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  • PANGAEA  (91)
  • Macmillian Magazines Ltd.  (1)
  • Public Library of Science  (1)
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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Microbial expansion following faunal mass extinctions in Earth history can be studied by petrographic examination of microbialites (microbial crusts) or well-preserved organic-walled microbes. However, where preservation is poor, quantification of microbial communities can be problematic. ...
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in PLoS Biology 10 (2012): e1001234, doi:10.1371/journal.pbio.1001234.
    Description: Since the first discovery of deep-sea hydrothermal vents along the Galápagos Rift in 1977, numerous vent sites and endemic faunal assemblages have been found along mid-ocean ridges and back-arc basins at low to mid latitudes. These discoveries have suggested the existence of separate biogeographic provinces in the Atlantic and the North West Pacific, the existence of a province including the South West Pacific and Indian Ocean, and a separation of the North East Pacific, North East Pacific Rise, and South East Pacific Rise. The Southern Ocean is known to be a region of high deep-sea species diversity and centre of origin for the global deep-sea fauna. It has also been proposed as a gateway connecting hydrothermal vents in different oceans but is little explored because of extreme conditions. Since 2009 we have explored two segments of the East Scotia Ridge (ESR) in the Southern Ocean using a remotely operated vehicle. In each segment we located deep-sea hydrothermal vents hosting high-temperature black smokers up to 382.8°C and diffuse venting. The chemosynthetic ecosystems hosted by these vents are dominated by a new yeti crab (Kiwa n. sp.), stalked barnacles, limpets, peltospiroid gastropods, anemones, and a predatory sea star. Taxa abundant in vent ecosystems in other oceans, including polychaete worms (Siboglinidae), bathymodiolid mussels, and alvinocaridid shrimps, are absent from the ESR vents. These groups, except the Siboglinidae, possess planktotrophic larvae, rare in Antarctic marine invertebrates, suggesting that the environmental conditions of the Southern Ocean may act as a dispersal filter for vent taxa. Evidence from the distinctive fauna, the unique community structure, and multivariate analyses suggest that the Antarctic vent ecosystems represent a new vent biogeographic province. However, multivariate analyses of species present at the ESR and at other deep-sea hydrothermal vents globally indicate that vent biogeography is more complex than previously recognised.
    Description: The ChEsSo research programme was funded by a NERC Consortium Grant (NE/DO1249X/1) and supported by the Census of Marine Life and the Sloan Foundation, and the Total Foundation for Biodiversity (Abyss 2100)(SVTH) all of which are gratefully acknowledged. We also acknowledge NSF grant ANT-0739675 (CG and TS), NERC PhD studentships NE/D01429X/1(LH, LM, CNR), NE/H524922/1(JH) and NE/F010664/1 (WDKR), a Cusanuswerk doctoral fellowship, and a Lesley & Charles Hilton-Brown Scholarship, University of St. Andrews (PHBS).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
    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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  • 4
    Publication Date: 2023-03-14
    Description: This is the archaeal biomarker dataset for global peatlands. The first dataset contains biomarker data for each individual sample as for many peatlands we analysed more than one sample. The second dataset contains the averaged data for isoGDGT isomers in all sites that contains both associated pH and temperature measurements.
    Keywords: Archaea; Area/locality; BDGTs; biogeochemistry; Country; crenarchaeol; ELEVATION; GDGTs; Index; isomers; Isoprenoid glycerol dialkyl glycerol tetraether; LATITUDE; LONGITUDE; Me-GDGTs; pH; Temperature; Temperature, annual mean; wetlands
    Type: Dataset
    Format: text/tab-separated-values, 825 data points
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  • 5
    Publication Date: 2023-03-14
    Description: This is the archaeal GDGT dataset for global peatlands. The first dataset contains biomarker data for each individual sample as for many peatlands we analysed more than one sample. The second dataset contains the averaged data for isoGDGT isomers in all sites that contains both associated pH and temperature measurements. Other biomarker data for these samples can be found here: https://doi.pangaea.de/10.1594/PANGAEA.883763
    Keywords: Archaea; Area/locality; BDGTs; biogeochemistry; Country; crenarchaeol; Crenarchaeol, fractional abundance; Crenarchaeol (peak area); Crenarchaeol isomer, fractional abundance; Crenarchaeol isomer (peak area); Depth, description; GDGTs; Index; isomers; Isoprenoid acyclic glycerol dialkyl glycerol tetraether, fractional abundance; Isoprenoid dicyclic glycerol dialkyl glycerol tetraether, fractional abundance; Isoprenoid glycerol dialkyl glycerol tetraether, 5, fractional abundance; Isoprenoid glycerol dialkyl glycerol tetraether, 5 (peak area); Isoprenoid monocyclic glycerol dialkyl glycerol tetraether, fractional abundance; Isoprenoid tricyclic glycerol dialkyl glycerol tetraether, fractional abundance; Me-GDGTs; pH; pH, standard deviation; Temperature; Temperature, annual mean; Temperature, coldest month; Temperature, warmest month; wetlands
    Type: Dataset
    Format: text/tab-separated-values, 9870 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Inglis, Gordon N; Collinson, Margaret E; Riegel, Walter; Wilde, Volker; Robson, Brittany E; Lenz, Olaf K; Pancost, Richard D (2015): Ecological and biogeochemical change in an early Paleogene peat-forming environment: Linking biomarkers and palynology. Palaeogeography, Palaeoclimatology, Palaeoecology, 438, 245-255, https://doi.org/10.1016/j.palaeo.2015.08.001
    Publication Date: 2023-05-12
    Description: Sphagnum moss is the dominant plant type in modern boreal and (sub)arctic ombrotrophic bogs and is of particular interest due to its sensitivity to climate and its important role in wetland biogeochemistry. Here we reconstruct the occurrence of Sphagnum moss - and associated biogeochemical change - within a thermally immature, early Paleogene (~55 Ma) lignite from Schöningen, NW Germany using a high-resolution, multi-proxy approach. Changes in the abundance of Sphagnum-type spores and the C23/C31n-alkane ratio indicate the expansion of Sphagnum moss within the top of the lignite seam. This Sphagnum moss expansion is associated with the development of waterlogged conditions, analogous to what has been observed within modern ombrotrophic bogs. The similarity between biomarkers and palynology also indicates that the C23/C31n-alkane ratio may be a reliable chemotaxonomic indicator for Sphagnum during the early Paleogene. The d13C value of bacterial hopanes and mid-chain n-alkanes indicates that a rise in water table is not associated with a substantial increase in aerobic methanotrophy. The absence of very low d13C values within the top of the seam could reflect either less methanogenesis or less efficient methane oxidation under waterlogged sulphate-rich conditions.
