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Tubbataha Reef National Marine Park

In the heart of Sulu Sea lies the Tubbataha Reef National Marine Park— 33,200 hectares of underwater paradise teeming with diverse marine life. It is the Philippines’ first and only national marine park and its only coral reef atoll.

Despite its isolation, or perhaps because of it, Tubbataha is a dream destination for diving enthusiasts all over the world. Live-aboard dive boats offer visitors the necessary amenities to enjoy their stay in Tubbataha. Divers should spare at least five days to explore the expanse of the Park’s famous dive sites like the Delsan and Malayan Wrecks and Black Rock. Visitors are required to secure an entry permit from the Tubbataha Management Office before entry into the Park

Tubbataha was inscribed by UNESCO in the prestigious World Heritage List because of its significance to regional and global biodiversity and its outstanding universal value. It is one of only nine purely marine World Heritage Sites in the world and the only one in South East Asia.

Tubbataha is home to at least 441 species of fish, 396 species of corals, 71 species of algae, 44 species of birds, 6 species of marine mammals, two species of nesting marine turtles and still more unaccounted wonders.

Believed to be the spawning ground of various marine species dispersed in Palawan and other neighboring islands, Tubbataha yields the highest fish biomass in the country at 120 metric tons per square kilometer (2003).

How to get there. More info about Palavan Island.

Dive Site in Tubbataha Reefs

TUBBTAHA REEFS (North & South)
The best amongst the reefs in Sulu Sea are those in the eastern part. In the very heart of it lies the TUBBATAHA REEF. These reefs are declared as one of the Philippines National Marine Park and many have considered it as the best that we have in the country. It was also named by UNESCO as one of the World Heritage sites in 1993. In order to protect the reefs the Tubbataha Marine Park Foundation was established in the mid 1980’s. The Department of Environment deputized it and Natural resources by patrolling the marine reserve and undertaking preliminary measures such setting up of permanent buoys and moorings. The foundation has been very successful because it prevented the increase of commercial fishing from the illegal fishermen.

Tubbataha Reef is about 182 km (98 nautical miles) south of Puerto Princesa. Puerto Princesa, the capital province of Palawan is the main gateway to Sulu Sea. It is a two-small tropical extensive atoll-like reefs (with inner lagoons) separated by a channel. Topography includes crevices, overhangs, cavelets, gradual slopes and stony corals. In the 1982 countdown they have discovered that Tubbataha has 300 species of corals and 379 species of fish.

On the northeast end of the North Reef is "Bird Islet", a rookery by sea bird, Brown Boobies and nestling grounds for sea turtles. The north face of the reef has sandy slope with coral heads to 15 meters (50 feet) while the east face is between 14 meters (45 feet) to 20 meters (65 feet), then drops as a wall with caves and crevices to deeper than sports diver can dive. The coral cover is good with lots of stony, leathery and whip corals. Guitar sharks, leopard sharks, whitetip sharks, blacktip sharks, gray reef sharks, nurse sharks, manta rays, blue-spotted lagoon rays, eagle rays, flounders and turtles are just some of the marine life forms you can find. The walls abound with cleaning stations, some of which have magnificent gorgonians. Large fish are plentiful that patrol the walls; dog tooth tuna, jacks, surgeons, unicorns, and snappers still prowl the area. Just about every Pacific reef fish are present like: trumpetfish, corentfish, anthias, damsels, anemones with clownfish, angelfish, scorpionfish, boxfish, peacock groupers, titan, clown, orange-striped triggerfish, redtooth triggerfish, Moorish idols, Star pufferfish, sleeping parrotfish, hawkfish, big wrasse and female Napoleon wrasse.

Night dives are quite interesting because it is when the fish are feeding though current can be a problem to photographers. There is also quite a number of pleurobranchs, crustaceans, morays, garden eels, Feather Duster worms, segmented worms, nudibranchs, crinoids, sea stars, Bohadschia sea cucumbers, basket stars and flashlight fish. Water is generally calm with some swell. Currents can become strong and might change without warning. Visibility can reach to 40 meters (130 feet).

The South Islet, called "Lighthouse", is a solar-powered lighthouse where gulls and terns rest. On the east side of the lighthouse, is a wreck of the Delsan, an old log-carrier.

