NOAA
IS COMMITTED TO PRESERVING THE NORTHWESTERN HAWAIIAN ISLANDS
“The designation concludes a multi-year process started in 2001 that has involved the active participation of the public under the National Marine Sanctuary Act. Under this designation, NOAA gains its first major role in a national monument," said Vice Admiral Conrad C. Lautenbacher, undersecretary of commerce for oceans and atmosphere and NOAA administrator. "The NOAA National Marine Sanctuary Program will manage marine areas, taking advantage of their current tools and broad new authority under the President’s Proclamation.” The U.S. Fish and Wildlife Services will manage the two existing refuges and the State of Hawaii will manage state controlled waters.
Ecosystems
of the Northwestern Hawaiian Islands
If they were laid atop the continental United States, the NWHI would cover a distance equal to that between New York City and Omaha, or Boston and the Florida Everglades. These ancient volcanic remnants with their fringes of truly wild coral reefs remind us of our past — when coral reefs and sea life across the planet thrived. The living coral reef colonies of the NWHI are a spectacular underwater landscape covering thousands of square nautical miles — nearly 70 percent of all U.S. coral reefs. Over millennia, invertebrate animals and algae have constructed massive structures in the shallow seas. Coral animals, bonded to basalt from ancient volcanoes, secreted skeletons of calcium carbonate that formed the substance of future reef growth. The NWHI coral reefs are the foundation of an ecosystem that hosts more than 7,000 marine species, including marine mammals, fishes, sea turtles, birds and invertebrates. Many are rare, threatened or endangered. Approximately one quarter are endemic, found nowhere else on Earth. Besides supporting these species, the coral reefs and bits of land of the NWHI provide an amazing geological record of the volcanic powers that created the area and the erosion and subsidence that sculpted it. Beyond biological
significance, the area boasts a rich cultural history. During their Trans-Pacific
voyages, ancient Polynesians sailed these waters and used these islands
for centuries as places of residence and worship. When Western explorers
found these islands they raced to claim them for their own nations after
original Polynesian settlement. Entrepreneurs tried to make a living from
natural resources found there, and the world's first global communications
network linked through these islands. In World War II, the U.S. military
fought a definitive battle near Midway and used the region for national
security. Most of the NWHI are less than a square mile in landmass. Northwest of Ni'ihau, (the westernmost of the main Hawaiian Islands) the rocky islands, atolls and reefs become progressively older and smaller. For at least 80 million years new islands have formed as the Pacific plate drifts over a stationary plume of magma rising from a hot spot within the Earth's mantle. Millions of years of eruptions have pushed the fluid rock up through the ocean floor creating high volcanic islands, The Pacific plate creeps northwestward at about 3.4 inches per year, slowly separating the volcanic islands from their source, as a new volcano builds over the hot spot. (Click NOAA image for larger view masked boobies in the NWHI. Click here for high resolution version, which is a large file. Please credit “NOAA.”) Gradually the islands subside and erode. In the NWHI, only basalt remnants from ancient volcanoes (Nihoa and Necker Islands, Gardner and La Perouse Pinnacles) remain above the ocean's surface. As Hawaiian islands sink, reef building corals ring them. A lagoon is formed between the sinking island and the ring of coral. When the island slips below the surface all that remains is a lagoon bordered by a coral ring. Over time, the reef erodes and coral rubble and sands form low islets near the reef edge that in turn are sculpted by the wind and waves. These coral rings and islets are known as atolls. At Kure Atoll,
the last emergent island in the archipelago, coral growth barely keeps
pace with the rate of subsidence and erosion. Scientists named this the
Darwin Point. In the cold waters north of Kure, where coral growth rates
are slower than the rate at which submerged lands sink, corals begin to
die. From here on are the seamounts, drowned remnants of the Hawaiian
chain which ultimately form the Emperor Seamounts, extending all the way
to Japan and Russia. Scientific research in the NWHI is finding that the coral reef ecosystem is predator dominated, with large carnivores such as sharks, jacks and groupers composing over half of the overall biomass of fishes. This is a very different view than what has been found in the main Hawaiian Islands and most other major coral reef ecosystems worldwide. These findings may provide insight into how humans have affected coral reef communities. The NWHI coral reefs are some of the northernmost reefs in the world. Surface water temperatures at some NWHI reef areas drop to 18°C in late winter. At 16-18°C reef building coral growth is inhibited, and sustained periods at these temperatures can cause mortality in reef building coral species.
Another effect of the isolation of NWHI coral reefs is the high rate of endemism. About one quarter of all marine species found in the Hawaiian Archipelago are found nowhere else on Earth. Few up-curent coral reef species were able to survive the long journey to the Hawaiian Islands and of those that did, only a few established themselves and reproduced. Because of the distance from the original population, interbreeding became rare, if not impossible and new species evolved over time, in response to the new environment, that were quite different from the original parent species. These new species exist only in the Hawaiian Archipelago and cannot be replaced from anywhere else if they become extinct. Along with coral reef areas there are many deep sea banks and seamounts in the NWHI that provide important habitat for bottomfish and other unique sea creatures, some new to science. A few of these deep sea areas also provide foraging grounds for the endangered Hawaiian monk seal.
Song and chant that have been passed down refer to islands beyond the main Hawaiian islands and recall the travels of seafaring ancestors on their way to and from the Hawaiian Archipelago. On genealogical, cultural, spiritual and geological levels, the Northwestern Hawaiian Islands are intimately connected to Native Hawaiians and the main populated islands. The natural elements (land, wind, rain) and creatures of the northwestern islands are considered primordial ancestors and therefore the older relatives of living Native Hawaiians. Both share an interdependent, family-based relationship which requires care for the older siblings who in turn provide for the well being of the younger. These traditions remind us of the time honored responsibility to care for this unique, fragile place and its many resources through strong conservation and protection principles. The need to care for the archipelago continues as NOAA look toward the future. For nearly
100 years, the islands and near shore waters of the NWHI have been protected
by various government agencies. New protections and long-term conservation
will help maintain the wild, natural character, and the splendor of irreplaceable
coral reefs and island ecosystems. Relevant
Web Sites NOAA National Marine Sanctuary Program 2005 State of the Sanctuaries Report THE NOAA NATIONAL MARINE SANCTUARY PROGRAM (NOAA Magazine article) WHAT IS THE STATE OF THE NATION’S MARINE SANCTUARIES? Media
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