@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 {85,
	title = {Microborer ichnocoenoses in Quaternary corals from New Caledonia: reconstructions of paleo-water depths and reef growth strategies in relation to environmental changes},
	journal = {Quaternary Science ReviewsQuaternary Science Reviews},
	volume = {30},
	number = {19},
	year = {2011},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000295387000031\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0277-3791\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0277-3791\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0277-3791\&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=Microborer+ichnocoenoses+in+Quaternary+corals+from+New+Caledonia\%3A+reconstructions+of+paleo-water+depths+and+reef+growth+strategies+in+relation+to+environmental+changes\&rft.jtitle=Quaternary+Science+Reviews\&rft.au=R\%C3\%A9my\%2C+Richet\&rft.au=V\%C3\%A9ronique\%2C+Chazottes\&rft.au=Guy\%2C+Cabioch\&rft.au=Norbert\%2C+Frank\&rft.date=2011\&rft.pub=Elsevier+Ltd\&rft.issn=0277-3791\&rft.eissn=1873-457X\&rft.volume=30\&rft.issue=19\&rft.spage=2827\&rft.epage=2838\&rft_id=info:doi/10.1016\%2Fj.quascirev.2011.06.019\&rft.externalDocID=doi_10_1016_j_quascirev_2011_06_019\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c2161-66f09c8dadfa839a11bdff8461a54b0cc2e81dc6920db46c84d411ee80a492031[]},
	pages = {2827-2838},
	publisher = {Elsevier B.V},
	address = {OXFORD},
	abstract = {Coral reef growth and development depend on several environmental factors, including tectonic and climatic parameters and local ecological drivers. Reef growth is especially sensitive to sea-level variations. Paleo-water depth reconstructions are essential tools used to determine reef growth patterns during different periods of reef growth. Assemblages of corals and/or coralline algae have been commonly used in such paleodepth reconstructions. This study shows that using microendolith ichnocoenoses can sometimes provide better accuracy than traditional coralgal analyses, particularly in the depth-range 0-10 m where coralgal assemblages usually show broad distribution ranges. Holocene and Pleistocene cores from two barrier reef sites on the west coast of Grande Terre in New Caledonia are examined here. Holocene reef development at these sites feature examples of microendolith ichnocoenoses that document rapid environmental changes and small sea-level variations of about 2-5 m in amplitude, and record these changes with more accuracy than coral and coralline algae assemblages which are highly dependant on the hydrodynamic energy of the setting. During the Pleistocene, which was less chronologically constrained, the microendolith ichnocoenoses also reflect paleo-water depths and reef-growth patterns at different periods of reef history. {\textcopyright} 2011 Elsevier Ltd.},
	keywords = {algae, Animal fossils, Climatic changes, Coasts, COMMUNITIES, coral reefs, Coral reefs and islands, Coralgal assemblages, Corals, Cores, development, Energy, Environmental aspects, Environmental changes, environmental factors, FRINGING REEFS, Fungi, GEOGRAPHY, PHYSICAL, GEOSCIENCES, MULTIDISCIPLINARY, GREAT-BARRIER-REEF, GROWTH, Growth patterns, Holocene, Hydrodynamics, INDIAN-OCEAN, ISEW, Pacific, New Caledonia, ISEW, Pacific, New Caledonia, Grande Terre, Marine, Microbioerosion, Microendolith assemblages, New Caledonia, NINO-SOUTHERN-OSCILLATION, palaeo studies, palaeoenvironments, Paleo-water depth, Pleistocene, Reef, Sea level changes, SEA-LEVEL CHANGES, SW PACIFIC, Tectonics (Geology), WEST PACIFIC},
	isbn = {0277-3791},
	author = {R{\'e}my, Richet and V{\'e}ronique, Chazottes and Guy, Cabioch and Norbert, Frank and Burr George, S.}
}
@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}
}
@article {63,
	title = {Microbial infestation of carbonate substrates planted on the St. Croix shelf, West Indies},
	journal = {GSA BulletinGSA Bulletin},
	volume = {87},
	number = {11},
	year = {1976},
