Access the full text.
Sign up today, get DeepDyve free for 14 days.
T. McClanahan, N. Muthiga, S. Mangi (2001)
Coral and algal changes after the 1998 coral bleaching: interaction with reef management and herbivores on Kenyan reefsCoral Reefs, 19
T. Hughes (1994)
Catastrophes, Phase Shifts, and Large-Scale Degradation of a Caribbean Coral ReefScience, 265
L. McCook, J. Jompa, G. Diaz-Pulido (2001)
Competition between corals and algae on coral reefs: a review of evidence and mechanismsCoral Reefs, 19
G. Diaz-Pulido, L. McCook (2002)
The fate of bleached corals: patterns and dynamics of algal recruitmentMarine Ecology Progress Series, 232
B. Brown (1997)
Coral bleaching: causes and consequencesCoral Reefs, 16
D. Littler, M. Littler (2003)
South Pacific reef plants
J. Veron (1993)
Corals of Australia and the Indo-Pacific
E. Titlyanov, T. Titlyanova, I. Yakovleva, Y. Nakano, R. Bhagooli (2005)
Regeneration of artificial injuries on scleractinian corals and coral/algal competition for newly formed substrateJournal of Experimental Marine Biology and Ecology, 323
L. McCook (2001)
Competition between corals and algal turfs along a gradient of terrestrial influence in the nearshore central Great Barrier ReefCoral Reefs, 19
Francis Breedon, P. Fisher (1996)
M0: Causes and ConsequencesThe Manchester School, 64
Yossi Loya, K. Sakai, K. Yamazato, Y. Nakano, Hariyani Sambali, R. Woesik (2001)
Coral bleaching: the winners and the losersEcology Letters, 4
Y. Nakano, S. Nakamura (1993)
Annual Record of Coastal Observation at Sesoko Marine Science Center in 1991Galaxea, 11
The species composition and distribution of marine plants on the fringing reef of Secoko Island were studied before and after the mass coral mortality in 1998. The study showed that changes in the bottom communities that occurred after bleaching of corals were caused by the presumed development of marine plants substituting reef-building corals on the bottom. The number of algal species grew from 211 to 345. The projective cover (PC) of hard substrate with macroalgae increased: in 1998, it was 1–10% in the subtidal zone and 20–50% in the intertidal zone, while in 2002 through 2005, the PC reached 71% in the subtidal and 40–85% in the intertidal zone. It is assumed that the phase of the “plant reef” on Sesoko Island is a temporary event, and that the coral reef can recover within several decades, unless a natural catastrophe occurs again.
Russian Journal of Marine Biology – Springer Journals
Published: Mar 20, 2007
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.