@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 {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.}
}
@article {39,
	title = {Taphonomic differentiation of Acropora palmata facies in cores from Campeche Bank Reefs, Gulf of M{\'e}xico},
	journal = {SedimentologySedimentology},
	volume = {51},
	number = {1},
	year = {2004},
	note = {http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2\&SrcAuth=SerialsSolutions\&SrcApp=Summon\&KeyUT=000189022900004\&DestLinkType=FullRecord\&DestApp=WOShttp://www.syndetics.com/index.aspx?isbn=/sc.gif\&issn=0037-0746\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/mc.gif\&issn=0037-0746\&client=sydneylibu;http://www.syndetics.com/index.aspx?isbn=/lc.gif\&issn=0037-0746\&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=Taphonomic+differentiation+of+Acropora+palmata+facies+in+cores+from+Campeche+Bank+Reefs\%2C+Gulf+of+M\%C3\%A9xico\&rft.jtitle=Sedimentology\&rft.au=Blanchon\%2C+Paul\&rft.au=Perry\%2C+Chris+T\&rft.date=2004-02-01\&rft.issn=0037-0746\&rft.eissn=1365-3091\&rft.volume=51\&rft.issue=1\&rft.spage=53\&rft.epage=76\&rft.externalDBID=n\%2Fa\&rft.externalDocID=38345945\&paramdict=en-US U7 - Journal Article U8 - FETCH-LOGICAL-c4970-96b53f9878631f2810e7e2ff88b147700200530f5d4f1b76b63cca05182d02be1[]},
	pages = {53-76},
	publisher = {Blackwell Science Ltd},
	address = {Oxford, UK},
	abstract = {A common assumption in the geological analysis of modern reefs is that coral community zonation seen on the surface should also be found in cores from the reef interior. Such assumptions not only underestimate the impact of tropical storms on reef facies development, but have been difficult to test because of restrictions imposed by narrow-diameter cores and poor recovery. That assumption is tested here using large-diameter cores recovered from a range of common zones across three Campeche Bank reefs. It is found that cores from the reef-front, crest, flat and rubble-cay zones are similar in texture and coral composition, making it impossible to recognize coral assemblages that reflect the surface zonation. Taphonomic signatures imparted by variations in encrustation, bioerosion and cementation, however, produce distinct facies and delineate a clear depth zonation. Cores from the reef-front zone (2{\textendash}10  m depth) are characterized by sections of Acropora palmata cobble gravel interspersed with sections of in-place (but truncated) A. palmata stumps. Upper surfaces of truncated colonies are intensely bioeroded by traces of Entobia isp. and Gastrochaenolites isp. and encrusted by mm-thick crustose corallines before colony regeneration and, therefore, indicate punctuated growth resulting from a hurricane-induced cycle of destruction and regeneration. Cores from the reef crest/flat (0{\textendash}2  m depth) are also characterized by sections of hurricane-derived A. palmata cobble-gravels as well as in-place A. palmata colonies. In contrast to the reef front, however, these cobble gravels are encrusted by cm-thick crusts of intergrown coralline algae, low-relief Homotrema and vermetids, bored by traces of Entobia isp. and Trypanites isp. and coated by a dense, peloidal, micrite cement. Cores from the inter- to supratidal rubble-cay zone (+0{\textendash}5  m) are only composed of A. palmata cobble gravels and, although clasts show evidence of subtidal encrustation and bioerosion, these always represent processes that occurred before deposition on the cay. Instead, these gravels are distinguished on the basis of their limited bioerosion and marine cements, which exhibit fabrics formed in the intertidal zone. These results confirm that hurricanes have a major influence on facies development in Campeche Bank reefs. Instead of reflecting the surface coral zonation, each facies records a distinctive, depth-related set of taphonomic processes, which reflect colonization, alteration and stabilization following the production of new substrates by hurricanes.},
	keywords = {Acropora palmata, ASW, Mexico Gulf, Campeche Bank, bioerosion, Cementation, Colonization, Community structure, Elkhorn coral, Entobia, FRINGING-REEF, GEOLOGY, GRAND-CAYMAN, GREAT-BARRIER-REEF, HOLOCENE REEF, Hurricanes, intertidal environment, Marine, PLEISTOCENE CORAL-REEFS, reef crest, reef front, Reefs, Rubble rampart, Sea level, SEA-LEVEL CHANGES, Sedimentary facies, Sedimentary structures, SHELF-EDGE-REEF, ST-CROIX, STATES-VIRGIN-ISLANDS, taphofacies, Tropical depressions, Trypanites},
	isbn = {0037-0746},
	author = {Blanchon, Paul and Perry, Chris T.}
}
