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  • Erba, Elisabetta  (3)
  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 2022
    In:  Earth and Planetary Science Letters Vol. 578 ( 2022-01), p. 117324-
    In: Earth and Planetary Science Letters, Elsevier BV, Vol. 578 ( 2022-01), p. 117324-
    Type of Medium: Online Resource
    ISSN: 0012-821X
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2022
    detail.hit.zdb_id: 300203-2
    detail.hit.zdb_id: 1466659-5
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 2
    In: Geology, Geological Society of America, Vol. 49, No. 12 ( 2021-12-01), p. 1452-1456
    Abstract: Widespread oceanic anoxia, biological crises, and volcanic activity are associated with the onset of Early Aptian (ca. 120 Ma) Oceanic Anoxic Event 1a (OAE1a). Reconstructions of oceanic deoxygenation and its links to broadly contemporaneous volcanism, however, remain poorly resolved. We use geochemical data, including δ53Cr ratios and rare Earth element abundances, to define the timing and tempo of submarine volcanism and global oceanic deoxygenation across this event. Pacific Ocean sediments deposited in the run up to OAE1a record multiple phases of marine volcanism associated with the emplacement of Ontong Java Plateau lavas. Rapid oceanic deoxygenation followed the initial phases of volcanism and a biocalcification crisis. Large swaths of the oceans likely became anoxic from the Tethys to the Pacific Oceans in & lt;30 k.y. Oceanic anoxia persisted for almost one million years after this and was likely sustained through intensified continental and submarine weathering. These results paint a new picture of OAE1a in which volcanism, biological crisis, and oceanic deoxygenation are separated in time and linked through Earth system responses that operate on time scales of tens of thousands of years.
    Type of Medium: Online Resource
    ISSN: 0091-7613 , 1943-2682
    Language: English
    Publisher: Geological Society of America
    Publication Date: 2021
    detail.hit.zdb_id: 184929-3
    detail.hit.zdb_id: 2041152-2
    SSG: 13
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2023
    In:  Geobiology Vol. 21, No. 3 ( 2023-05), p. 341-354
    In: Geobiology, Wiley, Vol. 21, No. 3 ( 2023-05), p. 341-354
    Abstract: Oceanic Anoxic Events (OAEs) are conspicuous intervals in the geologic record that are associated with the deposition of organic carbon (OC)‐rich marine sediment, linked to extreme biogeochemical perturbations, and characterized by widespread ocean deoxygenation. Mechanistic links between the marine biological carbon pump (BCP), redox conditions, and organic carbon burial during OAEs, however, remain poorly constrained. In this work we reconstructed the BCP in the western Tethys Ocean across OAE1a (~120 Mya) using sediment geochemistry and OC mass accumulation rates ( OC Acc ). We find that OC Acc were between 0.006 and 3.3 gC m −2  yr −1 , with a mean value of 0.79 ± 0.78 SD gC m −2  yr −1 —these rates are low and comparable to oligotrophic regions in the modern oceans. This challenges longstanding assumptions that oceanic anoxic events are intervals of strongly elevated organic carbon burial. Numerical modelling of the BCP, furthermore, reveals that such low OC fluxes are only possible with either or both low to moderate OC export fluxes from ocean surface waters, with rates similar to oligotrophic (nutrient‐poor, 〈 30 gC m −2  yr −1 ) and mesotrophic (moderate‐nutrients, ~50–100 gC m −2  yr −1 ) regions in the modern ocean, and stronger than modern vertical OC attenuation. The low OC fluxes thus reflect a relatively weak BCP. Low to moderate productivity is further supported by palaeoecological and geochemical evidence and was likely maintained through nutrient limitation that developed in response to the burial and sequestration of phosphorus in association with iron minerals under ferruginous (anoxic iron‐rich) ocean conditions. Without persistently high productivity, ocean deoxygenation during OAE1a was more likely driven by other physicochemical and biological factors including ocean warming, changes in marine primary producer community composition, and fundamental shifts in the efficiency of the BCP with associated effects and feedbacks.
    Type of Medium: Online Resource
    ISSN: 1472-4677 , 1472-4669
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2023
    detail.hit.zdb_id: 2113509-5
    SSG: 12
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