Threats to Guam's Coral Reefs

A bleached coral reef
A stressed coral mound in Guam's Tumon Bay Marine Preserve.

Curt Storlazzi, USGS

Climate change, sedimentation, and overfishing impact corals in War in the Pacific National Historical Park.

 
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As we enjoy the beautiful biodiversity of the coral reefs in the War in the Pacific National Historical Park, we need to understand that natural and human processes are threatening their health.

For example, using fossil fuels releases greenhouse gases into the atmosphere, which contributes to global warming. Clearing and burning vegetation allows more sediment to wash into the ocean and onto coral reefs. Taking fish from the reef faster than the population can reproduce reduces the number of fish on the reef and alters the balance of the food web.

Coral reefs at the park may be less resistant to ocean acidification and bleaching.

Current threats to the coral reefs at War in the Pacific National Historical Park will only be increased by climate change. For example, low numbers of herbivores (a result of overfishing) and poor water quality (caused by sedimentation from run-off on the land) put stress on corals. If corals are already living under stressful conditions, they become less resilient or less able to adapt to changes in the environment (Burdick et al. 2009).

 
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Sedimentation along the coral reef.

In the face of climate change, corals must contend with changing conditions such as rising water temperatures and ocean acidification. Those corals already under stress will become less healthy as the alterations brought on by climate change become even more pronounced.

Ocean acidification also affects coral populations. Already, reef monitoring has recorded low coral recruitment (the number of juvenile corals that settle on a reef) in the park (NPS 2009. Warmer water temperatures and the ocean acidification associated with a change in water chemistry (lower pH) are reducing or preventing coral growth (Kleypas et al. 2006). With low coral recruitment and slowed coral growth, coral reefs are less able to maintain their structure and are more easily damaged by waves and storms.

Although severe bleaching events have not been observed in the park, increased water temperatures make strong, regularly-occurring bleaching events more likely in the future (Burdick et al. 2009).

 
View of a ocean from the top of a hill
When there is more bare land, more sediments flow into the ocean via rain and runoff.

Land clearing causes sediment runoff on coral reefs

Every time it rains, soil on bare land washes into streams and the ocean. Lands become bare when wildfires are set for ease of hunters or when bulldozers remove plants and trees to make room for development or agriculture. Without plants and trees to soak up the rainwater and trap sediments, loose soil erodes from the land as runoff and clouds waterways. When this soil is carried to coral reefs, it reduces water clarity and smothers corals by settling on the reef. As more and more land is cleared of plants and trees, larger and larger amounts of soil make their way to coral reefs, sediment runoff increases, and the threat to coral reefs grows. As a result of a lack of vegetation, park lands are more susceptible to erosion and sediment runoff on park coral reefs increases.

Scientists at War in the Pacific National Historical Park have observed low coral recruitment on the reef and believe that sediment runoff may be the cause (PACN 2006). With low numbers of coral recruiting to the reef, coral reefs are less able to grow or maintain their structure. In order to reduce soil delivery to coral reefs, park staff will continue to work with communities to support replanting programs, to discourage fires, and continue to monitor sediment on the reefs (NPS 2009).

 
Underwater photograph of Tumon Bay Marine Reserve, Guam, showing some of the amazing biologic diversity of coral reefs.
A'aga (Barred thicklip) at the Tumon Bay Marine Reserve in Guam.

Curt Storlazzi, PhD / USGS

Overfishing and modern fishing methods are reducing the number of large reef fish

In recent years, people have seen fewer and fewer large fish on the coral reefs of Guam, even on reefs with healthy coral communities (Burdick et al. 2009). One reason for this decline is modern fishing practices that allow people to take large numbers of reef organisms such as parrortfish, surgeonfish, octopus, and other commercially important species (Porter et al. 2005). Of particular concern are the non-traditional fishing methods of scuba spear fishing and monofilament gillnet fishing (Burdick et al. 2009). In fact, scuba spear fishing has probably contributed to the dramatic decline of humphead wrasse and bumphead parrotfish on local coral reefs (Burdick et al. 2009).

Low numbers of algae-controlling herbivores (caused by overfishing), upsets the balance of the coral reef food web. Without herbivores to control the amount of algae growing on a reef, algae can grow rapidly and smother corals. Overfishing also impacts our diet. If the fish caught for food become more and more scarce, it will be harder to prepare daily meals and traditional dishes.

 
Learn more about the park's reefs at Teach Ocean Science, a collaborative effort between the National Park Service and other partners.

Last updated: December 4, 2024

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