Ar. Baco et al., The phylogenetic relationships of whale-fall vesicomyid clams based on mitochondrial COI DNA sequences, MAR ECOL-PR, 182, 1999, pp. 137-147
Whale skeletons on the deep-sea floor provide sulfide-rich habitats that ma
y act as stepping stones for the dispersal of animals dependent on chemoaut
otrophic production. However, the phylogenetic relationships between the fa
unas of whale falls, hydrothermal vents and colds seeps are not fully evalu
ated. Tb examine vesicomyid phylogenetic relationships, we collected 10 ves
icomyid clams from 2 whale falls on the California margin, one at 1240 m in
the Santa Catalina Basin and one at 960 m on the slope west of San Nicolas
Island. We then compared DNA sequences for a portion of the mitochondrial
cytochrome c oxidase subunit I gene from the whale-skeleton clams to those
from other clam populations in this taxonomically difficult family. Seven a
dult whale-fall vesicomyids clustered with clams identified as Vesicomya gi
gas, a species also found near hydrothermal vents in Guaymas Basin (Gulf of
California) and Middle Valley (Juan de Fuca Ridge). A single small whale-f
all individual clustered with clams identified as Calyptogena kilmeri, a sp
ecies found at cold seeps in Guaymas Basin, Monterey Bay, and along the Ore
gon Subduction Zone. A single small whale-fall clam clustered with Calyptog
ena elongata, a species found in anoxic California basins. Finally, a singl
e adult clam was difficult to assign to any previously examined species gro
up and could represent a new species in the 'gigas/kilmeri'' cryptic specie
s complex. With the inclusion of these vesicomyids, whale falls are known t
o share a total of 16 species with the faunas of deep-sea hydrothermal vent
s and cold seeps.