Post–glacial tephrochronology record off the Chilean continental margin (~41° S). Including: Table S1.- Globigerina bulloides δ18O and the resulting age model for core MD07-3098 with its respective 1σ and 2σ envelopes. Table S2. Inividual glass shard analyses in core MD07-3100. Major elements not normalized‚ analyzed by EPMA‚ trace elements analyzed by LA-ICP-MS. Table S3. Inividual glass shard analyses in core MD07-3098. Major elements, not normalized, analyzed by EPMA. Table S5.- Planktonic foraminifera radiocarbon ages from core MD07-3098 and the respective marine surface reservoir age correction applied (Rs) in the calibration.
    Keywords: chilean margin; Marine Sediment Core; post-glacial; tephrochronology
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 7
    Publication Date: 2023-01-30
    Description: The dataset contains counts of meiofauna organisms on high taxonomic level and predicted distributions computed for overall meiofauna abundance, diversity (Simpson's Index D and Evenness E), richness (ntax) and individual taxa using random forest regressions. Furthermore, a habitatmap is provided, dividing the area based on k-means clustering of combined predicted distributions, bathymetry and backscatter. The spatial layers are saved as grid-files, being the standard format of the R-package "raster" (https://cran.r-project.org/web/packages/raster/index.html). Study area is an area allocated to the German Federal Institute for Geosciences and Natural Resources for the exploration of polymetallic nodule mining. Deep-sea mining highly endangers the benthic communities; hence the definition of preservation zones, not only for preservation but also to enable the re-settlement of mined areas, is highly important. These datasets on the spatial distribution of meiofauna have been used to account for a modelling approach to find areas with similar environmental conditions and similar benthic communities.
    Keywords: distribution model; Habitat Mapping; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; meiofauna; random forest regression
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
    Publication Date: 2023-01-30
    Description: The dataset contains predicted distributions computed for overall meiofauna abundance, diversity (Simpson's Index D and Evenness E), richness (ntax) and individual taxa using random forest regressions. Furthermore, a habitatmap is provided, dividing the area based on k-means clustering of combined predicted distributions, bathymetry and backscatter.
    Keywords: CCZ_GER; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; distribution model; Habitat Mapping; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; meiofauna; random forest regression
    Type: Dataset
    Format: application/zip, 8.9 MBytes
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  • 9
    Publication Date: 2023-06-22
    Description: The data of two sections studied in the Barremian (Early Cretaceous) of the Subbetic Domain (SE Spain) are shown here together with a detailed log showing the bed number and the biostratigraphic scheme. The samples were collected with a geologist hammer in May 2016. The average sample distance is 0.07 m and was kept as constant as possible using a Jacob's staff to ensure the detection of all the Milankovitch cycles applying Fast Fourier Transforms and related methods (e.g. multi-taper). The lithology is composed of marl-limestone alternations deposited in a (hemi-)pelagic setting. Observed fauna is composed of ammonites, radiolarians, foraminifera, calcareous nannofossils and scarce belemnites, bivalves, gastropods, brachiopods and irregular echinoids. The biostratigraphy scheme is provided in the detailed logs and is based on Tethyan ammonite and calcareous nannofossils. The interval studied of Barranco de Cavila section (38°3'10'' N; 1°53'20'' W) covers from the Late Barremian (Vandenheckii Zone) to the Early Aptian (Forbesi Zone). Carbon and oxygen isotope ratios were measured with a Wahlen VG Prism II mass spectrometer. The mass spectrometer was calibrated with three NBS standards, Nos. 18, 19 and 20
    Keywords: Barranco_de_Cavila_Section; Barremian; CaCO3 content; carbon isotope ratios; Cretaceous; Level; magnetic susceptibility; Mass spectrometer VG Prism Series II; Murcia, Spain; oxygen isotope ratios; Sample ID; Subbetic Domain; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 188 data points
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  • 10
    Publication Date: 2023-06-22
    Description: The data of two sections studied in the Barremian (Early Cretaceous) of the Subbetic Domain (SE Spain) are shown here together with a detailed log showing the bed number and the biostratigraphic scheme. The samples were collected with a geologist hammer in May 2016. The average sample distance is 0.07 m and was kept as constant as possible using a Jacob's staff to ensure the detection of all the Milankovitch cycles applying Fast Fourier Transforms and related methods (e.g. multi-taper). The lithology is composed of marl-limestone alternations deposited in a (hemi-)pelagic setting. Observed fauna is composed of ammonites, radiolarians, foraminifera, calcareous nannofossils and scarce belemnites, bivalves, gastropods, brachiopods and irregular echinoids. The biostratigraphy scheme is provided in the detailed logs and is based on Tethyan ammonite and calcareous nannofossils. The two sections studied are Arroyo Gilico section (38°9'35'' N; 1°40'41'' W; the interval studied covers from the Late Hauterivian (Balearis Zone) to the Late Barremian (Vandenheckii Zone)) and Barranco de Cavila section (38°3'10'' N; 1°53'20'' W; the interval studied covers from the Late Barremian (Vandenheckii Zone) to the Early Aptian (Forbesi Zone)).Magnetic susceptibility was measured with a KLY-3 and calcium carbonate content was measured following the volumetric method using the automatic calcimeter Dream Electronique
    Keywords: ARM, Susceptibility, per unit mass; Arroyo_Gilico_Section; Barranco_de_Cavila_Section; Barremian; CaCO3 content; Calcium carbonate; carbon isotope ratios; Cretaceous; Event label; Kappabridge, AGICO KLY-3; Level; magnetic susceptibility; Murcia, Spain; oxygen isotope ratios; Sample ID; Subbetic Domain; Volumetric method using the automatic calcimeter Dream Electronique
    Type: Dataset
    Format: text/tab-separated-values, 8099 data points
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