The north/northeast of the islet is a rich slope between 10 meters (33 feet) and 20 meters (66 feet) ends in an equally rich wall going deeper. There is some evidence of blast fishing on the reef-top but no signs of damage on the walls, which contains gorgonian sea fans, barrel sponges and soft corals. Pelagic species varies more in this area than the North islet of Tubbataha reef, including mackerel, barracudas and rainbow runners. The caves and crevices contain Spiny Lobsters, squirrelfish, soldierfish, whitetip sharks, nurse sharks, jacks, Emperor and Six-banded angelfish, barracudas, groupers, sweetlips, goatfish, butterflyfish, triggerfish, Green and Hawksbill Turtles, eagle rays and mantas. One portion of the wall is in fact covered with white hyroids. Site is ideal for night dives.

The south/southeast/southwest end almost the same as north/northwest end but with far larger area of shallow reef-top, which have been more, affected by dynamite fishing. But despite of this, the area is still rich with smaller fish, leathery corals, whip corals, sponges, anemones with clownfish, damsel, chromis and anthias. Blue-spotted lagoon rays, sea cucumbers and sea stars are predominant in the sandy patches. The shallow part of the lighthouse has sea grass that attracts turtles. Recently, the area has shown improvement and is now displaying a spectacular growth of corals.

JESSIE BEAZLEY
This reef is 23km (12 nautical miles) northwest of North Islet of Tubbataha. It is a mound of broken coral surrounded by white sand and reef. This tiny islet is almost invisible during high tides. A rich coral slope at 5 meters (16 feet) to 10 meters (33 feet) is a wall often undercut to 40 meters (130 feet) sloping out into infinity. It is known for an amazing overhang that has Tubastrea corals and Blue sponges, crevices, large fans corals, huge grogonian sea fans, black corals and giant barrel sponges. In fact, the reef-top is covered with lettuce and leathery corals teeming with different variety of reef fish.

Schools of snappers, jacks, surgeonfish, groupers, Sabre squirrelfish and bigeyes, Midnight snappers, black and white snappers, jacks, Vlaming’s Unicornfish, rainbow runners, emperors, pennantfish, batfish, spotted sweetlips and lined sweetlips, hawkfish, gobies, blennies, morays, lobsters are always present. Pelagics in the form of whitetip sharks, grey reef sharks, large groupers, Napoleon wrasse, tuna, trevallies, barracudas and mackerels are present. Spiny lobsters can be found in many small holes. Large shoals of fish roam around the area or at times follow scuba divers.

More about Tubbataha

Tubbataha Reef lies in the middle of the Sulu Sea and is one of the last marine frontiers of the region. Because of its globally significant biodiversity, UNESCO declared it a natural World Heritage Site in December 11, 1993. The total area of the Park covers 33,200 hectares including surrounding waters. Tubbataha Reef consists of two coral atolls, separated by an eight-kilometer channel.

The coral reefs of Tubbataha Reef National Marine Park have been surveyed since 1982 (White and Arquiza, 1999). Many different organizations and academic agencies have visited and collected data in these two remote atolls in the Sulu Sea. Hypothesized to populate neighboring reefs with fish and coral larvae due to the prevailing currents in the Sulu Sea (Alcala, 1993), Tubbataha Reef is a valuable resource to the country. Tubbataha is one of the last few reefs in the Philippines that is relatively intact and harbors an abundant and diverse association of organisms. In one survey alone, more than 300 coral species and at least 379 species of fish were recorded ( White and Arquiza, 1999).

The Park, despite its remoteness, was still affected by illegal fishing practices commonly found all over Southeast Asia. Tubbataha experienced the highest levels of destruction in the 1980’s and by 1989 the reefs were no longer in pristine condition (White and Arquiza, 1999). The stresses on the reef eased when it was designated as National Marine Park in 1988 and was closed off to fishing. However, due to lack of surveillance equipment, illegal fishers still continued to exploit the Park.

A Tubbataha Protected Area Management Board (TPAMB) was established in July 1999 and as a result, the rules of the Park are now fully and strongly enforced by a composite team of Park rangers, using a new radar system and more chase boats. This had led to many improvements in the Park and has kept illegal fishers out.

Given the critical levels of over-exploitation of many coral reefs, marine reserves may be the only viable option available to maintain levels of spawning stock biomass necessary to sustain reef fisheries (Russ et al, 1992). Hence, the goals of our monitoring efforts are to expand knowledge of the unique ecosystem of Tubbataha and to provide technical information that will improve and facilitate the management of this Marine Park.

