@article {82,
	title = {Response of Mediterranean coralline algae to ocean acidification and elevated temperature},
	journal = {Global Change BiologyGlobal Change Biology},
	volume = {15},
	number = {8},
	year = {2009},
	note = {http://DD8GH5YX7K.search.serialssolutions.com?ctx_ver=Z39.88-2004\&ctx_enc=info\%3Aofi\%2Fenc\%3AUTF-8\&rfr_id=info:sid/summon.serialssolutions.com\&rft_val_fmt=info:ofi/fmt:kev:mtx:journal\&rft.genre=article\&rft.atitle=Response+of+Mediterranean+coralline+algae+to+ocean+acidification+and+elevated+temperature\&rft.jtitle=Global+Change+Biology\&rft.au=Martin\%2C+Sophie\&rft.au=Gattuso\%2C+Jean-Pierre\&rft.date=2009-08-01\&rft.pub=Blackwell+Publishers+Ltd\&rft.issn=1354-1013\&rft.eissn=1365-2486\&rft.volume=15\&rft.issue=8\&rft.spage=2089\&rft.externalDBID=n\%2Fa\&rft.externalDocID=202853632\&paramdict=en-UShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=1354-1013\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=1354-1013\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=1354-1013\&client=sydneylibu; U6 - ctx_ver=Z39.88-2004\&ctx_enc=info\%3Aofi\%2Fenc\%3AUTF-8\&rfr_id=info:sid/summon.serialssolutions.com\&rft_val_fmt=info:ofi/fmt:kev:mtx:journal\&rft.genre=article\&rft.atitle=Response+of+Mediterranean+coralline+algae+to+ocean+acidification+and+elevated+temperature\&rft.jtitle=Global+Change+Biology\&rft.au=Martin\%2C+Sophie\&rft.au=Gattuso\%2C+Jean-Pierre\&rft.date=2009-08-01\&rft.pub=Blackwell+Publishers+Ltd\&rft.issn=1354-1013\&rft.eissn=1365-2486\&rft.volume=15\&rft.issue=8\&rft.spage=2089\&rft.externalDBID=n\%2Fa\&rft.externalDocID=202853632\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c1828-680f3695c39fbe10f77e027fda95f02c750f1c3384b6289afc6fb34f5727178c1[]},
	pages = {2089},
	publisher = {Blackwell Publishers Ltd},
	address = {Oxford},
	abstract = {The effects of elevated partial pressure of CO2 ( p CO2) and temperature, alone and in combination, on survival, calcification and dissolution were investigated in the crustose coralline alga Lithophyllum cabiochae . Algae were maintained in aquaria during 1 year at near-ambient conditions of irradiance, at ambient or elevated temperature (+3 {\textdegree}C) and at ambient [ca. 400 parts per million (ppm)] or elevated p CO2 (ca. 700 ppm). Algal necroses appeared at the end of summer under elevated temperature first at 700 ppm (60\% of the thallus surface) and then at 400 ppm (30\%). The death of algae was observed only under elevated temperature and was two- to threefold higher under elevated p CO2. During the first month of the experiment, net calcification was significantly reduced under elevated p CO2. At the end of the summer period, net calcification decreased by 50\% when both temperature and p CO2 were elevated while no effect was found under elevated temperature and elevated p CO2 alone. In autumn and winter, net calcification in healthy algae increased with increasing temperature, independently of the p CO2 level, while necroses and death in the algal population caused a net dissolution at elevated temperature and p CO2. The dissolution of dead algal thalli was affected by elevated p CO2, being two- to fourfold higher than under ambient p CO2. These results suggest that net dissolution is likely to exceed net calcification in L. cabiochae by the end of this century. This could have major consequences in terms of biodiversity and biogeochemistry in coralligenous communities dominated by these algae. [PUBLICATION ABSTRACT]},
	keywords = {algae, Aquatic ecosystems, Biogeochemistry, carbon dioxide, Climate change, GEOLOGY, Global warming, Greenhouse gases, Ocean, Survival analysis, temperature, Water acidification},
	isbn = {1354-1013},
	author = {Sophie, Martin and Jean-Pierre, Gattuso}
}
@article {80,
