Factors influencing the stable carbon and oxygen isotopic composition of Porites lutea coral skeletons from Phuket, South Thailand

Coral Reefs

Volumn 15, Issue 1, 1996, Pages 43-57

  Allison, N ^a,c   Tudhope, A W ^a   Fallick, A E ^b  

^a Grant Institute of Geology   (United Kingdom)

^b SCOTTISH UNIVERSITIES ENVIRONMENTAL RESEARCH CENTRE   (United Kingdom)

^c UNIVERSITY OF PLYMOUTH   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

CALCIFICATION RATE; CARBON; CORAL; ENVIRONMENTAL FACTORS; ISOTOPIC COMPOSITION; OXYGEN; SALINITY; SKELETAL GROWTH RATE; TEMPERATURE;

THAILAND, PHUKET;

PORITES LUTEA;

EID: 0029667382     PISSN: 07224028     EISSN: None     Source Type: Journal    
DOI: 10.1007/s003380050027     Document Type: Article

References (5)

1. Boto K, Isdale P (1985) Fluorescent bands in massive corals result from terrestrial fulvic acid inputs to nearshore zone. Nature 315: 396-37
2. Brown BE, Le Tissier MDA, Howard LS, Charuchinda M, Jackson JA (1986) Asynchronous deposition of dense skeletal bands in Parités lutea (Edwards and Haime). Mar Biol 93:83-89
3. Carr DJ (1992) Quaternary sediments of a tropical estuary and bay: Phangnga Bay, South Thailand. Unpublished PhD thesis, University of Edinburgh
4. Chakraborty S, Ramesh R (1993) Monsoon-induced sea surface temperature changes recorded in Indian corals. Terra Nova 5:545-551
5. Chansang H, Phongsuwan N, Boonyanate P ( 1992) Growth of corals under effect of sedimentation along the northwest coast of Phuket Island, Thailand. Proc 7th Int Coral Reef Symp 1:241-248