@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.}
}
