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• W2002113856 abstract "Research Article| January 01, 2006 THE EFFECT OF SHALLOW MARINE HYDROTHERMAL VENT ACTIVITY ON BENTHIC FORAMINIFERA (AEOLIAN ARC, TYRRHENIAN SEA) Giuliana Panieri Giuliana Panieri * Dipartimento di Scienze della Terra e Geologico-Ambientali, Università di Bologna, Via Zamboni 67, 40126 Bologna, Italy *E-mail: panieri@geomin.unibo.it Search for other works by this author on: GSW Google Scholar Journal of Foraminiferal Research (2006) 36 (1): 3–14. https://doi.org/10.2113/36.1.3 Article history received: 26 Jul 2004 accepted: 01 Aug 2005 first online: 09 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 Giuliana Panieri; THE EFFECT OF SHALLOW MARINE HYDROTHERMAL VENT ACTIVITY ON BENTHIC FORAMINIFERA (AEOLIAN ARC, TYRRHENIAN SEA). Journal of Foraminiferal Research 2006;; 36 (1): 3–14. doi: https://doi.org/10.2113/36.1.3 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 An exceptional intensification of hydrothermal degassing activity occurred on November 3, 2002, to the east of Panarea, the smallest island of the Aeolian Archipelago (Tyrrhenian Sea, Italy). This event represents a unique opportunity to study benthic foraminiferal assemblages under the ecological stress of hydrothermal emissions in shallow (10–15 m water depth) environments. Benthic foraminifera (>63 μm) were collected by a scuba diver from sediments and seagrass of a Posidonia oceanica meadow off the coast of Panarea. Assemblages were studied to assess mortality and monitor the composition of benthic communities following the sudden venting event, characterized by an intensification of the emission of gases with high temperatures (40–50°C), low pH (~5), and high concentrations of HCl, HF, SO2 and some H2S. Surface foraminiferal assemblages were monitored during surveys on November 13–14, 2002, and May 22–24, 2003. In November 2002 (10 days after the venting event) agglutinated forms dominated the assemblages in sediment samples, whereas hyaline forms dominated the assemblages collected from the leaves and roots of P. oceanica. Six months later, in May 2003, when environmental conditions had returned to normal, sediment samples were barren of foraminifera, whereas the assemblages associated with P. oceanica were composed of allogromiids, which can be considered opportunistic pioneer species able to colonize disturbed environments. 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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• W2002113856 title "THE EFFECT OF SHALLOW MARINE HYDROTHERMAL VENT ACTIVITY ON BENTHIC FORAMINIFERA (AEOLIAN ARC, TYRRHENIAN SEA)" @default.
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