	title = {Microbioerosion in Tahitian reefs: A record of environmental change during the last deglacial sea-level rise (IODP 310)},
	journal = {LethaiaLethaia},
	volume = {42},
	number = {3},
	year = {2009},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000268271800007\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=1502-3931\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=1502-3931\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=1502-3931\&client=sydneylibu; U6 - ctx_ver=Z39.88-2004\&ctx_enc=info\%3Aofi\%2Fenc\%3AUTF-8\&rfr_id=info:sid/summon.serialssolutions.com\&rft_val_fmt=info:ofi/fmt:kev:mtx:journal\&rft.genre=article\&rft.atitle=Microbioerosion+in+Tahitian+reefs\%3A+A+record+of+environmental+change+during+the+last+deglacial+sea-level+rise+\%28IODP+310\%29\&rft.jtitle=Lethaia\&rft.au=Heindel\%2C+Katrin\&rft.au=Wisshak\%2C+Max\&rft.au=Westphal\%2C+Hildegard\&rft.date=2009\&rft.issn=1502-3931\&rft.eissn=1502-3931\&rft.volume=42\&rft.issue=3\&rft.spage=322\&rft.epage=340\&rft.externalDBID=n\%2Fa\&rft.externalDocID=355036214\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-e4657-390b938fd41e95c9c216b6b54bd7e78d6eb04dcad18ef219794bba3112bf369e1[]},
	pages = {322-340},
	publisher = {WILEY-BLACKWELL},
	address = {MALDEN},
	abstract = {The main motivation for Integrated Ocean Drilling Program Expedition 310 to the Tahitian Archipelago was the assumption that the last deglacial sea-level rise is precisely recorded in the coral reefs of this far-field site. The Tahitian deglacial succession typically consists of coral framework subsequently encrusted by coralline algae and microbialites. The high abundance of microbialites is uncommon for shallow-water coral reefs, and the environmental conditions favouring their development are still poorly understood. Microbioerosion patterns in the three principal framework components (corals, coralline algae, microbialites) are studied with respect to relative light availability during coral growth and subsequent encrustation, in order to constrain the palaeobathymetry and the relative timing of the encrustation. Unexpectedly for a tropical, light-flooded setting, ichnotaxa typical for the deep-euphotic to dysphotic zone dominate. The key ichnotaxa for the shallow euphotic zone are scarce in the analysed sample set, and are restricted to the base of the deglacial succession, thus reflecting the deglacial sea-level rise. At the base of the deglacial reef succession, the ichnocoenoses present in the corals indicate shallower bathymetries than those in the encrusting microbialites. This is in agreement with radiocarbon data that indicate a time gap of more than 600 years between coral death and microbialite formation. At the top of the deglacial reef succession, in contrast, the microbioerosion patterns in the three framework components indicate a uniform palaeobathymetry, and radiocarbon ages imply that encrustation took place shortly after coral demise. An enigma arises from the fact that the ichnocoenoses imply photic conditions that appear very deep for zooxanthellate coral growth. During the deglacial sea-level rise increased nutrients and fluvial influx may have led to (seasonal?) eutrophication, condensing the photic zonation. This would have exerted stress on the coral ecosystem and played a significant role in initiating microbialite development.},
	keywords = {Abundance, AGE CALIBRATION, algae, BARRIER-REEF, CAL KYR BP, coral reefs, CORAL-REEFS, DP hunter, EUTROPHICATION-RELATED ALTERATIONS, Expedition 310, FRENCH-POLYNESIA, HUON-PENINSULA, INDIAN-OCEAN, last deglacial sea-level rise, Marine, microbialites, Microbioerosion, Microendoliths, Palaeobathymetry, PALEONTOLOGY, PAPUA-NEW-GUINEA, Sea level, Tahiti sea-level, YOUNGER DRYAS},
	isbn = {1502-3931, 0024-1164},
	author = {Heindel, Katrin and Wisshak, Max and Westphal, Hildegard}
}