    Keywords: Lower Saxony, Germany; OUTCROP; Outcrop sample; Schoningen
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 7
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    PANGAEA
    In:  Supplement to: Kuypers, Marcel MM; Lourens, Lucas Joost; Rijpstra, W Irene C; Pancost, Richard D; Nijenhuis, Ivar A; Sinninghe Damsté, Jaap S (2004): Orbital forcing of organic carbon burial in the proto-North Atlantic during oceanic anoxic event 2. Earth and Planetary Science Letters, 228(3-4), 465-482, https://doi.org/10.1016/j.epsl.2004.09.037
    Publication Date: 2023-06-27
    Description: The Cenomanian/Turonian (C/T) intervals at DSDP Sites 105 and 603B from the northern part of the proto-North Atlantic show high amplitude, short-term cyclic variations in total organic carbon (TOC) content. The more pronounced changes in TOC are also reflected by changes in lithology from green claystones (TOC〈1%) to black claystones (TOC〉1%). Although their depositional history was different, the individual TOC cycles at Sites 105 and 603B can be correlated using stable carbon isotope stratigraphy. Sedimentation rates obtained from the isotope stratigraphy and spectral analyses indicate that these cycles were predominately precession controlled. The coinciding variations in HI, OI, delta13Corg and the abundance of marine relative to terrestrial biomarkers, as well as the low abundance of lignin pyrolysis products generated from the kerogen of the black claystones, indicate that these cyclic variations reflect changes in the contribution of marine organic matter (OM). The cooccurrence of lamination, enrichment of redox-sensitive trace metals and presence of molecular fossils of pigments from green sulfur bacteria indicate that the northern proto-North Atlantic Ocean water column was periodically euxinic from the bottom to at least the base of the photic zone (〈150 m) during the deposition of the black claystones. In contrast, the green claystones are bioturbated, are enriched in Mn, do not show enrichments in redox-sensitive trace metals and show biomarker distributions indicative of long oxygen exposure times, indicating more oxic water conditions. At the same time, there is evidence (e.g., abundance of biogenic silica and significant 13C-enrichment for OC of phytoplanktic origin) for enhanced primary productivity during the deposition of the black claystones. We propose that increased primary productivity periodically overwhelmed the oxic OM remineralisation potential of the bottom waters resulting in the deposition of OM-rich black claystones. Because the amount of oxygen used for OM remineralisation exceeded the amount supplied by diffusion and deep-water circulation, the northern proto-North Atlantic became euxinic during these periods. Both Sites 105 and 603B show trends of continually increasing TOC contents and HI values of the black claystones up section, which most likely resulted from both enhanced preservation due to increased anoxia and increased production of marine OM during oceanic anoxic event 2 (OAE2).
    Keywords: 93-603B; Carbon, organic, total; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg93; Manganese/Aluminium ratio; Molybdenum/Aluminium ratio; Nickel/Aluminium ratio; Rock type; Sample code/label; Vanadium/Aluminium ratio; X-ray diffraction (XRD); Zinc/Aluminium ratio
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: 165-999A; AGE; Caribbean Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg165; Noelaerhabdaceae, length; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2754 data points
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  • 9
    Publication Date: 2023-05-12
    Keywords: Apectodinium; Identification; Inaperturopollenites; Laevigatosporites; Lithologic unit/sequence; Lithology/composition/facies; Lower Saxony, Germany; OUTCROP; Outcrop sample; Schoningen; Sphagnum-type; Zygnemataceae
    Type: Dataset
    Format: text/tab-separated-values, 297 data points
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  • 10
    Publication Date: 2023-05-12
    Keywords: Carbon, organic, total; Carbon/Nitrogen ratio; Identification; Lithologic unit/sequence; Lithology/composition/facies; Lower Saxony, Germany; OUTCROP; Outcrop sample; Schoningen; Sulfur, total
    Type: Dataset
    Format: text/tab-separated-values, 238 data points
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