1999
DOI: 10.1007/s005310050273
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Why did ancient chemosynthetic seep and vent assemblages occur in shallower water than they do today?

Abstract: Cold-seep communities have relatively low diversity, are dominated by one or two taxa present in high density and high biomass in comparison with the surrounding fauna, and are restricted to aphotic habitats. Their associated heterotrophic fauna are usually distinctive from the fauna of their surroundings. In contrast, a more commonplace chemoautotrophically based community occurs in shallow photic habitats. The associated heterotrophic fauna includes many of the species typical of the surrounding communities … Show more

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Cited by 29 publications
(12 citation statements)
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“…Clear exceptions occur in all three petroleum seep assemblages and, less obviously, in the chemoautotrophic assemblages from Copano Bay. This bias towards the importance of predator refuges in chemoautotrophic assemblages supports the importance of predation in determining the distribution of chemoautotrophic communities (Callender & Powell 1999).…”
Section: Age-frequency Distributionssupporting
confidence: 53%
“…Clear exceptions occur in all three petroleum seep assemblages and, less obviously, in the chemoautotrophic assemblages from Copano Bay. This bias towards the importance of predator refuges in chemoautotrophic assemblages supports the importance of predation in determining the distribution of chemoautotrophic communities (Callender & Powell 1999).…”
Section: Age-frequency Distributionssupporting
confidence: 53%
“…It is also well documented in the fossil cold-seep record (Callender & Powell 1999). Several observations suggest that the nutrition of C. disjuncta could be mixotrophic.…”
Section: Conchocele Spmentioning
confidence: 93%
“…Van Dover (2000) reported rich decapod faunas at hydrothermal vents, which may explain the rich crustacean remnants (coprolites and crabantennae) at Zengõvárkony. On the other hand, Callender and Powell (1999) and Little et al (2002) demonstrated that vent/seep communities were continuously ubiquitous in space and time from neritic to bathyal environments. This leaves the door open for the challenging possibility that the decapods that left the rich coprolite deposits were shallow marine and vent-restricted animals.…”
Section: Micro-and Macrofaunamentioning
confidence: 99%