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A T O L L R E S E A R C H B U L L E T I N N O * 2 8 1

CORAL A S S E M B L A G E S OF R E E F F L A T S AROUND P U L A U P A R I , THOUSAND I S L A N D S , I N D O N E S I A

BY

B . E - BROWN, M - C . HOLLEY, L o SYA'RANI

AND

M - LE TISSIER

ISSUED

BY

T H E S M I T H S O N I A N I N S T I T U T I O N WASHINGTON, D o C., U . S . A .

DECEMBER 1983

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CORAL ASSEMBLAGES OF R E E F F L A T S AROUND P U L A U P A R I , THOUSAND I S L A N D S , I N D O N E S I A

BY

Abstract

A spectrum of physical influences, resulting from the reversing monsoons, governs the distribution of corals on reef flats around the Pulau Pari complex of islands in the Java Sea, Indonesia, with greater diversity in the

relatively sheltered southern reefs and reduced diversity on the more physically exposed northern reefs. A total of 74 species were recorded on southern reefs as compared with 43 species on the exposed northern reef flats.

The outer reef flats at all sites were dominated by Acropora species which showed

a

distinct zonation pattern.

Acropora pulchralaspera species dominated the unconsolidated landward section of the outer reef flat, Acropora digitifera occupied the mid-seaward section, while Acropora hyacinthus colonised the seaward edge.

lDept. of Zoology 'Dept. of Zoology University of Newcastle upon Tyne University of Oxford Newcastle upon Tyne NE1 7 R U South Parks Road

England Oxf ord, England

3 ~ a c u l t y of Fisheries

&

Animal

~ u s b a n d r ~

University of Diponegoro Semarang, Indonesia

current address: Dept. of Zoology

University of Newcastle upon Tyne

Newcastle upon Tyne NEI 7RU, England

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INTRODUCTION

Umbgrove (1929) was the first scientist to study the reefs of the Java Sea tn detail. In these early studies Umbgrove recognised the important role of physical factors both in governing the morphology of the islands and the structure of benthic communities or "facies" comprising the reef flats. In 1975 Rosen proposed a similar scheme for reefs in the Indian Ocean, with different coral assemblages reflecting exposure to varying levels of wave energy and light. Other workers have recently shown the importance of exposure to wave energy in controlling reef development

(Bradbury

&

Young 1981, Brown and Dunne 1980, Chappel 1980) and reef diversity (Grigg and Maragos 1974, Dollar, 1982).

Clearly then wave energy may te paramount in

determining both reef type and resulting community structure in shallow waters. The present study presents data on the influence of reversing monsoons on the composition and zonation of reef flats in the Java Sea, an area little studied since the extensive work of Umbgrove i n the early part of the century.

MATERIAL AND METHODS

a) Study site

The Pulau Part complex of islands 1s situated at the southerly end of a chain of more than a hugdred islands, commonly known as the Thousand Islands, which extends NNW -

SSE across the Java Sea towards the Sunda Straits, Indonesia (Fig. 1).

The island complex is composed of Pulau Burung, Pulau Tikus, Pulau Kongsi and Pulau Tengah, the islands being separated from each other by a system of lagoons (Fig. 1).

The islands are surrounded by well developed fringing reefs with prominent shingle banks o n the north east and east rim.

The dominant physical influence in the area is the reversing monsoon wind. Umbgrove (1929, 1930) related the monsoons to be geomorphology of coral islands in the

Thousand Islands and concluded that the more southerly islands of the group were subject to a strong wind effect from the north west quarter (the westerly monsoon which

prevails from December-April) and an even stronger wind from

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the east (the easterly monsoon which prevails from May-November) .

The Thousand Islands are also strongly influenced by the effects of reversing currents - Umbgrove noted that the reefs and islands of the group were aligned in the direction of their long axes and attributed this to the erosive

effects of a current which runs along the north coast of Java, eight months westward and four monts eastward. The latter current is described as twice as fast as the wes ward current and Umbgrove quotes figures of 28 and 17 cm sec f

for currents in the open sea of the region during the west and east monsoons respectively.

