@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 {45,
	title = {Syn-depositional alteration of coral reef framework through bioerosion, encrustation and cementation: Taphonomic signatures of reef accretion and reef depositional events},
	journal = {Earth Science ReviewsEarth Science Reviews},
	volume = {86},
	number = {1},
	year = {2008},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000252555200006\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0012-8252\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0012-8252\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0012-8252\&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=Syn-depositional+alteration+of+coral+reef+framework+through+bioerosion\%2C+encrustation+and+cementation\%3A+Taphonomic+signatures+of+reef+accretion+and+reef+depositional+events\&rft.jtitle=Earth+Science+Reviews\&rft.au=Perry\%2C+C.T\&rft.au=Hepburn\%2C+L.J\&rft.date=2008\&rft.pub=Elsevier+B.V\&rft.issn=0012-8252\&rft.eissn=1872-6828\&rft.volume=86\&rft.issue=1\&rft.spage=106\&rft.epage=144\&rft_id=info:doi/10.1016\%2Fj.earscirev.2007.08.006\&rft.externalDocID=doi_10_1016_j_earscirev_2007_08_006\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c5256-915e05a14e5ea93ce793d23559bd625e1d7b8e2d534559ac12bcd21ad68d10fd1[]},
	pages = {106-144},
	publisher = {Elsevier B.V},
	address = {AMSTERDAM},
	abstract = {The development of coral reef framework and the preservational character of both in-situ and rubble coral is strongly influenced by a range of physical, chemical and biologically-mediated taphonomic processes. These operate at, or just below, the reef framework-water interface and can be defined as having either a constructive or destructive effect upon primary reef framework (i.e., coral) constituents. Constructional activities add additional calcium carbonate to the primary framework structure via secondary framework growth and early cementation. Destructive processes, which remove or degrade primary (and secondary) framework carbonate, are associated with the effects of either physical (mainly storm) disturbance or biological erosion (termed bioerosion). Key bioeroding groups include the grazing fish and echinoid groups, as well as the activities of an array of infaunal borers. These include specific groups of sponges, bivalves and worms (termed macroborers), as well as cyanobacteria, chlorophytes, rhodophytes and fungi (termed microborers). The relative importance of each process and the rates at which they operate vary spatially across individual reef systems. In addition, many of these processes leave distinctive signatures on, or in, the coral framework. In some cases (e.g., calcareous encrusters) these are the skeletons of the organisms themselves, whilst in other cases the organism may leave behind a trace of their activity (e.g., macro- and microborers). These represent useful palaeoenvironmental tools, firstly because they often have good preservation potential and, secondly because the range and extent of many of the individual species, groups and processes involved exhibit reasonably well-constrained environment and/or depth-related distributions. As a result these taphonomically important organisms or processes can be used to delineate between reef environments in core or outcrop, and to aid the interpretation of reef depositional processes and {\textquoteright}events{\textquoteright}. This review summarises current understanding regarding the distribution of these species/processes within contemporary reef settings and considers the suites of taphonomic signatures that may aid in the recognition and interpretation of depositional environments and events. {\textcopyright} 2007 Elsevier B.V. All rights reserved.},
