کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8910138 | 1637481 | 2018 | 42 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Oscillating redox conditions in the Vocontian Basin (SE France) during Oceanic Anoxic Event 2 (OAE 2)
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
ژئوشیمی و پترولوژی
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چکیده انگلیسی
The Cenomanian-Turonian boundary (~94â¯Ma) was marked by an episode of widespread organic carbon burial largely associated with low oxygen concentrations in bottom oceanic waters, named Oceanic Anoxic Event 2 (OAE 2). In the Vocontian Basin (SE France), the Pont d'Issole section exposes a 22â¯m interval called Niveau Thomel, the local sedimentary expression of the OAE 2, characterized by levels of laminated dark shales with marine-derived organic matter enrichments (up to 2.5â¯wt%). An episodic disruption in total organic carbon (TOC) enrichment is observed in bioturbated limestones within the Niveau Thomel, reflecting bottom-water reoxygenation associated to the Plenus Cold Event. Oscillations in redox conditions during the OAE 2 are evidenced by variations in the degree of pyritisation of the sediments reflecting suboxic to anoxic conditions associated with organic-rich intervals. These variations are additionally highlighted by enrichments in redox-sensitive trace elements (Mo, V, Zn) in sediments containing at least 1.5â¯wt% TOC, which may reflect a threshold between suboxic and anoxic conditions at Pont d'Issole section. Low Mn and Fe concentrations in >0.3â¯wt% TOC samples mark a large O2 depletion in pore waters. Phosphorus released from the sediments under deoxygenated conditions could have contributed to sustain the primary productivity in the basin, promoting further O2 consumption. A large negative excursion in the sulfur isotopic composition of pyrite (δ34Spy) with minimum values down to â40â° suggests that microbial sulfate reduction was non sulfate-limited and was characterized by pyrite precipitation in an open system with regard to the marine sulfate reservoir. This feature is probably linked to a higher sulfate availability within the Vocontian Basin due to important Large Igneous Province outgassing at the onset of the OAE 2.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Chemical Geology - Volume 493, 20 August 2018, Pages 136-152
Journal: Chemical Geology - Volume 493, 20 August 2018, Pages 136-152
نویسندگان
Julien Danzelle, Laurent Riquier, François Baudin, Christophe Thomazo, Emmanuelle Pucéat,