The tidal cycle for Jakarta shows a range of

approximately one metre between high and low tide levels throughout the year. Salinities in the area vary between 31

- 33%.

b) Reef surveillance

Five areas were chosen for study (Fig. 1) using methods adopted by Loya (1978). After plotting a specieslarea

curve, 10 m long measuring tapes were place at 5 or 10 m intervals across the inner reef flat and the percentage coral cover of individual colonies noted. Measuring tapes were placed at 2 m intervals across the outer reef flat areas. All observations were made by snorkelling.

RESULTS

The reef flats around the islands of Pulau Part are characterised by an extensive sand flat (up to 500 m in extent), an inner reef flat, a shallow moat, an outer reef flat (varying from 10 - 20 m in width) and on the north east and east rim of Part Island prominent shingle ramparts.

a) Species composition

A total of 88 coral species from 28 genera were

recorded (Table 1) on transects across reef flats at all

sites, with southern reef flats showing greater diversity in

terms of number of species than northern reefs. A total of

74 species was recorded on southern reef flats, while only

4 5 species were noted on northern reef flats.

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b) Species distribution

Figure 2 illustrates the percentage living and dead cover of all corals and also the distribution of the dominant genera with respect to distance across the reef flat at all sites.

In almost all cases coral cover generally increased across the inner reef flat to reach

a

maximum in the moat area with dead coral cover reaching a maximum on t h e

landward edge of the outer reef flat. After this point living coral cover rapidly increased up to and beyond the reef front.

Montipora ramosa occupied the inner reef flat at all sites, being particularly conspicuous at site 1 , where it accounted for about

80%

of the total coral cover. I n

addition it was abundant in the moat areas of sites 2 , 3 and

5.

Micro atolls of Heliopora coerulea were also conspicuous in the moat at site 3.

Stands of Porites species (Porites lutea, Porites

attenuata, Porites nigrescens, Porites andrewsi and Porites (Synaraea) iwayamaensis) were obvious only on the southern reefs, particularly at site

5

where they accounted for more than

5 0 %

of the total cover.

All the outer reef areas were dominated bv A C ~ O D O ~ ~ species and only at site 1 was Montipora foliosa abundant.

At site 2 encrusting and branching Montipora species

(Montipora informis, Montipora composita, Montipora levis and Montipora tortuosa) accounted for

3 5 %

total midway across the outer reef flat.

Figure 3 illustrates a distinct zonation pattern for Acropora species on the outer reef flat which was

particularly marked at sites 1 , 2, 3 and 4. At these sites the number of Acropora species recorded varied between 3 -

6 , the common dominant species being Acropora aspera/pulchra (these species being included together because of the

difficulty in separate identification on the reef flat (Wallace 1978)). Acropora digitifera and Acropora

hyacinthus with Acropora formosa occurring abundantly at

site 2. The relatively limited number of Acropora species

recorded at these sites contrasted markedly with the more

diverse outer reef flat at site

5

where 1 4 Acropora species

were identified.

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Generally Acropora asperalpulchra species favoured the unconsolidated landward edge of the outer reef flat where broken coral fragments survived the breaking waves to the exclusion of other species. Acropora digitifera

successfully colonised the mid-seaward edge of the outer reef flat while plates of Acropora hyacinthus dominated the reef edge. At site

5

this zonation pattern was not as clear as that described at other sites. The cover of each

individual species was low being less than 12% of the total transect, compared with individual covers of between 30-60%

for Acropora asperalpulchra at site 2 and 3 5 % for

--

Acropora

hvacinthus at site 1.

DISCUSSION

There is a very clear resemblance between the reefs described in this paper and those described to the south in the Bay of Batavia by Umbgrove (1939). The wind rose

described for reefs i n the Bay of Batavia, with the greatest

"wind effect" on the northern reefs and the least influence o n the south western reefs appears to hold in the Pari

Island complex. The wind rose actually proposed (Umbgrove 1929) for islands i n the southern sectcr of the Thousand Island group w i t h the greatest "wind effect" on north west and south east reefs and relatively little influence o n the north east sector certainly does not fit observations made in the present study. Features noted at Pari Island such a s the ~ o n ; i ~ o r a ramosa dominated moat, the northerly located shingle ramparts anii the abundance of Montipora foliosa o n the north west side of the island complex are all

characteristics of reefs described by Umbgrove in the Bay of Batavia.

