All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Elemental and isotopic compositions of trench-slope black shales, Bohemian Massif, with implications for oceanic and atmospheric oxygenation in early Cambrian

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F21%3A00000046" target="_blank" >RIV/00025798:_____/21:00000046 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/21:00538188 RIV/00216208:11310/21:10438946

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S003101822030643X?casa_token=ZGFI_kZ_xz0AAAAA:CldCOHCPfLd4A1ZqxV-mJ4-xaNS4sLGlMml6LbfTDkI-h2SOOTucIJq5JuToiuA9JkrJv9KAiA" target="_blank" >https://www.sciencedirect.com/science/article/pii/S003101822030643X?casa_token=ZGFI_kZ_xz0AAAAA:CldCOHCPfLd4A1ZqxV-mJ4-xaNS4sLGlMml6LbfTDkI-h2SOOTucIJq5JuToiuA9JkrJv9KAiA</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.palaeo.2020.110195" target="_blank" >10.1016/j.palaeo.2020.110195</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Elemental and isotopic compositions of trench-slope black shales, Bohemian Massif, with implications for oceanic and atmospheric oxygenation in early Cambrian

  • Original language description

    This study examines a lower Cambrian pyrite-bearing black shale–graywacke succession in the Czech Republic interpreted as infill of a deep-marine, extensional trench-slope basin on top of an accretionary wedge that developed during subduction of an oceanic plate beneath the northern margin of Gondwana. The new U–Pb detrital zircon geochronology of the graywacke constrains the maximum age of deposition to 533 +5/−6 Ma, whereas the Re–Os dating of pyrite yielded a younger age of 7 ± 16 Ma. Distribution of major and trace elements and calculated enrichment factors (EF) indicate that this succession was deposited under changing redox conditions over a short time span and that the basin was presumably controlled by tectonic subsidence and varying supply of terrigenous arc-derived material. This depositional setting is reflected by largely variable EFs and delta98Mo and delta53Cr values. Euxinic conditions detected at the base of the sampled black shale interval are documented by the highest values of EFs of redox-sensitive metals (e.g., Mo, U, V, Ni, Co, As) and also the Corg/P (>;1000) and DOPT (>;0.7) values. Black shales show lower delta56Fe values due to the excess of authigenic pyrite-Fe with a mean delta56Fe value of −0.02per mille over detrital Fe in graywacke with a mean delta56Fe value of +0.25per mille. However, the Fe isotopic signatures of the black shales are not consistent with iron shuttling, mixing of authigenic and detrital sources, or hydrothermal metal enrichment. Instead, they most likely resulted from partial oxidation of pyrite through the syndepositional oxidizing hydrothermal fluids (Si–Ba enrichment), which resulted in precipitation of isotopically heavy Fe-oxyhydroxides. We propose that our maximal recorded delta98Mo value (+ 0.98per mille) might represent the best estimate for the ancient local seawater Mo composition at around 533 Ma and argues against deep-ocean oxygenation in the early Cambrian. On the other hand, the Se/Co ratios of synsedimentary pyrite indicate a mean atmosphere O2 value of ~27percent.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GA20-13644S" target="_blank" >GA20-13644S: Cherts and carbonates as geochemical proxies of paleoenvironmental conditions and Ocean Plate Stratigraphy</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Palaeogeography, Palaeoclimatology, Palaeoecology

  • ISSN

    0031-0182

  • e-ISSN

  • Volume of the periodical

    564

  • Issue of the periodical within the volume

    February : 110195

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    21

  • Pages from-to

    nestránkováno

  • UT code for WoS article

    000636756800021

  • EID of the result in the Scopus database

    2-s2.0-85100186796