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• W2158528018 abstract "Research Article| July 01, 2011 FAUNAL EVIDENCE OF A HOLOCENE PLUVIAL PHASE IN SOUTHERN ARABIA WITH REMARKS ON THE MORPHOLOGICAL VARIABILITY OF HELENINA ANDERSENI Giordana Gennari; Giordana Gennari 6 1University of Fribourg, Department of Geosciences, Earth Sciences, Ch. du Musée 6, 1700 Fribourg, Switzerland 6Corresponding author. E-mail: giordana.gennari@unifr.ch Search for other works by this author on: GSW Google Scholar Thomas Rosenberg; Thomas Rosenberg 2University of Bern, Institute of Geological Sciences, Baltzerstrasse 1-3, 3012 Bern, Switzerland3University of Bern, Oeschger Centre for Climate Change Research, Zähringerstrasse 25, 3012 Bern Switzerland Search for other works by this author on: GSW Google Scholar Silvia Spezzaferri; Silvia Spezzaferri 1University of Fribourg, Department of Geosciences, Earth Sciences, Ch. du Musée 6, 1700 Fribourg, Switzerland Search for other works by this author on: GSW Google Scholar Jean-Pierre Berger; Jean-Pierre Berger 1University of Fribourg, Department of Geosciences, Earth Sciences, Ch. du Musée 6, 1700 Fribourg, Switzerland Search for other works by this author on: GSW Google Scholar Dominik Fleitmann; Dominik Fleitmann 2University of Bern, Institute of Geological Sciences, Baltzerstrasse 1-3, 3012 Bern, Switzerland3University of Bern, Oeschger Centre for Climate Change Research, Zähringerstrasse 25, 3012 Bern Switzerland Search for other works by this author on: GSW Google Scholar Frank Preusser; Frank Preusser 2University of Bern, Institute of Geological Sciences, Baltzerstrasse 1-3, 3012 Bern, Switzerland 5Present address: Stockholm University, Department of Physical Geography and Quaternary Geology, 10691 Stockholm, Sweden Search for other works by this author on: GSW Google Scholar Mahmoud Al-Shanti; Mahmoud Al-Shanti 4Saudi Geological Survey, P.O. Box 54141, Jeddah 21514, Saudi Arabia Search for other works by this author on: GSW Google Scholar Albert Matter Albert Matter 2University of Bern, Institute of Geological Sciences, Baltzerstrasse 1-3, 3012 Bern, Switzerland Search for other works by this author on: GSW Google Scholar Journal of Foraminiferal Research (2011) 41 (3): 248–259. https://doi.org/10.2113/gsjfr.41.3.248 Article history received: 22 Sep 2009 accepted: 05 Mar 2011 first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Giordana Gennari, Thomas Rosenberg, Silvia Spezzaferri, Jean-Pierre Berger, Dominik Fleitmann, Frank Preusser, Mahmoud Al-Shanti, Albert Matter; FAUNAL EVIDENCE OF A HOLOCENE PLUVIAL PHASE IN SOUTHERN ARABIA WITH REMARKS ON THE MORPHOLOGICAL VARIABILITY OF HELENINA ANDERSENI. Journal of Foraminiferal Research 2011;; 41 (3): 248–259. doi: https://doi.org/10.2113/gsjfr.41.3.248 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract Although foraminifera have been found living in inland saline lakes isolated from the sea, this phenomenon has rarely been recognized in the fossil record. This study documents the occurrence of benthic foraminifera in Holocene lake sediments located nearly 500 km inland from the Red Sea, in the Al-Mundafan region of southern Saudi Arabia. The lake formed during a regional pluvial period, 10,500–6000 yr BP. The presence of foraminifera and brackish charophytes in the studied section represent an interval when the lake was slightly brackish due to high evaporation. The studied sediments yielded a bispecific benthic foraminiferal fauna comprised of Helenina anderseni and Trichohyalus aguayoi, as well as the brackish charophyte genus Lamprothamnium. The benthic foraminifera are species characteristic of mangrove swamps, salt marshes, and lagoons, which are environments currently widespread along the Red Sea coasts. Because the Al Mundafan area was never connected to the sea during the Quaternary, wading birds must have been the vector that transported the foraminifera to the paleolake. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2158528018 date "2011-07-01" @default.
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• W2158528018 title "FAUNAL EVIDENCE OF A HOLOCENE PLUVIAL PHASE IN SOUTHERN ARABIA WITH REMARKS ON THE MORPHOLOGICAL VARIABILITY OF HELENINA ANDERSENI" @default.
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• W2158528018 doi "https://doi.org/10.2113/gsjfr.41.3.248" @default.
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