There are however important differences to be noted between the reefs of the Bay of Batavia and the Pari Island complex in the southerly Thousand Islands. Firstly the shingle ramparts of Pari Island are restricted to the north east and eastern sectors of the complex and do not extend along the entire northern border a s described for reefs in the Eay of Batavia. Secondly U ~ b g r o v e describes the reefs of the south west sector of the islands of the Bay of

Ratavia as showning a n impoverished reef facies because of the strong sedimentation effect i n this area. Within the Pulau Pari complex the reefs of the south west sector constitute a much more diverse coral assemblage than any other encountered i n the present study. Table 1 and Figure 3 reflect the diversity of corals at site 5 with 57 species recorded here compared with between 20-27 noted for the

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n o r t h e r n r e e f s ; t h e o u t e r r e e f f l a t a t s i t e 5 e x h i b i t i n g a p a r t i c u l a r l y h i g h d i v e r s i t y o f A c r o p o r a s p e c i e s .

T h e r e l a t i v e l y h i g h d i v e r s i t y o b s e r v e d a t s i t e 5 may b e e x p l a i n e d b y t w o f a c t o r s

-

p r o t e c t i o n f r o m s e v e r e w a v e

a c t i o n a n d t h e g r e a t e r d e p t h o f w a t e r ( 4 0 cm) c o v e r i n g t h e r e e f f l a t a t l o w w a t e r w h e n c o m p a r e d t o t h e d e p t h s ( 5

-

1 0 cm) r e c o r d e d a t s i t e s 1

-

4 ( S y a c r a n i

-

u n p u b l i s h e d ) . T h e s o u t h e r n r e e f s ( s i t e s 4 a n d 5 ) a p p e a r t o b e r e l a t i v e l y

p r o t e c t e d f r o m m o n s o o n i n f l u e n c e s s i n c e P o r i t e s a s s e m b l a g e s , c h a r a c t e r i s t i c o f s h e l e t e r e d w a t e r s ( R o s e n 1 9 7 1 , 1 9 7 5 ) a r e f o u n d a t b o t h s i t e s .

C l e a r l y t h e d e g r e e o f p h y s i c a l e x p o s u r e i s c r i t i c a l a n d i t may b e t h a t a r e v e r s i n g m o n s o o n i n f l u e n c e w h e r e c e r t a i n s i t e s a r e e x p o s e d t o s t r o n g p h y s i c a l i n f l u e n c e s f o r o n l y p a r t o f t h e y e a r p r o v i d e s s u i t a b l e c o n d i t i o n s f o r

c o e x i s t e n c e o f n u m e r o u s c o r a l s p e c i e s . S p e c i e s c a p a b l e o f w i t h s t a n d i n g h e a v y w a v e s u r g e s u c h a s A c r o p o r a

-

a s p e r a / p u l c h r a w i t h h i g h g r o w t h r a t e ( Y a p a n d Gomez 1 9 8 1 a n d r e p r o d u c t i o n b y f r a g m e n t a t i o n ( B o t h w e l l 1 9 8 1 [ 1 9 8 2 1 )

c o l o n i s e t h e o u t e r r e e f f l a t t o g e t h e r w i t h m o r e f r a g i l e p l a t e l i k e s p e c i e s i n a c h a r a c t e r i s t i c h i g h e n e r g y A c r o p o r a a s s e m b l a g e w h i c h i n c l u d e s e n c r u s t i n g a n d b r a n c h i n g

M o n t i p o r a , P o r i t e s , P a v o n a a n d f a v i i d s p e c i e s . I n t h i s way h i g h d i v e r s i t y a n d h i g h c o v e r i s m a i n t a i n e d i n t h e s h a l l o w a n d w e l l i l l u m i n a t e d w a t e r s o f t h e o u t e r r e e f f l a t .