Methods

Survey of Bethnic Communities

In 1997, seven (100-meter) permanent transects were set parallel to the reef crest at an average depth of 10 meters around the two atolls of Tubbataha. These sites were to be monitored annualy from 1997 to 2000. However, due to technical difficulties that prevented the collection of data in some sites, only three of the sites were considered in the change through time analysis. Change in percentage cover of benthic communities through time was recorded using the video technique, modified from English et al (1997) except for 1999 when the benthos point-intercept transect method was used. A separate benthos point-intercept transect survey was done in year 2000 to compare the results obtained by the two methods. A paired T-test showed that there was no significant difference between the two methods (T = 0.012, P = 0.990), therefore data obtained from 1999 was included in the change through time analysis. Coral mortality indices were calculated based on Gomez et al (1994). A one-way ANOVA was used to test for changes through time. Data sampling for benthic cover was conducted within the summer months of March to May.

Fish Visual Census

Fish populations were surveyed from 1998 to 2000 using the visual fish census modified from English et al (1997) in all seven (100-m) permanent transect sites. For each variety of fish encountered, the numbers and sizes were estimated. Biomass of fish assemblages were calculated based on Kulbicki et al (1993) and ICLARM Fishbase and was standardized to metric tons per square kilometer. Data on fish density were standardized to density per square meter. A one-way ANOVA was used to test for changes between years. Biomass data was log transformed prior to analysis to ensure normality. Data sampling for the fish census was conducted also within the summer months of March to May.

Results

Mean live coral cover in the tree sites (sites N1, N3 & S5) decreased by 24.9% from 1997 to 1999. However, there was a recorded 3.3% increase in live coral cover from 1999 to 2000. Results from the one-way ANOVA, however, show that both hard coral and soft coral did not differ significantly over time. There were no significant differences in the abiotic component and other live benthic components (OT). Algal cover, however, significantly increased (F = 15.585, P = 0.001) between 1998 and 1999, and dead coral with algae (DCA) (F = 23.010, P = 0.0001) between 1999 and 2000, thus showing an increase in coral mortality from 1998 – 2000. There was a significant increase (F = 4.307, P = 0.030) in the mean total fish biomass in all seven sites over the latter three years. Estimated mean total fish biomass was 63.73, 446.92 and 647.33 metric tons per square kilometer (MT/sq km) for 1998, 1999 and 2000 (Figure 3), respectively. This dramatic increase in fish stocks represents more than 900% rise since 1998. It was the presence of large schools of pelagic fish species that accounted significant increase (F = 4.246, P = 0.031) while demersal fish species showed no significant changes over time (Figure 3). Although mean density of total fish species decreased by 10% from 1999 to 2000, the value for year 2000 was 36% higher than that recorded for 1998. Pelagic species, Caesonids, significantly increased in mean density from 1998 to 2000 (F = 5.091, P = 0.018) while Carangids displayed increasing trends. Some commercially important demersal fish families such as Lethrinids and Serranids showed an increase in both mean density and biomass over the study period, however, these were not statistically significant.

For the purpose of comparing the relationship of benthic cover and fish biomass, the mean total fish biomass for three transect sites used in the survey of benthic communities were calculated. The estimated mean total fish biomass was 56.98, 128.92 and 302.09 MT/sq km for 1998, 1999 and 2000, respectively. This increase was not statistically significant (F = 4.470, P = 0.065), nevertheless, this still represented a 530% increase in total fish biomass.

Discussion

Coral Reef Benthic Communities

The decline in coral reef cover was attributed to the bleaching event caused by the El Niño phenomenon in 1998. Compared to other countries, the bleaching in the Philippines was relatively fair. The bleaching in the country was described by Wilkinson et al (1998) as moderate and patchy on some reefs in large areas, with a mix of coral recovery and approximately 20-50% mortality. Other countries recorded as high as a 95% mortality rate (Wilkinson et al, 1998). The bleaching all over the world was most pronounced in shallow water (less than 15 meters deep) and particularly affected staghorn and plate Acropora and other fast growing species (Wilkinson et al, 1998). Dead but intact Acropora forests were observed in Site 1 and 5. This observation could be the after effect of the bleaching event when algae colonizes over corals unable to recover after being bleached and an explanation for the significant increase in algal assemblage (AA) between 1998 and 1999. There was no significant change in live coral cover from year to year, nevertheless, there was a recorded 24.9% decline from 1997 to 1999. The recorded 3.3% increase in live coral cover from 1999 to 2000 could indicate the absence of both natural and anthropogenic stresses within the year and could indicate signs of recovery.

The coral mortality index was highest in year 2000. However, the low coral mortality index in 1999 could be an underestimated value; the significant increase in algae in 1999 could have covered areas of dead coral which the observer was unable to distinguish , thus some accounted for algae and not dead coral with algae (DCA).

