Relevant bibliographies by topics / Euxinic basins

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers
  5. Reports

Academic literature on the topic 'Euxinic basins'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Euxinic basins"

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Helz, George R., and Marvourneen K. Dolor. "What regulates rhenium deposition in euxinic basins?" Chemical Geology 304-305 (April 2012): 131–41. http://dx.doi.org/10.1016/j.chemgeo.2012.02.011.

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Bura-Nakić, Elvira, Morten B. Andersen, Corey Archer, Gregory F. de Souza, Marija Marguš, and Derek Vance. "Coupled Mo-U abundances and isotopes in a small marine euxinic basin: Constraints on processes in euxinic basins." Geochimica et Cosmochimica Acta 222 (February 2018): 212–29. http://dx.doi.org/10.1016/j.gca.2017.10.023.

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Filatova, N. I. "Jurassic anoxic event in the Pacific (on the West Kamchatka-Asia data)." Доклады Академии наук 487, no. 5 (2019): 543–46. http://dx.doi.org/10.31857/s0869-56524875543-546.

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The correlation of allochthonous lithotectonic complexes of the Pacific allows to establish Early Jurassic (Sinemurian-Toarcian) anoxic event (J1-OAE) for time in the Asia-West Kamchatka region. This event is characterized by organic-riched black cherts and shales bearing pyrite that accumulated in the euxinic oceanic deep water basins of the Pacific. Later anoxic regime gradually weakened that was reflected in dominating of Midle-Upper Jurassic red gematite jaspers. J1-OAE in the Pacific was synchronous to global warming induced by planetary magmatic activity. Volcanic gases and hydroterms st
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Fulton, J. M., M. A. Arthur, B. Thomas, and K. H. Freeman. "Pigment carbon and nitrogen isotopic signatures in euxinic basins." Geobiology 16, no. 4 (2018): 429–45. http://dx.doi.org/10.1111/gbi.12285.

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Kunert, Alexandra, Johnathan Clarke, and Brian Kendall. "Molybdenum Isotope Constraints on the Origin of Vanadium Hyper-Enrichments in Ediacaran–Phanerozoic Marine Mudrocks." Minerals 10, no. 12 (2020): 1075. http://dx.doi.org/10.3390/min10121075.

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Vanadium is an important redox-sensitive trace metal for paleoenvironmental reconstructions. Modern organic-rich sediments persistently contain sediment V enrichments <500 μg/g, but many ancient marine organic-rich mudrocks record enrichments >500 μg/g. Previous studies propose that ancient V enrichments of these magnitudes (“V hyper-enrichments”) were deposited from hyper-sulfidic bottom-waters with higher H2S levels (≥10 mM) than observed in modern euxinic basins. To test the importance of hyper-sulfidic conditions for generating V hyper-enrichments, we compare V concentrations with Mo
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Nainggolan, T. B., U. Nurhasanah, and I. Setiadi. "Depositional sequence interpretation using seismic and well data of offshore Central Sumatra Basin." IOP Conference Series: Earth and Environmental Science 944, no. 1 (2021): 012002. http://dx.doi.org/10.1088/1755-1315/944/1/012002.

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Abstract Offshore Central Sumatra Basin is an integral part of Central Sumatra Basin known for producing hydrocarbon basins. The derivation of stratigraphic study of seismic and well data is intended to improve accuracy of geological interpretation. Sequence stratigraphy studies have a significant role in exploratory studies to determine which depositional sequence can be inferred as hydrocarbon reservoir and its correlation in petroleum system. This study aims to identify biogenic gas sequential interpretation using seismic and well data of offshore Central Sumatra Basin. The procedure to ana
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Lenz, C., T. Jilbert, D. J. Conley, M. Wolthers, and C. P. Slomp. "Are recent changes in sediment manganese sequestration in the euxinic basins of the Baltic Sea linked to the expansion of hypoxia?" Biogeosciences 12, no. 16 (2015): 4875–94. http://dx.doi.org/10.5194/bg-12-4875-2015.

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Abstract. Expanding hypoxia in the Baltic Sea over the past century has led to the development of anoxic and sulfidic (euxinic) deep basins that are only periodically ventilated by inflows of oxygenated waters from the North Sea. In this study, we investigate the potential consequences of the expanding hypoxia for manganese (Mn) burial in the Baltic Sea using a combination of pore water and sediment analyses of dated sediment cores from eight locations. Diffusive fluxes of dissolved Mn from sediments to overlying waters at oxic, hypoxic and euxinic sites are consistent with an active release o
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Wendt, Anna K., Mike A. Arthur, Rudy Slingerland, Daniel Kohl, Reed Bracht, and Terry Engelder. "Geochemistry and depositional history of the Union Springs Member, Marcellus Formation in central Pennsylvania." Interpretation 3, no. 3 (2015): SV17—SV33. http://dx.doi.org/10.1190/int-2014-0228.1.