A l t h o u g h s e v e r a l w o r k e r s ( G r i g g a n d M a r a g o s 1 9 7 4 ; P o r t e r 1 9 7 4 ) h a v e d e s c r i b e d o b s e r v e d d i f f e r e n c e s i n

d i v e r s i t y a n d c o v e r o f r e e f c o m m u n i t i e s i n t e r m s o f S a n d e r s s t a b i l i t y - t i m e h y p o t h e s i s , S a n d e r s ( 1 9 6 8 ) h i m s e l f s t a t e s t h a t t h e r e i s n o s u c h t h i n g a s a " p u r e " p h y s i c a l l y

c o n t r o l l e d o r b i o l o g i c a l l y a c c o m m o d a t e d c o m m u n i t y . T h e r e e f s s u r r o u n d i n g t h e P u l a u P a r i c o m p l e x a r e t h e r e s u l t o f b o t h p h y s i c a l a n d b i o l o g i c a l i n f l u e n c e s a n d s o r e p r e s e n t i n t e r m e d i a t e s o n t h e g r a d i e n t b e t w e e n t h e s e e x t r e m e t y p e s o f c o m m u n i t y ; r e e f s t o t h e n o r t h s h o w i n g a t e n d e n c y t o w a r d s p h y s i c a l l y c o n t r o l l e d s y s t e m s w h i l e t h e m o r e d i v e r s e s o u t h e r n r e e f s r e f l e c t a b i a s t o w a r d s m o r e b i o l o g i c a l l y a c c o m m o d a t e d c o m m u n i t i e s . I t i s p e r h a p s s i g n i f i c a n t t h a t b i o l o g i c a l i n t e r a c t i o n s i n v o l v i n g A c a n t h a s t e r a t t a c k ( A z i z a n d S u k a r n o 1 9 7 7 ) a n d a g r e s s i v e o v e r g r o w t h b y d i a d e m n i d

a s c i d i a n s ( B r o w n u n p u b l i s h e d ) h a v e b e e n n o t e d o n l y o n c o r a l s a t t h e m o s t d i v e r s e r e e f ( s i t e 5 ) s t u d i e d i n t h e p r e s e n t

i n v e s t i g a t i o n .

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ACKNOWLEDGEMENTS

T h i s r e s e a r c h w a s c a r r i e d o u t a t t h e P a r i I s l a n d

L a b o r a t o r y o f t h e N a t i o n a l I n s t i t u t e o f O c e a n o l o g y , J a k a r t a . We w o u l d l i k e t o t h a n k D r . APRILANI S o e g i a r t o f o r p r o v i d i n g t h e s e f a c i l i t i e s a n d a l s o D r . K a s i j a n R o m i m o h t a r t o , L a t i f a n d M a d i y o f o r t h e i r i n v a l u a b l e h e l p a n d a s s i s t a n c e . We s h o u l d a l s o l i k e t o a c k n o w l e d g e t h e B r i t i s h C o u n c i l , t h e U n i v e r s i t y o f D i p o n e g o r o , S e m a r a n g a n d t h e U n i v e r s i t y o f N e w c a s t l e u p o n T y n e f o r f i n a n c i a l s u p p o r t .

LITERATURE CITED

A Z I Z , A . , a n d SUKARNO, S . ( 1 9 7 7 ) . P r e l i m i n a r y o b s e r v a t i o n o n l i v i n g h a b i t s o f A c a n t h a s t e r p l a n c i ( L i n n a e u s ) a t P u l a u T i k u s S e r i b u I s l a n d s . M a r . R e s . I n d o n e s i a 1 7 :

-

1 2 1 - 1 3 2 .

BOTHWELL, A . M . ( 1 9 8 1 [ 1 9 8 2 ] ) F r a g m e n t a t i o n , a m e a n s o f a s e x u a l r e p r o d u c t i o n a n d d i s p e r s a l i n t h e c o r a l g e n u s A c r o p o r a . . , P r o c . 4 t h I n t . C o r a l R e e f S y m p . M a n i l a .

