The Aptian evaporites of the South Atlantic: a climatic paradox?

For a long time, evaporitic sequences have been interpreted as indicative of an arid climate. Such systematic interpretations led to the suggestion that the Central segment of the South Atlantic (20–0°) was characterized by an arid climate during the upper Aptian. Indeed, synchronous to this period...

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Main Authors: A.-C. Chaboureau, Y. Donnadieu, P. Sepulchre, C. Robin, F. Guillocheau, S. Rohais
Format: Article
Language:English
Published: Copernicus Publications 2012-06-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/8/1047/2012/cp-8-1047-2012.pdf
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spelling doaj-db89d11b6f9b4e6082ab314cdd96bfa92020-11-24T23:54:06ZengCopernicus PublicationsClimate of the Past1814-93241814-93322012-06-01831047105810.5194/cp-8-1047-2012The Aptian evaporites of the South Atlantic: a climatic paradox?A.-C. ChaboureauY. DonnadieuP. SepulchreC. RobinF. GuillocheauS. RohaisFor a long time, evaporitic sequences have been interpreted as indicative of an arid climate. Such systematic interpretations led to the suggestion that the Central segment of the South Atlantic (20–0°) was characterized by an arid climate during the upper Aptian. Indeed, synchronous to this period that corresponds to the rifting and to the opening of this part of the South Atlantic, a large evaporitic sequence spreads out from the equator to 20° S. Using the fully ocean atmosphere coupled model FOAM, we test the potential for the Aptian geography to produce an arid area over the Central segment. Sensitivity to the altitude of the rift shoulders separating the Africa and the South America cratons, to the water depth of the Central segment and to the drainage pattern have been performed. Using seawater salinity as a diagnostic, our simulations show that the southern part of the Central segment is characterized by very high salinity in the case of catchment areas draining the water out of the Central segment. Conversely, whatever the boundary conditions used, the northern part of the Central segment remains humid and salinities are very low. Hence, we conclude that the evaporites deposited in the southern part of the Central segment may have been controlled by the climate favouring aridity and high saline waters. In contrast, the evaporites of the northern part can hardly be reconciled with the climatic conditions occurring there and may be due to hydrothermal sources. Our interpretations are in agreement with the gradient found in the mineralogical compositions of the evaporites from the North to the South, i.e. the northern evaporites are at least 4 times more concentrated than the southern one.http://www.clim-past.net/8/1047/2012/cp-8-1047-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A.-C. Chaboureau
Y. Donnadieu
P. Sepulchre
C. Robin
F. Guillocheau
S. Rohais
spellingShingle A.-C. Chaboureau
Y. Donnadieu
P. Sepulchre
C. Robin
F. Guillocheau
S. Rohais
The Aptian evaporites of the South Atlantic: a climatic paradox?
Climate of the Past
author_facet A.-C. Chaboureau
Y. Donnadieu
P. Sepulchre
C. Robin
F. Guillocheau
S. Rohais
author_sort A.-C. Chaboureau
title The Aptian evaporites of the South Atlantic: a climatic paradox?
title_short The Aptian evaporites of the South Atlantic: a climatic paradox?
title_full The Aptian evaporites of the South Atlantic: a climatic paradox?
title_fullStr The Aptian evaporites of the South Atlantic: a climatic paradox?
title_full_unstemmed The Aptian evaporites of the South Atlantic: a climatic paradox?
title_sort aptian evaporites of the south atlantic: a climatic paradox?
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2012-06-01
description For a long time, evaporitic sequences have been interpreted as indicative of an arid climate. Such systematic interpretations led to the suggestion that the Central segment of the South Atlantic (20–0°) was characterized by an arid climate during the upper Aptian. Indeed, synchronous to this period that corresponds to the rifting and to the opening of this part of the South Atlantic, a large evaporitic sequence spreads out from the equator to 20° S. Using the fully ocean atmosphere coupled model FOAM, we test the potential for the Aptian geography to produce an arid area over the Central segment. Sensitivity to the altitude of the rift shoulders separating the Africa and the South America cratons, to the water depth of the Central segment and to the drainage pattern have been performed. Using seawater salinity as a diagnostic, our simulations show that the southern part of the Central segment is characterized by very high salinity in the case of catchment areas draining the water out of the Central segment. Conversely, whatever the boundary conditions used, the northern part of the Central segment remains humid and salinities are very low. Hence, we conclude that the evaporites deposited in the southern part of the Central segment may have been controlled by the climate favouring aridity and high saline waters. In contrast, the evaporites of the northern part can hardly be reconciled with the climatic conditions occurring there and may be due to hydrothermal sources. Our interpretations are in agreement with the gradient found in the mineralogical compositions of the evaporites from the North to the South, i.e. the northern evaporites are at least 4 times more concentrated than the southern one.
url http://www.clim-past.net/8/1047/2012/cp-8-1047-2012.pdf
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