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Mulinia modesta

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(Redirected from Mulinia coloradoensis)

Mulinia modesta
Dry shells
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Order: Venerida
Family: Mactridae
Genus: Mulinia
Species:
M. modesta
Binomial name
Mulinia modesta
(Carpenter, 1864)
Synonyms[1]
  • Mactra modesta Carpenter, 1864
  • Mulinia coloradoensis Dall, 1894
  • Mactra coloradoensis Dall, 1894
  • Mulinia coloradoensis var. acuta Dall, 1894
  • Mulinia coloradoensis subsp. acuta (Dall, 1894)

Mulinia modesta is a species of clam belonging to the family Mactridae.[2]

Description

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The longitude of a medium sized specimen is 49 mm, the altitude 36.5 mm and the diameter 82 mm.

The shell is solid, rude and equilateral. It resembles Mulinia modesta, but is larger and has the posterior dorsal margin more arched. The base behind the posterior dorsal angle is somewhat concavely flexuous, and the surface anteriorly and on the dorsal area is marked with obsolete, little elevated radii.[3]

Distribution

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It is endemic to the northern and central Gulf of California. The clam is known to live in both brackish and fully marine habitats. It is a shallow-water filter feeder that prefers mud-sand bottoms.

Conservation history

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Prior to the diversion of water upstream in the Colorado River, this species might have been the most common mollusc in the Colorado River Delta, in the extreme northwestern region of the northern Gulf of California. It has been estimated to have constituted 80-90% of the clams throughout the delta and was so abundant that heaps of the shells formed ridges that stretched for miles. The density of Mulinia modesta has estimated to have been reduced from 25 to 50 per m2 to three per m2.

It has been hypothesized that the increase in salinity of the water and decrease of nutrient input from the river as a result of diversion and use of water led to the decline of the clam in the extreme northeastern region of the upper Gulf of California.[4][5] The clams are not harvested and are not affected by pressure from fishing.[6]

Studies of the clam have been used to infer the original extent the estuary in the absence of earlier survey data. Shells of the clam became sharply less prevalent about 65 km (40 mi) south of the river's mouth, constituting only 25% of shells in this area, and becoming rare to absent at a distance of 80 km (50 mi). These observations have been used to infer that the mixing zone of river and sea water probably extended as far as 65 km (40 mi) south of the river's mouth. Isotope analysis of oxygen in the shells of the clam have also been used to independently estimate rates of salinity, and the results from this approach were found to correspond with observations of the prevalence of the clam shells, and also to agree with numerical models proposed in the past.[7]

Ecology

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Damage to shells was used to assess the trophic importance of this species, and it was found to be a major source of food for crabs and predatory gastropods. On the basis of these studies, it was predicted that restoration of water flow in the Colorado River would result in an increase in this species, which would result in an increase of species that depend on it for food, including commercially valuable crabs.[8]

References

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  1. ^ "Mulinia modesta (Carpenter, 1864)". Global Biodiversity Information Facility. Retrieved 4 February 2023.
  2. ^ MolluscaBase eds. (2023). MolluscaBase. Mulinia modesta (P. P. Carpenter, 1864). Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=505739 on 2023-10-07
  3. ^ Dall, W. H. (1894). On some species of Mulinia from the Pacific coast. The Nautilus. 8(1): 5-6, pl. 1.
  4. ^ Rodriguez, Carlie A.; Flessa, Karl W.; Dettman, David L. (2001). "Effects of Upstream Diversion of Colorado River Water on the Estuarine Bivalve Mollusc Mulinia coloradoensis". Conservation Biology. 15 (1): 249–258. doi:10.1111/j.1523-1739.2001.99463.x. JSTOR 2641663. S2CID 36263274.
  5. ^ Karl W. Flessa, D.L. Dettman,"THE SOURCE OF SUSTENANCE FOR SIPHONING SHELLFISH IN THE COLORADO RIVER ESTUARY: NITROGEN ISOTOPES IN BIVALVE SHELLS REVEAL CHANGES IN NUTRIENT DELIVERY", GSA Denver Annual Meeting, Oct. 2007.
  6. ^ All, John D. (2006). "Colorado River Floods, Droughts, and Shrimp Fishing in the Upper Gulf of California, Mexico". Environmental Management. 37 (1): 111–125. Bibcode:2006EnMan..37..111A. doi:10.1007/s00267-004-0184-9. PMID 16362490. S2CID 3138679.
  7. ^ CA Rodriguez, KW Flessa, DL Dettman, "Macrofaunal and isotopic estimates of the former extent of the Colorado River Estuary, upper Gulf of California, Mexico", Journal of Arid Environments, Vol. 49, pp. 183-193, 2001.
  8. ^ Cintra-Buenrostro, Carlos E.; Flessa, Karl W.; Guillermo, Avila-Serrano (2005). "Who Cares About a Vanishing Clam? Trophic Importance of Mulinia coloradoensis Inferred from Predatory Damage". PALAIOS. 20 (3): 296–302. Bibcode:2005Palai..20..296C. doi:10.2110/palo.2004.p04-21. S2CID 86312221.
  • Huber, M. (2010). Compendium of bivalves. A full-color guide to 3,300 of the world's marine bivalves. A status on Bivalvia after 250 years of research. Hackenheim: ConchBooks. 901 pp., 1 CD-ROM
  • Coan, E. V.; Valentich-Scott, P. (2012). Bivalve seashells of tropical West America. Marine bivalve mollusks from Baja California to northern Peru. 2 vols, 1258 pp