-

2 :

1 3 7 - 1 4 4 .

B R A D B U R Y , R . H . , a n d Y O U N G , P . C . ( 1 9 8 1 ) . T h e e f f e c t s o f a m a j o r f o r c i n g f u n c t i o n , w a v e e n e r g y , o n a c o r a l r e e f e c o s y s t e m . M a r . E c o l . P r o g . S e r 5 : 2 2 9 - 2 4 1 .

-

B R O W N , B . E . , a n d DUNNE, R . P . ( 1 9 8 0 ) . E n v i r o n m e n t a l c o n t r o l s o f p a t c h r e e f g r o w t h a n d d e v e l o p m e n t . M a r . B i o l . 5 6 : 8 5 - 9 6 .

DOLLAR, S . J . , ( 1 9 8 2 ) . Wave s t r e s s a n d c o r a l c o m m u n i t y s t r u c t u r e i n H a w a i i . C o r a l R e e f s l ( 2 ) : 7 1 - 8 1 .

-

G R I G G , R . W . , a n d MARAGOS, J . E . ( 1 9 7 4 ) . R e c o l o n i z a t i o n o f h e r m a t y p i c c o r a l s o n s u b m e r g e d l a v a f l o w s i n H a w a i i . E c o l o g y 5 5 : 3 8 7 - 3 9 5 .

-

LOYA, Y . ( 1 9 7 8 ) . P l o t l e s s a n d t r a n s e c t m e t h o d s . I n : S t o d d a r t , D . R . , J o h a n n e s , R . E . ( e d s . ) C o r a l R e e f s : R e s e a r c h M e t h o d s , M o n o g r . o c e a n o g r . m e t h o d , UNESCO, P a r i s , 5 8 1 p p .

PORTER, J.W. ( 1 9 7 4 ) . C o m m u n i t y s t r u c t u r e o f c o r a l r e e f s o n o p p o s i t e s i d e s o f t h e I s t h m u s o f P a n a m a . S c i e n c e N . Y . 1 8 6 : 5 4 3 - 5 4 5 .

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ROSEN, E . R . ( 1 9 7 1 ) . T h e d i s t r i b u t i o n o f r e e f c o r a l g e n e r a i n t h e I n d i a n O c e a n . S y m p . Z o o l . S o c . L o n d . 2 8 :

-

2 6 3 - 3 0 0 .

ROSEN, B . R . ( 1 9 7 5 ) . T h e d i s t r i b u t i o n o f r e e f c o r a l s . U n d e r w a t e r A s s . R e p t . , n . s .

-

1 : 1 - 1 6 .

SANDERS, H . L . ( 1 9 6 8 ) . M a r i n e b e n t h i c d i v e r s i t y

-

a c o m p a r a t i v e s t u d y . A m . N a t . 1 0 2 : 2 4 3 - 2 8 2 .

-

UMBGROVE, J . H . F . ( 1 9 2 9 ) . De k o r a a l r i f f e n d e r

D u i z e n d - E i l a n d e n ( ~ a v a z e e ) . Wet. M e d e d . D r e r i s t M i j n b . N e d . O o s t - I n d i e 1 2 :

-

1 - 4 7 .

UMBGROVE, J . H . F . ( 1 9 3 0 ) . T h e i n f l u e n c e o f t h e m o n s o o n s o n t h e g e o m o r p h o l o g y o f c o r a l i s l a n d s . P r o c . ' 4 t h P a c i f i c S c i . C o n g r . 2A: 5 9 - 5 4 .

-

UMBGROVE, J . H . F . ( 1 9 3 9 ) . M a d r e p o r a r i a f r o m t h e B a y o f B a t a v i a . Z o o l . M e d e d . ( L e i d e n ) 2 2 : 1 - 6 4 .

7

WALLACE, C . C . ( 1 9 7 8 ) . T h e c o r a l g e n u s A c r o p o r a i n t h e

c e n t r a l a n d s o u t h e r n G r e a t B a r r i e r R e e f P r o v i n c e . Mem.

