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  • PANGAEA  (4)
  • Instytut Paleobiologii PAN  (2)
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  • 1
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    PANGAEA
    In:  Supplement to: Küchler, Rony R; Birgel, Daniel; Kiel, Steffen; Freiwald, André; Goedert, James L; Thiel, Volker; Peckmann, Jörn (2012): Miocene methane-derived carbonates from southwestern Washington, USA and a model for silicification at seeps. Lethaia, 45(2), 259-273, https://doi.org/10.1111/j.1502-3931.2011.00280.x
    Publikationsdatum: 2023-11-20
    Beschreibung: Exotic limestone masses with silicified fossils, enclosed within deep-water marine siliciclastic sediments of the Early to Middle Miocene Astoria Formation, are exposed along the north shore of the Columbia River in southwestern Washington, USA. Samples from four localities were studied to clarify the origin and diagenesis of these limestone deposits. The bioturbated and reworked limestones contain a faunal assemblage resembling that of modern and Cenozoic deep-water methane-seeps. Five phases make up the paragenetic sequence: (1) micrite and microspar; (2) fibrous, banded and botryoidal aragonite cement, partially replaced by silica or recrystallized to calcite; (3) yellow calcite; (4) quartz replacing carbonate phases and quartz cement; and (5) equant calcite spar and pseudospar. Layers of pyrite frequently separate different carbonate phases and generations, indicating periods of corrosion. Negative d13Ccarbonate values as low as -37.6 per mill V-PDB reveal an uptake of methane-derived carbon. In other cases, d13Ccarbonate values as high as 7.1 per mill point to a residual, 13C-enriched carbon pool affected by methanogenesis. Lipid biomarkers include 13C-depleted, archaeal 2,6,10,15,19-pentamethylicosane (PMI; d13C: -128 per mill), crocetane and phytane, as well as various iso- and anteiso-carbon chains, most likely derived from sulphate-reducing bacteria. The biomarker inventory proves that the majority of the carbonates formed as a consequence of sulphate-dependent anaerobic oxidation of methane. Silicification of fossils and early diagenetic carbonate cements as well as the precipitation of quartz cement - also observed in other methane-seep limestones enclosed in sediments with abundant diatoms or radiolarians - is a consequence of a preceding increase of alkalinity due to anaerobic oxidation of methane, inducing the dissolution of silica skeletons. Once anaerobic oxidation of methane has ceased, the pH drops again and silica phases can precipitate.
    Schlagwort(e): Center for Marine Environmental Sciences; MARUM
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Eickmann, Benjamin; Bach, Wolfgang; Kiel, Steffen; Reitner, Joachim; Peckmann, Jörn (2009): Evidence for cryptoendolithic life in Devonian pillow basalts of Variscan orogens, Germany. Palaeogeography, Palaeoclimatology, Palaeoecology, 283, 120-125, https://doi.org/10.1016/j.palaeo.2009.09.006
    Publikationsdatum: 2023-11-20
    Beschreibung: Late Devonian (Frasnian) pillow basalts from the Frankenwald and Thüringer Wald within the Saxothuringian zone in Germany were found to contain abundant putative biogenic filaments, indicating that the volcanic rocks once harbored microbial life. The mineralized filaments are found in calcite-filled amygdules (former vesicles), where they started to form on internal surfaces of vesicles after seawater ingress. The filaments postdate an early fibrous carbonate cement but predate later equant calcite spar, revealing syngenetic formation. A biogenic origin of filaments is indicated by their size and morphology resembling modern microorganisms, their independence of crystal faces and cleavage plans, complex branching patterns, and internal segmentation. The filamentous microorganisms represent cryptoendoliths that lived in structural cavities of the basalt. They became preserved upon microbial clay authigenesis similar to the encrustation of modern prokaryotes in iron-rich environments. Filaments consist of clay minerals with the endmember composition berthierine-chamosite and illite-glauconite. Based on the discovery of fossilized filamentous microorganisms in Late Devonian pillow basalts of the Saxothurigian zone that are similar to filaments previously found in Middle Devonian pillow basalts of the Rhenohercynian zone, it is apparent that cryptoendolithic life was more widespread than previously recognized. Structural cavities within seafloor basalt may thus represent a common, perhaps universal niche for life in the oceanic crust.