Fish Visual Census

Fish Density and Biomass

The mean total density of fish in the seven sites decreased from 1999 to 2000, mainly due to the decrease in damselfish density. In 1999, 58% of the average fish density was made up of damselfishes, this lessened to 49% in year 2000. It was noted in year 2000 that fish density was not comprised mainly of the smaller reef fishes such as anthiases and damselfishes compared to the past years. It was observed that there were greater aggregations of larger fish species, such as more encounters with pelagic species. Total fish density in 2000 was still higher than in 1998. In support of this data, according to the Tubbataha report of Sulu Fund and the Coastal Resource Management Program (CRMP), average fish density has increased by 26% since 1996 (White et al, 2000).

Compared to the past years, there were larger commercially valuable fishes in 2000. This explains the large increase in fish biomass. Important food fish and pelagic species which accounted for the significant increase were present in greater numbers in the recent year compared to 1999. In year 2000, pelagic species made up 77% of the total biomass (501.57 MT/sq km). In 1998 and 1999, pelagic species made 16% (12.55 MT/sq km) and 58% (275.01 MT/sq km) of the total biomass, respectively. Unlike demersal species, pelagics are not permanent residents of a reef. Instead, they only visit seaward reef dropoffs or enter deep lagoons and are adapted to life in the open ocean (Lieske and Myers, 1996).

However, the presence of pelagics in great numbers, being carnivorous, could indicate the abundance of food resources in the area. Demersal fishes (biomass) on the other hand, decreased by only 5% from 1999 to 2000, but recorded an increase of 45% from 1998 to 1999. This could be explained by the 123% increase in Acanthurid density, which are herbivores. Although not statistically significant, this increase could be explained by the significant increase in algae between 1998 to 1999. Despite of the increase in total live coral cover from 1997 to 1999, the mean total fish biomass in the three permanent transect sites (N1, N3, and S5) from 1998 to 2000 was also increasing although not statistically significant.

The significant increase in total fish biomass and increasing trends in density of some commercially important fishes in the seven sites are promising in terms of Tubbataha’s recovery. These increases could suggest the decline in fishing pressure due to the increased enforcement in the protection of the Park. It is believed that the increased patrols in Tubbataha have curtailed fishing inside the Park. According to Salm et al (2000), predatory fishes such as groupers, emperors, jacks, and snappers are the first fishes to disappear from heavily fished areas. Conversely, their presence in increasing numbers supports the grounds that the decrease in fishing pressure could be one of the main reasons why fish biomass has increased substantially.

The resulting increase in biomass that could indicate the decrease in fishing pressure over the years is starting to pay conservation dividends. Anecdotal evidence from Cagayancillo (nearest municipality to Tubbataha), fishermen seem to bear out that there has been some kind of spillover effect. The spillover effect is the adult (post-settlement) movements from reserve to fished areas (Russ and Alcala, 1996). The fishermen have observed large fish species coming back into their fishing grounds and a number of them attributed this to the protection of Tubbataha.

Due to the prevailing currents in the Sulu Sea, fish larvae may not be retained in Tubbataha reefs until recruitment size, but may be carried by water currents to other reefs (Dolar and Alcala, 1993). Therefore, Tubbataha could also serve as a source of fish larvae and other larval recruits (Alcala, 1993).

Recommendations

The surveys were conducted on the reef crest and some on the upper reef wall, which only gives a fraction overview of the reef. To serve as baseline data to monitor change over time, the comprehensiveness of the data collected is essential for understanding the reef ecosystem. The data collected so far do not give the full view of Tubbataha Reef. The reef crest of an atoll is strongly influenced by wind and waves (Castro and Huber, 1997), therefore, more exposed to stresses compared to the reef slopes and walls. Bleaching and mortality were also more pronounced in water with less than 15 meters depth (Wilkinson et al, 1998). Tubbataha is known for its steep slopes and walls and these were not surveyed due to time constraints. Therefore, more transect surveys at different depths to show different habitats should be done to give a fuller view of the status of the Tubbataha Reef. The outer reef slope and reef walls could display more resiliency being relatively free from environmental stresses and minimally affected by bleaching, thus displaying a different status than that of the reef crest.

Conclusion

The monitoring of Tubbataha’s complex marine ecosystem found increases in fish populations and decrease in live coral cover due to bleaching. This outcome is promising for the ecosystem’s conservation and is rewarding for conservation organizations working to save this natural World Heritage Site. Tubbataha’s remoteness and relative resiliency to stresses compared to other reefs in the country sets its reputation for being the last marine frontier of the Philippines. Other studies that explore this reef’s importance and connectivity to other reefs should be done to further expand knowledge to implement the appropriate management of the Park.


 


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