Sipuncula of the western North Atlantic. Bulletin of the AMNH ; v. 152, article 3

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dc.contributor.authorCutler, Edward Bayler.en_US
dc.date.accessioned2005-10-06T14:24:03Z
dc.date.available2005-10-06T14:24:03Z
dc.date.issued1973en_US
dc.descriptionp. 105-204 : ill., maps ; 27 cm.en_US
dc.descriptionIncludes bibliographical references (p. 199-204).en_US
dc.description.abstract"More than 8300 sipunculans from more than 500 stations of the east coast of the United States are identified and described. The area under investigation extends from Nova Scotia to cape Kennedy, Florida, in depths from 10 to 5400 meters. Several abiotic factors of the environment (topography, currents, temperature, and sediments) are described. Each species is characterized morphologically and also in terms of depth, latitude, sediment, and temperature. A key is given for the identification of all the 26 species collected. Distribution maps for the species are presented, as well as figures showing their morphology. In the description of each species, particular attention is paid to variation in morphology due to ontogeny. Several combinations of existing species names are suggested. Based on abiotic niche features, the species are grouped into four major ecological units: southern, shallow, warm water; northern, shallow, cold water; slope; and abyssal. Competitive exclusion operates within each of these groups except the abyssal fauna; this group has more sympatric species than the shallower groups and their morphology is less distinctive. One possible explanation is the limited magnitude of the significant environmental differences, which may be too small to be effective. Another is that the relatively low density greatly reduces the likelihood of two worms coming into contact and competing for given resources. The continental slope may not be an ecotone, but ecotones may exist along its upper and lower boundaries. The existence of a shallow-water, zoogeographical barrier at Cape Hatteras is reaffirmed, but the role of currents on larval dispersal may be as important as temperature in maintaining this barrier. A barrier on the slope, maintained by the effect of the bottom currents on larval dispersion just south of Cape Hatteras (latitude 34°20'-34°30'N), is proposed. Three of the four ecological groupings of species fit into pre-existing zoogeographical provinces (Carolinian, Nova Scotian, and Abyssal Atlantic subarea), but a new province (Atlantic Transitional) is proposed for the slope. Sipunculans in the Virginian Province are extremely rare. Two pieces of evidence support the concept that abyssal, cold-water fauna is ancestral to the warmer, shallow-water fauna"--P. 107.en_US
dc.format.extent20970317 bytes
dc.format.mimetypeapplication/pdf
dc.identifier.urihttp://hdl.handle.net/2246/601
dc.languageengen_US
dc.language.isoen_US
dc.publisherNew York : [American Museum of Natural History]en_US
dc.relation.ispartofseriesBulletin of the American Museum of Natural History ; v. 152, article 3en_US
dc.subject.lcshSipuncula -- Atlantic Coast (U.S.)en_US
dc.subject.lcshSipuncula -- North Atlantic Ocean.en_US
dc.titleSipuncula of the western North Atlantic. Bulletin of the AMNH ; v. 152, article 3en_US
dc.typetexten_US

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Bulletin of the American Museum of Natural History