	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=Microbial+infestation+of+carbonate+substrates+planted+on+the+St.+Croix+shelf\%2C+West+Indies\&rft.jtitle=Bulletin+of+the+Geological+Society+of+America\&rft.au=Perkins\%2C+Ronald+D\&rft.date=1976\&rft.issn=0016-7606\&rft.eissn=1943-2674\&rft.volume=87\&rft.issue=11\&rft.spage=1615\&rft.epage=1628\&rft_id=info:doi/10.1130\%2F0016-7606\%281976\%2987\%3C1615\%3AMIOCSP\%3E2.0.CO\%3B2\&rft.externalDBID=n\%2Fa\&rft.externalDocID=368562863\&paramdict=en-UShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0016-7606\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0016-7606\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0016-7606\&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=Microbial+infestation+of+carbonate+substrates+planted+on+the+St.+Croix+shelf\%2C+West+Indies\&rft.jtitle=Bulletin+of+the+Geological+Society+of+America\&rft.au=Perkins\%2C+Ronald+D\&rft.date=1976\&rft.issn=0016-7606\&rft.eissn=1943-2674\&rft.volume=87\&rft.issue=11\&rft.spage=1615\&rft.epage=1628\&rft_id=info:doi/10.1130\%2F0016-7606\%281976\%2987\%3C1615\%3AMIOCSP\%3E2.0.CO\%3B2\&rft.externalDBID=n\%2Fa\&rft.externalDocID=368562863\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c1581-3dcd8c13b20f6c7809433ae6bf71764f6730f4f183ca60c5b970907d370955831[]},
	pages = {1615-1628},
	publisher = {Geological Soc America},
	abstract = {1 Department of Geology, Duke University, Durham, North Carolina 27708 Carbonate substrates prepared from the shells of living organisms and inorganic calcite were planted on the St. Croix shelf and periodically harvested to determine the nature and extent of microbial infestation by endolithic organisms. Substrates, 1 to 10 mm in diameter, were mounted on plexiglass sheets and anchored at five sites at depths ranging from the intertidal to 30 m. Samples were harvested after exposure times ranging from 9 days to 18 months. Scanning electron microscope (SEM) examination of plastic-impregnated endoliths and their resultant microborings, in association with specimens isolated through acid dissolution of host substrates, formed the basis for this investigation. Blue-green algae were found to be the dominant microborers, and green algae were of secondary importance. Red algae and fungi were relatively scarce. In order of decreasing abundance, the following endolithic organisms were observed: Mastigocoleus testarum (blue-green alga), Plectonema terebrans (blue-green alga), Phaeophila engleri (green alga), Hyella sp. A (blue-green alga), Ostreobium brabantium (green alga), Calothrix sp. (blue-green alga), Ostreobium constrictum (green alga), moniliform fungus(?), Conchocelis stage of Porphyra sp. (red alga), Scytonema (blue-green alga), microboring sponge, reticulate fungus(?), and Hyella sp. B (blue-green alga). Initial infestation of planted substrates was detectable after exposure periods of as little as 9 days and heavy infestation within 2 to 4 months. Less than 10 percent of the grains exposed for 9 days were colonized by endoliths; after 4 months approximately 95 percent of the grains were colonized. The distributional patterns of microborers that infested substrates planted on the St. Croix shelf are believed to be environmentally controlled and may be applicable in the paleoecological analyses of ancient carbonates.},
	keywords = {Abundance, algae, Aquatic plants, ASW, Caribbean Sea, West Indies, calcite, Calothrix, Carbonates, Conchocelis, Cyanobacteria, Cyanophyta, Dissolution, Fungi, Grain, Hyella, INE, USA, Washington, INFESTATION, Interspecific relationships, Mastigocoleus testarum, Ostreobium, palaeoecology, palaeoenvironments, Phaeophila, PHYTOPLANKTON, Plectonema terebrans, Population Dynamics, Porphyra, Scanning electron microscopy, Scytonema, Seaweeds, Shells, Substrate preferences, USA, Wisconsin},
	isbn = {0016-7606},
	author = {Perkins, Ronald D. and Tsentas, Constantine I.}
}
@article {68,
	title = {Experimental studies on microbial bioerosion at Lee Stocking Island, Bahamas and One Tree Island, Great Barrier Reef, Australia: implications for paleoecological reconstructions},
	journal = {LethaiaLethaia},
	volume = {33},
	number = {3},