Q d . M u s . 1 8 ( 2 ) : 2 7 3 - 3 1 9 .

-

YAP, H . T . , a n d GOMEZ, E . D . ( 1 9 8 1 [ 1 9 8 2 ) . T h e g r o w t h o f A c r o p o r a p u l c h r a ( B r o o k ) i n B o l i a n o , P a n g a i s a n ,

P h i l i p p i n e s . P r o c . 4 t h I n t . C o r a l R e e f S y m p . M a n i l a . 2 : 2 O 7 - 2 1 3 .

-

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F a m i l y : Genus:

Genus :

T a b l e 1. C o r a l s p e c i e s r e c o r d e d o n r e e f f l a t s a t s i t e s 1

-

5.

1 O r d e r : SCLERACTINIA Bourne

S u b o r d e r : ASTROCOENIIDA Vaughan & W e l l s

S i t e number

2 3 4 5

Genus :

F a m i l y : Genus :

POCILLOPORIDAE Gray STYLOPHORA S c h w e i g g e r S . p i s t i l l a t a E s p e r SERIATOPORA Lamarck S . h y s t r i x Dana POCILLOPORA Lamarck P. d a m i c o r n i s L i n n a e u s

P. v e r r u c o s a E l l i s & S o l a n d e r

+

ACROPORIDAE V e r r i l l ACROPORA Oken

A . r o b u s t a (Dana) A. g r a n d i s ( B r o o k )

A. a b r o t a n o i d e s (Lamarck) A . i n t e r m e d i a in rook) A. formosa (Dana) A. s p l e n d i d a Nemenzo A. v a u g h a n i ( W e l l s )

A. p u l c h r a / a s p e r a ( B r o o k ) / ( D a n a ) ?

+

A. h y a c i n t h u s (Dana)

+

A . c y t h e r e a (Dana) A . p a l i f e r a (Lamarck) A. m i l l e p o r a ( E h r e n b e r g ) A . a c u l e u s (Dana)

A . d e l i c a t u l a ( B r o o k ) A. n a s u t a (Dana)

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Genus :

Genus :

A. c e r e a l i s (Dana) A . d i v e r s a (Brook)

A . v a r i a b , l i s ( ~ l u n z i n g e r ) A . humil i s ( ~ a n a )

A . d i g i t i f e r a (Dana) A. c l a t h r a t a (Brook) A . d i v a r i c a t a (Dana) A . s u b g l a b r a (Brook) A . c a r d u u s (Dana)

A . microphthalma ( V e r r i l l ) A. s q u a r r o s a ( E h r e n b e r g ) A . cymbicyathus (Brook) A. s u r c u l o s a (Dana) ASTREOPORA de B l a i n v i l l e A. myriophthalma (Lamarck) MONTIPORA de B l a i n v i l l e M. t o r t u o s a (Dana) M. minuta Bernard M. i n f o r m i s Bernard M. ramosa Bernard M. composita C r o s s l a n d M. l e v i s (Quelch)

M. f o l i o s a ( ~ e r n a r d ) Suborder : FUNGIIDAE (Duncan) S u p e r f a m i l y : A G A R I C I I C A E (Gray) Family: AGARICIIDAE Gray

Genus : PAVONA Lamarck

P. d a n a i ( M i l n e - ~ d w a r d s & Haime) P. v a r i a n s V e r r i l l

P. venosa (Ehrenberg)

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P. d e c u s s a t a (Dana) Genus : COELOCERIS Vaughan C. m a y e r i Vaughan

S u p e r f a m i l y : FLJNGIICAE (Dana) F a m i l y : FUNGIIDAE (Dana)

Genus : FUNGIA Lamarck

Subgenus: FUNGIA Lamarck

F. ( F u n g i a ) f u n g i t e s ( L i n n a e u s ) Subgenus : CTENACTIS V e r r i l l

F. ( C t e n a c t i s ) e c h i n a t a ( P a l l a s ) S u p e r f a m i l y : PORITICAE ( G r a y ) F a m i l y : PORITIDAE (Gray)

