A Comparison of the SNP Variation in the Calcification PMCA Gene of Lottia gigantea between a Santa Barbara Population and a More Acidic Monterey Bay Population

As the atmospheric levels of CO2 rise from human activity, the carbonic acid levels of the ocean increase, causing ocean acidification. This increase in acidity breaks down the calcified bodies that many marine organisms depend upon. Upwelling regions such as Monterey Bay in California have pH levels that are not expected to reach the open ocean for a few decades. This study reviews one of the common intertidal animals of the California coast, the Owl Limpet Lottia gigantea, and its genetic variation of the plasma membrane Ca2+ ATPase (PMCA) in relation to the acidity of its environment. The PMCA protein functions in the calcification process of many organisms. Specifically in limpets, this gene functions to form its protective shell. Single-nucleotide polymorphisms (SNPs) were found among five sections of the gene to determine variation between the acidic environment population in Monterey, California and the non-acidic environment population in Santa Barbara, California. While some variation was determined, the Monterey Bay and Santa Barbara Lottia gigantea populations are not significantly distinct at the PMCA gene. Sections B, C, and D were found to be linked. Only one location in Section B was found to have an amino acid change within an exon. Section A has the strongest connection to the sampling location. Monterey individuals were seen to be more genetically recognizable, while Santa Barbara individuals showed slightly more variation. Understanding the trends of ocean acidification, upwelling region activities, and population genetics will assist in determining how the ocean environment will behave in the future.

News from Academy Bay

Oil Spill in Galápagos. Derrame de Combustible en las Aguas de Galápagos. Beagle V: The Station's New Vessel. Children Conservationists. Niños Conservacionistas. Fruto del Empeño: Nuevo Edificio en San Cristóbal. New Building in Isla San Cristóbal. CDRS Director in Argentina. Van Straelen Gift. Change in Directorship at the CDRS. Cambio del Director en la Estación Científica. International Symposium/Workshop on the Herpetology of the Galápagos Islands: Research & Conservation.

News from Academy Bay

Proclamation of a Great Galapagos Marine Reserve. Recovery of the Marine Iguana Population After the El Niño Catastrophe. The Española Tortoises - a Very Special Case. A Botanical Workshop at the Darwin Station. The Campaign to Save the Hawaiian Petrel. Visitors to the Galapagos National Park. Re-opening of the Cristobal Bonifaz Building. Joint Operational Planning. Meeting of the Permanent Commission for the South Pacific. Galapagos Conservationists Receive WWF Award.

News from Academy Bay

Donacion Japonesa. Japanese Donation. Nuevo Gerente en la ECCD. New Manager for the CDRS. Un "Rose-breasted Grosbeak" en Galapagos. A Rose-breasted Grosbeak in Galapagos.

News from Academy Bay

Donation Made in Memory of Last Grandchild of Ecuador's First President. Deaths of CDF Board Members. Major Gift by Mrs. Louise Van Straelen-Poirier. Itasca to Galápagos. Station Research Vessel.

News from Academy Bay

Change in Directorship at the Charles Darwin Research Station. H.R.H. Prince Henri of Luxembourg Visits Galápagos. 25 More Years : Agreement Renewed Between the Ecuadorian Government and the Charles Darwin Foundation to Operate the Charles Darwin Research Station. A Dawn of Despair : Journey to Alcedo.

News from Academy Bay

Ecología de los Chivos Ferales (Capra hircus) en el Volcán Alcedo. Ecology of Feral Goats (Capra hircus) on Alcedo Volcano. Pepino War, 1992.

News from Academy Bay

One Hundred and Fifty Years Ago. The Great Fire on Isabela. Campaign for a CDF Endowment Fund. The Extraordinary Consequences of the Extraordinary El Niño. Eternal Vigilance.

Marine biology of the Sierra Leone River Estuary. 1. The physical environment

The Sierra Leone River Estuary is a relatively young drowned river valley, it is shallow except for a deep channel which passes close to the Freetown shoreline. The upper reaches merge into a network of creeks and channels fringed by large areas of mangrove swamps. It is a tidal estuary of the semi-mixed type with the saline oceanic water entering it on a diurnal cycle. The climate of Sierra Leone is marked by a very distinct change between a very wet rainy season and a dry season. The tidal range of the Estuary (spring 3.03m; neap 2.28m) does not impede normal use of the harbour. The tidal variations can be felt as far as 42 miles inland along the water courses of the Sierra Leone River and its tributaries. The volume of fresh water entering the Estuary is large during the rainy season and greatly reduced during the dry season. Consequently there is a marked fall in salinity during the rainy season and higher salinities due to the marine influence prevailing during the dry season. The nature of the shores and bottom, the hydrography and chemistry of the estuarine system have been outlined in relation to the prevailing climatic conditions.