	year = {2000},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000166704600005\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0024-1164\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0024-1164\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0024-1164\&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=Experimental+studies+on+microbial+bioerosion+at+Lee+Stocking+Island\%2C+Bahamas+and+One+Tree+Island\%2C+Great+Barrier+Reef\%2C+Australia\%3A+Implications+for+paleoecological+reconstructions\&rft.jtitle=Lethaia\&rft.au=Vogel\%2C+K\&rft.au=Gektidis\%2C+M\&rft.au=Golubic\%2C+S\&rft.au=Kiene\%2C+W.E\&rft.date=2000\&rft.issn=0024-1164\&rft.eissn=1502-3931\&rft.volume=33\&rft.issue=3\&rft.spage=190\&rft.epage=204\&rft.externalDBID=n\%2Fa\&rft.externalDocID=30771793\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c1750-639394f2d6aae7875074d815a526b45853933d13fdae8551a832da1f82b5b6b1[]},
	pages = {190-204},
	publisher = {TAYLOR \& FRANCIS AS},
	address = {Oxford, UK},
	abstract = {Different kinds of experimental calcareous substrates were exposed at Lee Stocking Island (Bahamas) and One Tree Island (Great Barrier Reef, Australia) to study which endolithic bacteria, algae and fungi contribute to bioerosion and what their bioerosion rates are. The sites at Lee Stocking Island were several leeward shallow water and several windward shallow and deep-water positions (from the Acropora palmata reef at 2 m down to 275 m depth). At One Tree Island, the experiments were conducted in patch reefs treated with P and N to study the influence of mineral nutrients on bioerosion. The exposure periods ranged from 1 week to 2 years. The micritic carbonate substrates exposed on Lee Stocking Island contained 6 genera with 15 species of cyanobacteria, green and red algae, and different kinds of microendolithic heterotrophs. The mean values of bioerosion rates measured between 1 to 2 g/m 2 /y at 275 m and 520 g/m 2 /y at one of the leeward sites. The composition of the endolithic community and the bioerosion rates changed over time. At One Tree Island, shell pieces of Tridacna were used as substrate exposed for 5 months to endolith activity. Five genera and 6 species of cyanobacteria, green and red algae and different kinds of heterotrophic microendoliths were found with bioerosion rates of 20{\textendash}30 g/m 2 /y. There are differences in abundance of taxa between Lee Stocking Island and One Tree Island. The introduction of nutrients had no apparent impact on the microborer community. Controlling factors for the distribution and abundance of microborers are mainly light, but also the kind of substrate and, possibly, the biogeographic position. The results support the paleoecological importance of microendoliths.},
	keywords = {Acropora palmata, algae, ASW, Caribbean Sea, Bahamas, Exuma Cays, Lee Stocking I, Bacteria, Bahamas, barrier reefs, Biodegradation, bioerosion, boring organisms, Carbonates, Colonization, Community composition, Comparative studies, coral reefs, CORAL-REEFS, Cyanophyta, ECOLOGY, Endoliths, Environmental impact, Fungi, Great Barrier Reef, Heterotrophic organisms, ICHNOLOGY, INFESTATION, ISEW, Australia, Queensland, Great Barrier Reef, One Tree I, LAGOONS FRENCH-POLYNESIA, Light effects, Marine, MICROBORINGS, Microendoliths, MOOREA, Nutrients (mineral), palaeoecology, Paleoecology, PALEONTOLOGY, Quantitative distribution, Reefs, SEDIMENTS, Shallow water, Substrate preferences, Tridacna, WATER},
	isbn = {0024-1164},
	author = {Vogel, Klaus and Gektidis, Marcos and Golubic, Stjepko and Kiene, William E. and Radtke, Gudrun}
}
@article {56,
	title = {Bathymetric distribution of ichnocoenoses from recent subtropical algal nodules off Fraser Island, eastern Australia},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGYPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {369},
	number = {Journal Article},
	year = {2013},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000315127200006\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0031-0182\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0031-0182\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0031-0182\&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=Bathymetric+distribution+of+ichnocoenoses+from+recent+subtropical+algal+nodules+off+Fraser+Island\%2C+eastern+Australia\&rft.jtitle=Palaeogeography\%2C+Palaeoclimatology\%2C+Palaeoecology\&rft.au=Bassi\%2C+Davide\&rft.au=Iryu\%2C+Yasufumi\&rft.au=Braga\%2C+Juan+C\&rft.au=Takayanagi\%2C+Hideko\&rft.date=2013-01-01\&rft.issn=0031-0182\&rft.eissn=1872-616X\&rft.volume=369\&rft.spage=58\&rft.epage=66\&rft.externalDBID=n\%2Fa\&rft.externalDocID=52283827\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-e4306-3f828378db96d07f103a450d602212a3364d83b474126a4dc1035dde290f14041[]},
