Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean

<p>The Toarcian Oceanic Anoxic Event (T-OAE) interval was cored at Colle di Sogno and Gajum in the Lombardy Basin (Southern Alps, northern Italy). The Sogno and Gajum cores recovered 26.83 and 31.18 stratigraphic metres, respectively, of pelagic sediments consisting of marly limestones, marlst...

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Main Authors: E. Erba, G. Gambacorta, S. Visentin, L. Cavalheiro, D. Reolon, G. Faucher, M. Pegoraro
Format: Article
Language:English
Published: Copernicus Publications 2019-12-01
Series:Scientific Drilling
Online Access:https://www.sci-dril.net/26/17/2019/sd-26-17-2019.pdf
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spelling doaj-d4dcca8124494dafabc8a10d2a39708d2020-11-25T02:16:08ZengCopernicus PublicationsScientific Drilling 1816-89571816-34592019-12-0126172710.5194/sd-26-17-2019Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys OceanE. ErbaG. GambacortaS. VisentinL. CavalheiroD. ReolonG. FaucherM. Pegoraro<p>The Toarcian Oceanic Anoxic Event (T-OAE) interval was cored at Colle di Sogno and Gajum in the Lombardy Basin (Southern Alps, northern Italy). The Sogno and Gajum cores recovered 26.83 and 31.18 stratigraphic metres, respectively, of pelagic sediments consisting of marly limestones, marlstone, marly claystone, and black shale. Drilling at both sites resulted in 100&thinsp;% recovery of unweathered material. The pelagic succession comprises a relatively expanded black shale interval of 4.98&thinsp;m in the Sogno core and 15.35&thinsp;m in the Gajum core, with lower and upper boundaries without evidence of hiatuses. The Sogno and Gajum cores can be considered reference sections for the pelagic lower Toarcian interval of the western Tethys and will provide high-resolution micropaleontological, inorganic and organic geochemical, isotopic multiproxy data. Integrated stratigraphy and cyclostratigraphy are predicted to result in estimates of durations and rates to model the ecosystem resilience to the extreme perturbations of the T-OAE and gain a better understanding of current global changes and help provide better projections of future scenarios.</p>https://www.sci-dril.net/26/17/2019/sd-26-17-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Erba
G. Gambacorta
S. Visentin
L. Cavalheiro
D. Reolon
G. Faucher
M. Pegoraro
spellingShingle E. Erba
G. Gambacorta
S. Visentin
L. Cavalheiro
D. Reolon
G. Faucher
M. Pegoraro
Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
Scientific Drilling
author_facet E. Erba
G. Gambacorta
S. Visentin
L. Cavalheiro
D. Reolon
G. Faucher
M. Pegoraro
author_sort E. Erba
title Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
title_short Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
title_full Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
title_fullStr Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
title_full_unstemmed Coring the sedimentary expression of the early Toarcian Oceanic Anoxic Event: new stratigraphic records from the Tethys Ocean
title_sort coring the sedimentary expression of the early toarcian oceanic anoxic event: new stratigraphic records from the tethys ocean
publisher Copernicus Publications
series Scientific Drilling
issn 1816-8957
1816-3459
publishDate 2019-12-01
description <p>The Toarcian Oceanic Anoxic Event (T-OAE) interval was cored at Colle di Sogno and Gajum in the Lombardy Basin (Southern Alps, northern Italy). The Sogno and Gajum cores recovered 26.83 and 31.18 stratigraphic metres, respectively, of pelagic sediments consisting of marly limestones, marlstone, marly claystone, and black shale. Drilling at both sites resulted in 100&thinsp;% recovery of unweathered material. The pelagic succession comprises a relatively expanded black shale interval of 4.98&thinsp;m in the Sogno core and 15.35&thinsp;m in the Gajum core, with lower and upper boundaries without evidence of hiatuses. The Sogno and Gajum cores can be considered reference sections for the pelagic lower Toarcian interval of the western Tethys and will provide high-resolution micropaleontological, inorganic and organic geochemical, isotopic multiproxy data. Integrated stratigraphy and cyclostratigraphy are predicted to result in estimates of durations and rates to model the ecosystem resilience to the extreme perturbations of the T-OAE and gain a better understanding of current global changes and help provide better projections of future scenarios.</p>
url https://www.sci-dril.net/26/17/2019/sd-26-17-2019.pdf
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