Environmental factors affecting large-bodied coral reef fish assemblages in the Mariana Archipelago. PLoS ONE. doi: 10.1371/journal.pone.0031374

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Report on the Status of Marine Protected Areas in Coral Reef Ecosystems of the United States. Volume 1: Marine Protected Areas Managed by U.S. States, Territories, and Commonwealths. NOAA Technical Memorandum CRCP 2 February 2007

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The Mariana Islands are on the edge of the Philippine Plate. They were formed by underwater volcanoes along the Marianas Trench. The northern islands are high volcanic islands and the southern islands, while volcanic in origin, are capped by uplifted limestone derived from coral reefs. The southern islands have the oldest and most developed reefs in the CNMI, which are predominantly located along the western (leeward) sides.

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Coral reef resilience to climate change in Saipan, CNMI; field-based assessments and implications for vulnerability and future management

Assessing relative resilience potential of coral reefs to inform management in the Commonwealth of the Northern Mariana Islands

Shallow-water Benthic Habitat Maps of American Samoa, Guam, and the Commonwealth of the Northern Mariana Islands (CNMI)

NOAA's Coral Reef Conservation Program SSMC4, 10th Floor 1305 East West Highway Silver Spring, MD 20910

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Located just north of Guam in the western Pacific, the Commonwealth of the Northern Mariana Islands is a three-hundred mile archipelago consisting of 14 islands, with a total land area of 183.5 square miles. The principal inhabited islands are Saipan, Guguan, Rota and Tinian. The northern, largely uninhabited islands are Farallon de Medinilla, Anatahan, Sariguan, Gudgeon, Alamagan, Pagan, Agrihan, Asuncion, Maug Islands, and Farallon de Pajaro. Saipan is approximately 3,300 miles west-southwest of Honolulu and 3000 miles north of Sydney. The majority of the CNMI's residents live on Rota, Tinian, and Saipan, the capital and largest of the Northern Mariana Islands.

Coral reef ecosystems in the CNMI are, on the whole, reasonably healthy. However, environmental stressors acting along with anthropogenic stressors, such as nonpoint source pollution and fishing pressure, have clearly affected areas in proximity to the populated southern islands. From a fisheries perspective, the northern islands and more distant banks and reefs appear to be in better condition than those closer to population centers.

Saipan has the most diverse types of coral reefs and associated habitats in the CNMI. A fringing and barrier reef system protects the majority of the beaches along the western side of the island, forming a 12.4 square mile shallow-water lagoon system. This environment contains large assemblages of seagrass, branching corals, and the last remaining mangroves in the CNMI. The western side of the island is the most populated and the coral reefs along these areas are negatively affected by human activity. Continuing sediment and nutrient pollution, combined with sporadic stressors such as outbreaks of crown-of-thorns starfish (COTS) and bleaching, affect many of Saipan's western and southeastern reefs. These impacts are compounded by an expanding tourism industry and direct damage from heavy visitor use.

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Potential larval sources, destinations, and self-seeding in the Mariana Archipelago documented using ocean drifters (Journal of Oceanography, 2014)

The NOAA Coral Reef Conservation Program (CRCP) is a partnership between the NOAA Line Offices that work on coral reef issues: the National Ocean Service, the National Marine Fisheries Service, the Office of Oceanic and Atmospheric Research, and the National Environmental Satellite, Data and Information Service. The CRCP brings together expertise from across NOAA for a multidisciplinary approach to managing and understanding coral reef ecosystems.

Improving Monitoring and Management of the Saipan Lagoon through the Integration of Ground Surveys with Detailed Habitat Mapping

Appearing as solitary forms in the fossil record more than 400 million years ago, corals are extremely ancient animals that evolved into modern reef-building forms over the last 25 million years. Continue Reading →

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