	pages = {58-66},
	publisher = {Elsevier B.V},
	address = {AMSTERDAM},
	abstract = {Coralline algal nodules living on the subtropical shelf off Fraser Island, eastern Australia, from the inner to the uppermost outer-shelf, from 28 to 117 m water depth are pervasively bioeroded. Five ichnogenera have been identifed as nodule borers, comprising one ichnotaxon attributed to bivalves (Gastrochaenolites), one to sponges (Entobia) and three to polychaetes and barnacles (Trypanites, Maeandropolydora, Rogerella). Microtraces comparable to those produced by fungi, algae, bacteria and/or sponges are also present. Two ichnocoenoses have been recognised. The {\textquoteright}shallow{\textquoteright} water ichnocoenosis (EGTM) occurs at 60 m and shallower depths and includes all identified ichnogenera. The {\textquoteright}deep{\textquoteright} water ichnocoenosis (from 68 to 117 m) is characterised by Trypanites and the Trypanites/Maeandropolydora network (TM ichnocoenosis) with a generally higher boring density than in shallower nodules. Decreasing size of algal nodules and reduced thickness of the coralline thalli probably explain the decrease in diversity of ichnogenera with depth, as the larger bioeroders are excluded from the ichnoassemblages. Lower growth rates favour higher density of bioerosion in deeper algal nodules. (C) 2012 Elsevier B.V. All rights reserved.},
	keywords = {algae, AUSTRALIA, Bioeroder distribution, bioerosion, Coralline red algae, CRUSTOSE CORALLINE ALGAE, DESTRUCTION, FRAMEWORK, GEOGRAPHY, PHYSICAL, GEOSCIENCES, MULTIDISCIPLINARY, Ichnocoenosis, Ichnofacies, MACROBORERS, Marine, MECHANISMS, Nodules, OUTER-SHELF, PALEONTOLOGY, Recent, Reefs, STRATEGIES, Subtropical carbonates},
	isbn = {0031-0182},
	author = {Bassi, D. and Iryu, Y. and Braga, J. C. and Takayanagi, H. and Tsuji, Y.}
}
@article {40,
	title = {Influence of land runoff on rates and agents of bioerosion of coral substrates},
	journal = {Marine pollution bulletinMarine Pollution Bulletin},
	volume = {51},
	number = {1-4},
	year = {2005},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000227981800041\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0025-326X\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0025-326X\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0025-326X\&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=Influence+of+land+runoff+on+rates+and+agents+of+bioerosion+of+coral+substrates\&rft.jtitle=Marine+Pollution+Bulletin\&rft.au=Hutchings\%2C+Pat\&rft.au=Peyrot-Clausade\%2C+Mireille\&rft.au=Osnorno\%2C+Alicia\&rft.date=2005\&rft.issn=0025-326X\&rft.eissn=1879-3363\&rft.volume=51\&rft.issue=1-4\&rft.spage=438\&rft.epage=447\&rft.externalDBID=n\%2Fa\&rft.externalDocID=40341636\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c2431-12d5316fd10c8d6eb164af995488dd217f0bccb4de0bbcac310845b5645ce18a1[]},
	pages = {438-447},
	publisher = {PERGAMON-ELSEVIER SCIENCE LTD},
	address = {England},
	abstract = {Annually large volumes of fresh water laden with sediment are washed down the Daintree River in North Queensland into the Great Barrier Reef lagoon. To investigate the effects of land runoff on bioerosion, samples of recently killed colonies of Porites were laid at 6 sites on a cross shelf transect from Snapper Island at the entrance to the river to Osprey Reef, approximately 328 km from the river mouth out in the Coral Sea. Rates and agents of bioerosion were determined over 4 years and inshore sites exhibited significantly lower rates of total bioerosion than the other sites. Offshore sites experienced high rates of bioerosion primarily due to grazing and internal bioerosion by macroborers such as sponges and bivalves was also important at some of these sites. Inshore sites were covered in heavy layers of silt which inhibited colonization and growth of microborers, primarily algae. This resulted in lower levels of grazing than at offshore sites. However the activity of macroborers (primarily sponges and bivalves) was often high at these sites. The macroboring communities differed between sites and over time and it is hypothesised that these site differences were due to different levels of terrestrial runoff. These results are compared with those from French Polynesia where contaminated terrestrial runoff greatly influenced rates and agents of bioerosion. However other factors such as overfishing may also play an important role in some locations.},