Genus : GONIOPORA d e B l a i n v i l l e

G. s t o k e s i Milne-Edwards & Haime Genus: PORITES L i n k

P. l u t e a Milne-Edwards 6 Haime P. m a t t h a i i W e l l s

P. a t t e n u a t a Nemenzo P. m a y e r i Vaughan P. n i g r e s c e n s .Dana P. a n d r e w s i Vaughan Subgenus : SYNAREA V e r r i l l

P. ( S y n a r e a ) iwayamaensis Eguchi S u b o r d e r : FAVIINA Vaughan 6 W e l l s S u p e r f a m i l y : FAVIICAE Gregory F a m i l y : FAVIIDAE Gregory

S u b f a m i l y : FAVIINAE Gregory Genus: FAVIA Oken

F. p a l l i d a (Dana) F. f a v u s ( F o r s k a a l )

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Genus-r-

Genus :

Genus :

Genus :

Genus :

Genus :

Genus :

Genus :

F. l i z a r d e n s i s Veron, Pichon &

W i j sman-Bes t F. m a t t h a i Vaughan

FAVITES Link

F. c h i n e n s i s c erri ill)

F. a b d i t a ( E l l i s & S o l a n d e r ) F. h a l i c o r a (Ehrenberg)

OULOPHYLLIA Milne-Edwards & Haime O u l o p h y l l i a s p .

CAULASTREA Dana C . tumida M a t t h a i

GONIASTREA Milne-Edwards & Haime G . r e t i f o r m i s (Lamarck)

G . edwardsi C h e v a l i e r G . a s p e r a ( V e r r i l l ) G . f a v u l u s (Dana)

G. p e c t i n a t a ( ~ h r e n b e r g ) PLATYGYRA Ehrenberg P. p i n i C h e v a l i e r

P. s i n e n s i s Milne-Edwards & Haime P. d a e d a l e a ( E l l i s & S o l a n d e r ) P. verweyi Wijsman-Best

HYDNOPHORA F i s c h e r de Waldheim H. e x e s a ( P a l l a s )

MONTASTREA de B l a i n v i l l e M. m a g n i s t e l l a t a C h e v a l i e r

M. v a l e n c i e n n e s i (Edwards & Haime) LEPTASTREA Milne-Edwards & Haime L. p r u i n o s a C r o s s l a n d

t

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Genus: CYPHASTREA Milne-Edwards 6 Haime C . m i c r o p h t h a l m a (Lamarck)

C . s e r i a l i a ( F o r s k a l ) Genus : ECHINOPORA Lamarck

E. h o r r i d a Dana F a m i l y : OCULINIDAE Gray

S u b f a m i l y : GALAXEINAE ( ~ a u g h a n 6 W e l l s ) G e n u s : GALAXEA Oken

G . f a s c i c u l a r i s ( L i n n a e u s ) F a m i l y : MERULINIDAE V e r r i l l Genus : MERULINA E h r e n b e r g

M. a m p l i a t a ( ~ l l i s 6 S o l a n d e r ) G e n u s : SYMPHYLLIA Milne-Edwards 6 Haime

S. n o b i l i s (Dana)

S u b o r d e r : CARYOPHYLLINA Vaughan 6 W e l l s S u p e r f a m i l y : CARYOPHYLLIICAE Gray F a m i l y : CARYOPHYLLIIDAE Gray

S u b f a m i l y : EUSMILIINAE Milne-Edwards

& Haime Genus : EUPHYLLIA Dana

E . g l a b r e s c e n s (Chamisso & E y s e n h a r d t ) O r d e r : COENOTHECALIA Bourne

F a m i l y : HELIOPORIDAE M o s e l e y Genus: HELIOPORA de B l a i n v i l l e

H. c o e r u l e a ( P a l l a s ) C l a s s : HYDROZOA Huxley O r d e r : MILLEPORINA H i c k s o n

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Family: MILLEPORIDAE B l a i n v i l l e Genus : MILLEPORA Linnaeus

M. exaesa F o r s k a l

M. p l a t y p h y l l a Hemprich &

Ehrenber g M . dichotoma F o r s k a l

TOTAL NUMBER OF CORAL SPECIES : 21 28 20 38 57

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* JAVA SEA '

F i g u r e 1. P a r i I s l a n d Complex s h o w i n g s t u d y s i t e s a n d p o s i t i o n o f s h i n g l e r a m p a r t s ( m l a n d i t s l o c a t i o n w i t h i n t h e J a v a S e a ( i n s e t ) .