	keywords = {Accretion, ACROPORA-PALMATA FRAMEWORK, Animal fossils, ATOL-DAS-ROCAS, bioerosion, Borers, boring organisms, BRITISH-WEST-INDIES, calcareous encrusters, Calcium, Calcium carbonate, Calcium carbonates, CALIBRATED C-14 DATES, Carbonates, CARIBBEAN FRINGING REEF, CAVITY-DWELLERS COELOBITES, cements, coral reefs, Cores, Echinoida, encrustation, Fungi, GEOSCIENCES, MULTIDISCIPLINARY, grazing, GREAT-BARRIER-REEF, INTERTIDAL MANGROVE PEAT, MACROBORERS, Meiobenthos, microborers, ORGANISMS, palaeoecology, palaeoenvironments, Paleoecology, PHYTOPLANKTON, Preservation, reef taphonomy, Reefs, SEA-LEVEL CHANGES, Sedimentary environments, ST-CROIX SHELF},
	isbn = {0012-8252},
	author = {Perry, C. T. and Hepburn, L. J.}
}
@inbook {48,
	title = {The endolithic guild: an ecological framework for residential cavities in hard substrates},
	booktitle = {Current Developments in Bioerosion},
	series = {Erlangen Earth Conference Series},
	year = {2008},
	month = {2008/01/01},
	pages = {3-20},
	publisher = {Springer Berlin Heidelberg},
	organization = {Springer Berlin Heidelberg},
	chapter = {1},
	keywords = {bioclaustrations, bioerosion, classification, ECOLOGY, evolution, guild concept, Paleoecology},
	isbn = {978-3-540-77597-3},
	author = {Tapanila, Leif},
	editor = {Wisshak, Max and Tapanila, Leif}
}
@article {51,
	title = {Trypanites ichnofacies: Palaeoenvironmental and tectonic implications. A case study from the Miocene disconformity at Foz da Fonte (Lower Tagus Basin, Portugal)},
	journal = {Palaeogeography, Palaeoclimatology, PalaeoecologyPalaeogeography, Palaeoclimatology, Palaeoecology},
	volume = {292},
	number = {1},
	year = {2010},
	note = {http://www.sciencedirect.com/science/article/pii/S0031018210001513http://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=Trypanites+ichnofacies\%3A+Palaeoenvironmental+and+tectonic+implications.+A+case+study+from+the+Miocene+disconformity+at+Foz+da+Fonte+\%28Lower+Tagus+Basin\%2C+Portugal\%29\&rft.jtitle=Palaeogeography\%2C+Palaeoclimatology\%2C+Palaeoecology\&rft.au=Santos\%2C+Ana\&rft.au=Mayoral\%2C+Eduardo\&rft.au=da+Silva\%2C+Carlos+Marques\&rft.au=Cach\%C3\%A3o\%2C+M\%C3\%A1rio\&rft.date=2010\&rft.issn=0031-0182\&rft.eissn=1872-616X\&rft.volume=292\&rft.issue=1-2\&rft.spage=35\&rft.epage=43\&rft.externalDBID=n\%2Fa\&rft.externalDocID=50859995\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c1883-d15fb2a2b0af60533fd5614cb059b037c1bca4a8f8bd1a1a532edde8e4882aba1[]},
	pages = {35-43},
	publisher = {Elsevier B.V},
	address = {AMSTERDAM},
	abstract = {A well preserved bioeroded surface occurs at the unconformity separating Cretaceous limestones and Lower Miocene sediments, outcropping on the western coast of the Peninsula of Set{\'u}bal (Central West Portugal). The ichnoassemblage present in this bioeroded surface is herein assigned to the Trypanites ichnofacies. The preservation characteristics of the borings reflect several episodes of encrustation/boring and physical erosion. The erosional truncation of bioerosive structures, and the predominant preservation of the largest borings (Gastrochaenolites isp.) in the ichnocoenoses are herein related with repeated phases of bioerosion and physical abrasion occurred during an Early Miocene transgressive pulse. The recognition of this bioeroded transgressive surface also allowed confirming the presence, at that time, of an emergent topographic relief related to salt domes formed earlier, probably already during Palaeogene times. {\textcopyright} 2010 Elsevier B.V. All rights reserved.},
	keywords = {Abrasion, ANE, Portugal, bioerosion, Burdigalian, COMMUNITIES, Disconformity, Endolithic communities, evolution, Gastrochaenolites, GEOGRAPHY, PHYSICAL, GEOSCIENCES, MULTIDISCIPLINARY, ICHNOLOGY, Miocene, NEOGENE, ORDOVICIAN HARDGROUNDS, palaeo studies, Paleoecology, PALEONTOLOGY, Preservation, ROCKY-SHORE, SEA-LEVEL, STRATIGRAPHY, trace fossils, Transgressive surface, Trypanites ichnofacies},
	isbn = {0031-0182},
	author = {Santos, Ana and Mayoral, Eduardo and da Silva, Carlos Marques and Cach{\~a}o, M{\'a}rio and Kullberg, Jos{\'e} Carlos}
}