    Schlagwort(e): Aluminium oxide; Calcium oxide; Calculated; Center for Marine Environmental Sciences; Chromium(III) oxide; Electron microprobe JEOL JXA 8900R; Facies name/code; Frankenwald, northern Bavaria, Germany; FW-05-b; Geological sample; GEOS; Iron oxide, FeO; Magnesium oxide; Manganese oxide; MARUM; Potassium oxide; Sample ID; Silicon dioxide; Sum; TH-be-08-09C; Thuringian Forest, Germany; Titanium dioxide
    Materialart: Dataset
    Format: text/tab-separated-values, 1488 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-11-20
    Schlagwort(e): 447; 6132; Center for Marine Environmental Sciences; Columbia River, Washington State, USA; Compounds; Event label; HAND; JLG_447; LACMIP_6132; Lipids; MARUM; Mass spectrometer Finnigan MAT 252; Reference/source; Sampling by hand; δ13C
    Materialart: Dataset
    Format: text/tab-separated-values, 110 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-11-20
    Schlagwort(e): 447; 497; 6132; Center for Marine Environmental Sciences; Columbia River, Washington State, USA; Event label; HAND; JLG_447; JLG_497; LACMIP_6132; M2790; MARUM; Mass spectrometer Finnigan MAT 252; Phase; Sampling by hand; USGS_M2790; δ13C, calcite; δ13C, standard deviation; δ18O, calcite; δ18O, standard deviation
    Materialart: Dataset
    Format: text/tab-separated-values, 275 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2022-05-25
    Beschreibung: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Acta Palaeontologica Polonica 63 (2018): 569-577, doi:10.4202/app.00472.2018.
    Beschreibung: A limestone deposit with an unusual fauna is reported from the late Miocene of northern Italy (Ca’ Fornace site). The petrography of the carbonate and its distinct carbon isotope signature (with δ13C values as low as -57.6‰) clearly identify this limestone as an ancient methane-seep deposit. The dominant faunal elements are serpulid tubes belonging to Protis, and extremely inflated, medium-sized shells of the lucinid bivalve Anodontia mioinflata sp. nov. Also common is the small bathymodiolin Idas aff. tauroparva, plus some large specimens of the lucinid Lucinoma, and poorly preserved, medium-sized specimens of a possible vesicomyid bivalve, an arcid bivalve, small gastropods of the genera Laeviphitus (Elachisinidae), Anatoma (Scissurellidae), as well as desmophyliid and caryophyllid scleractinian corals. This faunal assemblage is quite distinct from the typical Miocene seep faunas in northern Italy, which are dominated by large bivalves of the Lucinidae (Meganodontia), Vesicomyidae (Archivesica), and Bathymodiolinae, possibly due to a shallower depositional depth of the Ca’ Fornace site.
    Beschreibung: Financial support was provided by the Swedish Research Council (Vetenskapsrådet) through grant 2016-03920 to SK.
    Schlagwort(e): Gastropoda ; Scleractinia ; Serpulidae ; Bivalvia ; Lucinidae ; Bathymodiolinae ; Methane seep ; Miocene ; Italy ; Apennines
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2022-05-25
    Beschreibung: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Acta Palaeontologica Polonica 63 (2018): 557-568, doi:10.4202/app.00473.2018.
    Beschreibung: Seven species of chemosymbiotic bivalves are described from the late Pliocene Stirone River hydrocarbon seep complex in northern Italy, including one new species and two in open nomenclature. The known species are the solemyid Acharax doderleini, the lucinids Lucinoma persolida and Megaxinus ellipticus, and the vesicomyid Isorropodon aff. perplexum; in open nomenclature we report two lucinids, including the largest species of Lucinoma known from the Italian Pliocene to date, and a strongly inflated, large Anodontia sp. The most abundant species at the Stirone seep complex is the lucinid Megaxinus stironensis sp. nov. This Pliocene seep fauna differs from that of the well-known Miocene “Calcari a Lucina” seep deposits by lacking large bathymodiolin mussels and vesicomyid clams; instead, the dominance of the lucinid Megaxinus stironensis gives this fauna a unique character. We speculate that at the Stirone seep complex, Megaxinus had occupied the ecological niche that Meganodontia occupied at the Miocene “Calcari a Lucina” seep sites in the Mediterranean basin, and that the dominance of Megaxinus could be a wide-spread feature of Pliocene chemosynthesis-based ecosystems in Mediterranean Pliocene.
    Beschreibung: Financial support for field work by SK was provided by the Deutsche Forschungsgemeinschaft through grant Ki802/6-1 and the Alméns fund of the Kungliga Vetenskaps-Akademien.
    Schlagwort(e): Bivalvia ; Lucinidae ; Vesicomyidae ; Hydrocarbon seep ; Chemosymbiosis ; Pliocene ; Italy ; Apennines
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Erwartet Verfügbarkeit
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