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SlTE 1 SlTE 2 SlTE 3

REEF F I A T

PROFILE - - 'mi XI

'0 3 0 50 70 90 110 r n w m i 3 l i

ACROSS R E E F F L A T

y

; Rs; FRR4ngTl

&.d ' 0 R E E F F L A T

. C O V E R 8 Y D O M I N A N T SPECIES

(/.A-

2,) ,,ll i n 90met!as

SlTE 4

D . p l h O-,,

b l - REEF F L A T

mart l o . datum

("I PROFILE

?0 10 . . 3 0 . . 50 . . 70

.

. 9 0 . . 110 . . . 130 1 5 0 110 190

80- L l V E X L E R A C T I N I A N C O V E R ACROSS REEF F L A T zowm

IDO-

D E A O S C L E R A C T I N I A N

cower

% C O V E R B Y D O H I N A N T SPECIES

kLOO[

ACROSS R E E F F L A T

W I!

REEF F L A T '' ' ' charm l i ,

1m1

10 3 0 150 7ii -in - , , . , r

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ACROSS REEF F L A T 17ve .,,,.

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0

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.

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C O V E R ACROSS

5. C O V E R a Y DOMINANT SPECIES

, I""[ ACROSS REEF F L A T

CD1.1 , , , I

, , I . ,

-

mevre.

F i g u r e 2 . D i s t r i b u t i o n o f l i v i n g a n d d e a d a ) P r o f i l e o f r e e f

b ) L i v e s c l n r a c t i n i a n c c v e r

SlTE 5

Mod, i h , n q l e R.,rn.*.!

R E E F F L A T

PROFILE

. , , . , . , , . . . , . . 4

REEF SLOPE

1 0 3 0 5 0 70 9 0 1 1 0 130 150

L l V E S C L E R A C T I N I A N C O V E R

mt m ACROSS R E E F F L A T

D E A D S C L E R A C T I N I A N C O V E R ACROSS R E E F F L A T

% C O V E R B V D O M I N A N T SPECIES

% Inn[ ACROSS R E E F F L A T corsr ,a

n E E F F L A T 1 1 ,.

datum P R O F I L E R E E F SLOPE

O E A D S C L E R A C T I N I A N COVER ACROSS R E E F F L A T

COVER B Y D O M I N A N T SPECIES A C R O S n r r r FLS

/

c o r a l a c r o s s t h e r e e f f l a t s a t s i t e s c ) Dead s c l e r a c t i n i a n c o v e r d ) Dominant s p e c i e s c o v e r

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S l T E 1

A.aspera/pulchra

A.digitifera

A.hyancinthus A. d i v e m A.formosa A. intermedia

SlTE 4

A.digitifera

A. formosa

SlTE 5

A. formosa A.intermedia A.divem A. cerealis A.delicatula A. variabilis A.surculasa A. divarica ta A.squamosa A.naruta

SlTE 3

-

1 1 -. 1 ' 1 1 1 1 1 1 1 1 1 1 1 1

0 2 4 6 0 2 4 6 8 10 12 14 1 6 1 8 20 22 24 26 28

Distance across outer rampan Im)

F i g u r e

3 .

Z o n a t i o n o f A c r o p o r a s p e c i e s a c r o s s t h e o u t e r r e e f f l a t s a t s i t e s 1 -

5 .

Referensi

Dokumen terkait

Ground water arrives from the east and the predominant flow direction from the proposed landfill site is to the south and north west, with a relatively steep hydraulic gradient of