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Debate continues over paleoenvironmental conditions that prevail during deposition of organic-carbon (C)-rich marine source rocks in foreland basins and epicontinental seas. The focus of disagreement centers largely on paleowater depth and the prevalence of anoxia/euxinia. The issues of paleodepth and water column conditions are important for prediction of lateral variations in source quality within a basin because the viability of a hydrocarbon play depends on a thorough understanding of the distribution of source rock quality and depositional environments. We used inorganic geochemical data
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Dellwig, Olaf, Antje Wegwerth, Bernhard Schnetger, Hartmut Schulz, and Helge W. Arz. "Dissimilar behaviors of the geochemical twins W and Mo in hypoxic-euxinic marine basins." Earth-Science Reviews 193 (June 2019): 1–23. http://dx.doi.org/10.1016/j.earscirev.2019.03.017.

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Lyons, Timothy W., and Silke Severmann. "A critical look at iron paleoredox proxies: New insights from modern euxinic marine basins." Geochimica et Cosmochimica Acta 70, no. 23 (2006): 5698–722. http://dx.doi.org/10.1016/j.gca.2006.08.021.

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Dissertations / Theses on the topic "Euxinic basins"

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Taniwaki, Takashi. "Photic Zone Euxinia and Microbial Mat Development in the Early Triassic of the Perth Basin, Western Australia: Implications for Petroleum Systems." Thesis, Curtin University, 2021. http://hdl.handle.net/20.500.11937/88829.

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Reconstruction of basin-scale paleogeography and paleoenvironments in the northern Perth Basin during the Early Triassic, utilising integrated geological and organic geochemical analyses, shows the distribution of photic zone euxinia and microbial mats following the end-Permian mass extinction. Such analyses also distinguish the organic geochemical signatures of photic zone euxinia and microbial mats, identify source rock potential across the basin, and have implications for the petroleum system in both the northern Perth and Northern Carnarvon basins.
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Book chapters on the topic "Euxinic basins"

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Giannetta, Leo G., and Richard J. Behl. "Chemostratigraphic and lithostratigraphic framework of the Eocene Kreyenhagen Formation, Kettleman area, central San Joaquin Basin, California." In Understanding the Monterey Formation and Similar Biosiliceous Units across Space and Time. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2556(12).

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ABSTRACT The Eocene Kreyenhagen Formation is a widespread siliceous, organic-rich mudstone within the San Joaquin Basin, but it is less studied than the Monterey Formation. This study characterizes the Kreyenhagen Formation in the Kettleman area to define its vertical and lateral variability on the basis redox conditions (Mo, U, Cr), paleoproductivity (biogenic SiO2, P, Ba), and detrital input (Al2O3, TiO2) to determine the dominant environmental conditions during deposition. The Kreyenhagen Formation was correlated across 72 wells over a 4600 km2 (1776 mi2) area, which revealed an eastward th
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Conference papers on the topic "Euxinic basins"

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Kafantaris, Fotios-Christos A., Martin Kurek, Gregory Druschel, William Gilhooly, Sabine Dvorski, and Philippe Schmitt-Kopplin. "REACTIVITY OF POLYSULFIDES AND ITS CONTRIBUTION TO CRYPTIC SULFUR CYCLING IN ANOXIC/EUXINIC BASINS." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291108.

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Krasnova, E. D., E. A. Labunskaya, V. I. Lobyshev, and D. A. Voronov. "How does yellow matter affect the pigment composition of the microbial community in euxinic lagoons and lakes?" In Всероссийская конференция и полевой симпозиум. ФИЦ КНЦ РАН, 2024. http://dx.doi.org/10.37614/978.5.91137.520.1.013.

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In coastal basins separated from the White Sea due to post-glacial uplift, the spectrum of light at the boundary of the photic zone gradually shifts towards long waves: from predominantly green (in marine area and in bucket bays) to green-orange-red in lagoons, then to yellow-orange-red in meromictic lakes with fresh mixolimnion and orange-red in fresh lakes. This is due to increase of concentration of humic substances (CDOM, «yellow substance»). They attenuate short-wavelength light and reduce the photic zone. The light spectra are consistent with the color of photosynthetic microorganisms th
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Zhou, Anwen, Chadlin Ostrander, Morrison Nolan, et al. "Recurrent photic zone euxinia in Ediacaran South China Basin revealed by mercury enrichment and isotope compositions." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7121.

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Kunert, Alex, and Brian Kendall. "EARLY JURASSIC PALEOENVIRONMENTAL RECONSTRUCTION IN THE WESTERN CANADA SEDIMENTARY BASIN AND INFERENCE OF EXPANDED OCEAN ANOXIA/EUXINIA ACROSS THE TOARCIAN OAE FROM GLOBAL RE AND MO MASS BALANCE MODELS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338613.

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Reports on the topic "Euxinic basins"

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Cesar, J. R., and O. H. Ardakani. Organic geochemistry of the Montney Formation: new insights about the source of hydrocarbons, their accumulation history and post accumulation processes. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329788.

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This study consists of a non-traditional molecular and stable isotope approach to analyze organic matter (soluble bitumen and produced oil/condensate) from the Montney Formation low-permeability reservoirs, with the purpose of identifying source(s) of hydrocarbons, accumulation history and post accumulation processes. The same approach bases on the distribution of compound classes such as aromatic carotenoids, polycyclic aromatic hydrocarbons (PAHs), bicyclic alkanes, and oxygen-polar compounds. The geochemical screening has been enhanced with performing compound specific isotope analysis (CSI
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Journal articles
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