Marine Resources Assessment for the Marianas Operating ... - SPREP
Marine Resources Assessment for the Marianas Operating ... - SPREP
Marine Resources Assessment for the Marianas Operating ... - SPREP
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AUGUST 2005 FINAL REPORT<br />
A fringing reef borders <strong>the</strong> Unai Dangkolo white carbonate beach (NCCOS/NOAA 2005). Macroalgae (10<br />
to 50% cover) populate <strong>the</strong> reef flat while <strong>the</strong> fringing reef is composed of coralline algae. Corals (10 to<br />
50% cover) are a main constituent of <strong>the</strong> <strong>for</strong>e reef and insular shelf (NCCOS/NOAA 2005). Surveys<br />
conducted in 1994, however, report that <strong>the</strong> inner reef flat supports an extensive (50 to 70% coral cover)<br />
and diverse reef community (25 coral species) (<strong>Marine</strong> Research Consultants 1999). On <strong>the</strong> reef front,<br />
<strong>the</strong>re is a spur-and-groove system down to a depth of 10 m, seaward of which <strong>the</strong> benthos is comprised<br />
of carbonate pavement. Both <strong>the</strong> spur-and-groove system and <strong>the</strong> <strong>for</strong>e reef pavement are densely<br />
populated by corals (36 species of corals). The passage of a typhoon in December 1997 severely altered<br />
<strong>the</strong> reef flat coral community diversity and cover. Coral cover on <strong>the</strong> reef flat was reduced from an original<br />
50 to 70% cover to 2% cover. No branching corals remained on <strong>the</strong> reef flat following <strong>the</strong> typhoon (<strong>Marine</strong><br />
Research Consultants 1999). The recent benthic habitat mapping of <strong>the</strong> CNMI by NCCOS/NOAA (2005)<br />
reflects <strong>the</strong> change in reef flat composition. Since NCCOS/NOAA (2005) show relatively abundant coral<br />
cover on <strong>the</strong> reef front, <strong>the</strong> <strong>for</strong>e reef has possibly retained some of its pre-December 1997 characteristics.<br />
The impacts of corallivorous predators on corals have most likely altered <strong>the</strong> coral composition and cover<br />
on <strong>the</strong> <strong>for</strong>e reef (Quinn and Kojis 2003).<br />
2.7.2.4 Coral Communities and Reefs of Farallon de Medinilla<br />
In contrast with <strong>the</strong> o<strong>the</strong>r sou<strong>the</strong>rn Mariana Islands, <strong>the</strong> study area at FDM does not include fringing or<br />
<strong>for</strong>e reefs (Figures 2-9a, 2-9b, and 2-9c). Ra<strong>the</strong>r, it has a relatively wide insular shelf (400 to 1,800 m<br />
wide) that supports limited coral cover along all sides except <strong>the</strong> western side of <strong>the</strong> island<br />
(NCCOS/NOAA 2005; Smith personal communication). In 2004, 81 species of corals were observed on<br />
reefs at FDM (DoN 2005). Overall, <strong>the</strong> northwestern nearshore area (eroded submerged cliff face and<br />
reef terrace) of <strong>the</strong> island supports <strong>the</strong> highest diversity of marine invertebrates and fishes on FDM (DoN<br />
2005). Most of <strong>the</strong> coastline of FDM is bordered by steep karstic cliffs which <strong>for</strong> <strong>the</strong> most part extend 6 to<br />
9 m below <strong>the</strong> waterline (DoN 2005). Cliffs on <strong>the</strong> western shoreline extend more than 20 m below <strong>the</strong><br />
waterline. There are numerous underwater caves along <strong>the</strong> FDM shoreline. Boulders dislodged from <strong>the</strong><br />
cliffs border <strong>the</strong> base of <strong>the</strong> cliffs. Seaward of <strong>the</strong> cliff face is a reef terrace that is 30 to 50 m wide and 10<br />
to 25 m deep beyond which is a sandy slope zone. On parts of <strong>the</strong> western side of <strong>the</strong> island, a vertical<br />
wall undercut by caves and ledges delimits <strong>the</strong> seaward edge of <strong>the</strong> reef terrace and intersects with <strong>the</strong><br />
sandy slope habitat. At <strong>the</strong> sou<strong>the</strong>rn end of <strong>the</strong> island, a 2 m deep “finger reef” extends 200 m southward.<br />
The edges of <strong>the</strong> finger reef are vertical walls that drop down to a 30 m depth. The reef terrace consists of<br />
a spur-and-groove system on <strong>the</strong> eastern (windward) side of <strong>the</strong> island where <strong>the</strong> island <strong>for</strong>ms an isthmus<br />
separating <strong>the</strong> lower narrow third of <strong>the</strong> island from <strong>the</strong> wider upper two-thirds of <strong>the</strong> island (DoN 2005).<br />
Near <strong>the</strong> cliff edge on <strong>the</strong> reef terrace of <strong>the</strong> eastern side of FDM, <strong>the</strong>re is less than 5% coral cover (DoN<br />
2005). Fur<strong>the</strong>r offshore, <strong>the</strong>re is 10 to 20% coral cover composed of encrusting Porites and head coral<br />
<strong>for</strong>ming Pocillopora. Coral cover on <strong>the</strong> boulders is 25 to 30% and comprised of Pocillopora, Porites,<br />
Montipora, and Millepora. Coral cover on <strong>the</strong> ridges of <strong>the</strong> spur-and-groove system off <strong>the</strong> island isthmus<br />
on <strong>the</strong> windward side ranges from 15 to 25% and is composed of Porites and Pocillopora. There are large<br />
aggregations of <strong>the</strong> long-spined urchin Echinotrix diadema (hundreds to thousands of individuals) seen<br />
both on <strong>the</strong> eastern and western sides of <strong>the</strong> island, and high coral cover is found on boulders along <strong>the</strong><br />
reef terrace on <strong>the</strong> leeward side of <strong>the</strong> island (50 to 70%, mostly Pocillopora coral heads). Most of <strong>the</strong><br />
branching colonies of Pocillopora sp. on <strong>the</strong> leeward side have broken branches (DoN 2005).<br />
Since 1971, FDM has been a target site <strong>for</strong> live-fire military exercises (ship-to-shore gunfire, aerial<br />
gunnery and bombing) (DoN 2005). The majority of <strong>the</strong> ordnance found underwater at FDM during reef<br />
assessments conducted since 1999 occur at <strong>the</strong> northwestern end of <strong>the</strong> island (DoN 2005).<br />
2.7.3 Softbottom Habitats<br />
Softbottom habitats are those habitats in which <strong>the</strong> benthos is covered with a layer of fine sediment<br />
(Nybakken 1997). Commonly identified habitats are beaches, sand flats, and mudflats (Figures 2-7<br />
through 2-9). Sand flats differ from sand beaches in that beaches are intertidal pile-ups along coasts,<br />
while sandflats can be found anywhere away from <strong>the</strong> coasts. Softbottom habitats can occur on a sloped<br />
seafloor and not only on a flat, horizontal surface (Paulay personal communication).<br />
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