	keywords = {algae, Algal Growth, Animals, Anthozoa, Anthozoa - growth \&amp, AUSTRALIA, Australia, Queensland, Australia, Queensland, Daintree, Australia, Queensland, Great Barrier Reef, Australia, Queensland, Queensland Plateau, Osprey Reef, barrier reefs, bioerosion, Biogenic deposits, Bivalves, Bivalvia, boring organisms, Colonization, Community composition, Conservation of Natural Resources, coral, Coral Sea, Corals, development, environmental factors, Environmental Monitoring, ENVIRONMENTAL SCIENCES, Fluvial deposits, Fluvial transport, French Polynesia, FRESHWATER BIOLOGY, Geologic Sediments, grazing, Great Barrier Reef, GREAT-BARRIER-REEF, GROWTH, ISE, Pacific, French Polynesia, ISEW, Australia, Queensland, Daintree, ISEW, Australia, Queensland, Great Barrier Reef, ISEW, Australia, Queensland, Queensland Plateau, Osprey Reef, ISEW, Coral Sea, Islands, Lagoons, LAGOONS FRENCH-POLYNESIA, LIZARD-ISLAND, Marine, MARINE \&amp, Marine molluscs, Marine pollution, microborers, MID-SHELF, Mollusks, On-site Investigations, Pacific, French Polynesia, PARROTFISHES FAMILY SCARIDAE, Population Dynamics, Porifera, PORITES, Rain, Reefs, River discharge, River Mouth, Rivers, Runoff, Sediment, Sediment Contamination, Sediment transport, Sediment-water interface, SEDIMENTATION, Silt, Sipunculans, Skeleton, SPARISOMA-VIRIDE, Sponges, Substrates, Terrigenous sediments, Water Movements},
	isbn = {0025-326X},
	author = {Hutchings, Pat and Peyrot-Clausade, Mireille and Osnorno, Alicia}
}
@article {14,
	title = {Bioerosion of intertidal limestone, Co. Clare, Eire {\textemdash} 3: Zonation, process and form},
	journal = {Marine GeologyMarine Geology},
	volume = {74},
	number = {1},
	year = {1987},
	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=Bioerosion+of+intertidal+limestone\%2C+Co.+Clare\%2C+Eire+\%E2\%80\%94+3\%3A+Zonation\%2C+process+and+form\&rft.jtitle=Marine+Geology\&rft.au=Trudgill\%2C+S.T\&rft.date=1987\&rft.pub=Elsevier+B.V\&rft.issn=0025-3227\&rft.eissn=1872-6151\&rft.volume=74\&rft.issue=1\&rft.spage=111\&rft.epage=121\&rft_id=info:doi/10.1016\%2F0025-3227\%2887\%2990009-0\&rft.externalDocID=doi_10_1016_0025_3227_87_90009_0\&paramdict=en-UShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0025-3227\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0025-3227\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0025-3227\&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=Bioerosion+of+intertidal+limestone\%2C+Co.+Clare\%2C+Eire+\%E2\%80\%94+3\%3A+Zonation\%2C+process+and+form\&rft.jtitle=Marine+Geology\&rft.au=Trudgill\%2C+S.T\&rft.date=1987\&rft.pub=Elsevier+B.V\&rft.issn=0025-3227\&rft.eissn=1872-6151\&rft.volume=74\&rft.issue=1\&rft.spage=111\&rft.epage=121\&rft_id=info:doi/10.1016\%2F0025-3227\%2887\%2990009-0\&rft.externalDocID=doi_10_1016_0025_3227_87_90009_0\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c1793-b603ff297e714745354171ae8cb3dfc01044bb31b504cf3fec7f4d649e9152dd1[]},
	pages = {111-121},
	publisher = {Elsevier B.V},
	abstract = {Scanning electron microscope photographs show that perforation by boring algae was the dominant agency in bioerosion in the mid-intertidal, with lichen penetration occurring in the upper intertidal and sponge boring in the lower. Chemical data showed that dissolution was possible but SEM observations suggested that it was of limited importance, dominating micro-surface form only in pools and the lower intertidal if algal and other biological covers were absent. Abrasion was also only locally important. Meso-scale form is interpreted in terms of the vertical distribution of bioerosive organisms, as influenced by the presence or absence of structural benches: slopes occurring within a bioerosive zone were dominated by forms produced by the particular organisms present.},
	keywords = {algae, ANE, Eire, Clare Cty, bioerosion, boring organisms, bottom erosion, Eire, intertidal environment, intertidal sedimentation, Lichenes, limestone, Marine, marine geology, Porifera, sedimentology},
	isbn = {0025-3227},
	author = {Trudgill, S. T.}
}
