LITHODIDAE SAMOUELLE, 1819
publication ID |
https://doi.org/10.1111/j.1096-3642.2005.00178.x |
DOI |
https://doi.org/10.5281/zenodo.5490570 |
persistent identifier |
https://treatment.plazi.org/id/03D96F29-FF80-FFA6-FC66-FD65FDD00F49 |
treatment provided by |
Diego (2021-08-31 18:10:01, last updated by Plazi 2023-11-06 11:23:18) |
scientific name |
LITHODIDAE SAMOUELLE, 1819 |
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FAMILY LITHODIDAE SAMOUELLE, 1819 View in CoL
Remarks: Chevaldonné & Olu (1996), in their review of anomurans from vents and seeps and citing Suess et al. (1985) and Kulm et al. (1986), noted that the first record of any lithodid from such habitats was an illustration of what was clearly a lithodid in a sketch of the cold-seep community along the lower Oregonian Subduction Zone ( Suess et al., 1985: fig. 1; see Kulm et al., 1986, for map). From this same area but at slightly shallower depths, Carey et al. (1988) later reported Lopholithodes foraminatus , but it is not known if the earlier observations were of this same species. Tunnicliffe & Jensen (1987) noted that the earlier illustration might have been based on a species of Paralomis found by them at vents in the Juan de Fuca Ridge system (see below). Chevaldonné & Olu (1996) listed ‘two species and six occurrences not yet clearly assigned to species’. The situation has not changed appreciably since then (see below), and the review by Chevaldonné & Olu (1996) remains a well-written and succinct introduction to the literature on vent- and seep-associated lithodids. According to those authors, cold-seep lithodids are known from 250 to 2037 m depths, with one personal observation (M. Sibuet) of a depth of 3800 m in the Nankai Trough of the Japan subduction zone, whereas hydrothermal vent-associated lithodids are known from 350–2000 m. Many reports exist of unidentified lithodids at vent or seep sites (in some cases, such as the paper by Sassen et al., 1993, the species was later identified). Interestingly, despite their wide depth and geographical range, lithodids have not been reported from any of the EPR, Galapagos Rift (with the possible exception of a report by Guinot & Macpherson, 1987) or MAR systems ( Chevaldonné & Olu, 1996).
Species belonging to this large and widespread family are assumed to be vagrants as opposed to vent- or seep-endemics, even though some are known only from such sites (see below and also Chevaldonné & Olu (1996). Macpherson (1988) provided an in-depth revision and review of all known Atlantic species of this family; see Macpherson (2001) for a brief overview of the family in the Indo-Pacific.
Carey AG Jr, Stein DL, Taghon GL, DeBevoise AE. 1988. Biology and ecology of the Oregon continental shelf edge associated with the accretionary prism. In: De Luca MP, Babb I, eds. Global venting, midwater, and benthic ecological processes. Groton: NOAA, 137 - 149.
Chevaldonne P, Olu K. 1996. Occurrence of anomuran crabs (Crustacea: Decapoda) in hydrothermal vent and cold-seep communities: a review. Proceedings of the Biological Society of Washington 109 (2): 286 - 298.
Guinot D, Macpherson E. 1987. Une araignee de mer qui n' En est pas une. L'Univers du Vivant 24: 111 - 114.
Kulm LD, Suess E, Moore JC, Carson B, Lewis BT, Ritger SD, Kadko DC, Thornburg TM, Embley RW, Rugh WD, Massoth GJ, Langseth MG, Cochrane GR, Scamman RL. 1986. Oregon subduction zone: venting, fauna, and carbonates. Science 231: 561 - 566.
Macpherson E. 1988. Revision of the family Lithodidae Samouelle, 1819 (Crustacea, Decapoda, Anomura) in the Atlantic Ocean. Monografias de Zoologia Marina 2: 9 - 153.
Macpherson E. 2001. New species and new records of lithodid crabs (Crustacea, Decapoda) from the southwestern and central Pacific. Zoosystema 23 (4): 797 - 805.
Samouelle G. 1819. The Entomologistt's Useful Compendium; or An Introduction to the Knowledge of British Insects, comprising the best means of obtaining and preserving them, and a description of the apparatus generally used; together with the genera of Linne, and the modern method of arranging the Classes Crustacea, Myriapoda, Spiders, Mites and Insects, from their affinities and structure, according to the views of Dr. Leach. Also an explanation of the terms used in entomology; a calendar of the times of appearance and usual situations of near 3000 species of British insects; with instructions for collecting and fitting up objects for the microscope. London: Thomas Boys.
Sassen R, Brooks JM, MacDonal IR, Kennicutt MC II, Guinasso NL Jr, Requejo AG. 1993. Association of oil seeps and chemosynthetic communities with oil discoveries, upper continental slope, Gulf of Mexico. Transactions of the Gulf Coast Association of Geological Societies 43: 349 - 355.
Suess E, Carson B, Ritger SD, Moore JC, Jones ML, Kulm LD, Cochrane GR. 1985. Biological communities at vent sites along the subduction zone off Oregon. Bulletin of the Biological Society of Washington 6: 475 - 484.
Tunnicliffe V, Jensen RG. 1987. Distribution and behavior of the spider crab Macroregonia macrochira Sakai (Brachyura) around the hydrothermal vents of the northeast Pacific. Canadian Journal of Zoology 65: 2443 - 2449.
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