{"refrec":{"BRefID":38609,"RR":"<b>Nakamura, T.; van Woesik, R.</b> (2001). Water-flow rates and passive diffusion partially explain differential survival of corals during the 1998 bleaching event. <i>Mar. Ecol. Prog. Ser. 212</i>: 301-304","BEntID":38609,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Mar. Ecol. Prog. Ser. 212</i>: 301-304","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Nakamura, T.; van Woesik, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Nakamura, T.; van Woesik, R.","Englishabstract":"In the western Pacific during 1998, coral bleaching, or the paling of corals through loss of pigmentation or loss of symbiotic algae (zooxanthellae), coincided with some of the warmest sea-surface temperatures (SSTs) on record. However, there was considerable spatial variation in coral survivorship; for example, corals of the same species at different locations around the Ryukyu Islands (Japan), within kilometers of each other, showed vastly different responses. Some locations experienced 100% coral mortality while other locations, nearby, suffered little coral mortality. Here we show experimental evidence for high survivorship of <i>Acropora digitifera</i> coral colonies that were subjected to both high SSTs (ranging from 26.22 to 33.65°C) and high-water flow (50 to 70 cm s<sup>-1</sup>), while corals that were subjected to both high SSTs and low-water flow (2 to 3 cm s<sup>-1</sup>) showed low survivorship. All experiments were conducted under high irradiance (~95% photosynthetically active radiation). We also empirically show that no coral mortality occurred when SSTs were below 30°C (ranging from 26.64 to 29.74°C) under similar flow regimes. The spatial differences in coral mortality during the 1998 bleaching event may have been, in part, a result of differences in water-flow rates that induced differential rates of passive diffusion, which varied among habitats.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Water-flow rates and passive diffusion partially explain differential survival of corals during the 1998 bleaching event","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2001,"MonPub":null,"DateUpdate":"2003-08-25","DateCreate":"2003-08-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000168017600025","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":38609,"PubliDate":2001,"Pagination":"301-304","XtraPublOfAnaID":null,"ISBN":null,"Volume":"212","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43354,"SerRR":"Marine Ecology Progress Series. 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