- Nov 29, 2008
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That is why the dead zone in the Gulf keeps growing and growing every yearSmart assed little cocksucker, aren't you. Since you linked to nothing but your stinking asshole, we know what your opinion is worth and where it comes from.I guarantee it's not temperature related at all. A
Coral has a lifespan anyway.
It could be some kind of foreign plankton or any damn thing, really.
So an aerial observation while flying overhead is their assessment?
No diving down for core samples to find anything out?
No consultation with Marine Biologists?
"We flew over and there was some white, so it must be global warming"
Thank you for your non-scientific conclusion without any studies done.
Now go choke yourself, Private Pyle!
http://cramp.wcc.hawaii.edu/Downloads/Publications/BC_Jokiel_2004_bleaching_chapter.pdf
The Bleaching Phenomenon Reef corals are symbioses that consist of an animal partner and dinoflagellate algae commonly known as zooxanthellae. This delicate association functions only within a very narrow range of environmental conditions in shallow tropical seas (Wells 1957). The symbiosis is thought to have developed as a means of coping with very low concentrations of nutrients in tropical marine waters (Muscatine and Porter 1977). This association provides benefits to both partners. The zooxanthellae are primary producers and supply their coral hosts with photosynthetic products vital to meeting their energetic requirements. In return, the zooxanthellae receive living space and nutrients in the form of waste metabolic products from the host. The tight cycling within the symbioses facilitates the high productivity and calcification rates observed in corals (Falkowski et al. 1984)
. “Coral bleaching”occurs when environmental conditions disrupt the symbiosis, leading the degeneration and/or expulsion of zooxanthellae from the coral host.As a result of photosynthetic pigment loss,the white skeleton becomes visible through the transparent coral tissue, giving the organism a “bleached”white appearance. Bleaching is fatal to the coral unless the symbiotic relationship can be quickly re-established. Reef corals play a central role in coral reef communities, so their continued health is of critical importance. Since the 1980s, spectacular regional bleaching events have occurred on coral reef areas throughout the world with increasing frequency and increasing geographic extent. These mass bleaching events correlate with elevated sea surface temperatures (SST). The mass bleaching phenomenon is believed to be associated with global warming due to anthropomorphic release of carbon dioxide and other gasses (reviewed by Jokiel and Coles 1990; Williams and Bunkley-Williams 1990; Glynn 1991, 1993; Goreau 1992; Pittock 1999; Fitt et al. 2001). The issue of global warming and mass coral bleaching will undoubtedly continue to be a major concern in the field of coral reef ecology