ABSTRACT
60th Anniversary of Geological Society of Korea
>> 88
Reef-building coral records surrounding environmental conditions in its skeleton. There is consensus on controlling factor of skeletal δ
18O (δ
18Oc), namely SST (sea surface temperature) and seawater δ
18O composition.
However, that of skeletal δ
13C ( δ
13Cc) is still controversial because δ
13Cc shows correlation with different environmental factors at different locations.
In order to better understand the controlling factor of δ
13Cc, two different coral species, Porites sp. and Platygyra ryukyuensis, were collected at the exactly same site from Ishigaki Island, Japan, and analyzed for δ
13Cc and δ
18Oc.
Then the results were compared with observed environmental variables.
δ
13Cc of Porites shows a clear seasonal fluctuation matching that of solar radiation, high in summer and low in winter. In contrast, δ
13Cc of Platygyra showed an opposite pattern to that of Porites with weaker seasonality. Both were exposed to same environmental conditions during growth, so these opposed trends should be attributed to species-dependent responses against same environmental condition.
It is likely caused by different symbiotic algae associations of two species, resulting in different photosynthetic efficiency to the same light stress. For example, photosynthesis of symbiotic algae in Porties is active during summer, while that in Platygyra during winter. Photosynthesis of symbiotic algae takes up
12C preferentially, leaving
13
C-enriched carbon pool for coral calcification. Thus active photosynthesis of symbiotic algae results in higher δ
13Cc; during summer for Porites and during winter for Platygyra. These results agree well with spatial distribution of Platygyra found in middle latitude region, where Porites is not distributed, with colder temperature and less light
intensity. Higher photosynthetic efficiency of symbiotic algae seems providing its host more tolerance to low light intensity. Despite of the opposed responses of two species, both species δ
13Cc variation can be used as a proxy for solar radiation.
Michiyo Shimamura
1,*, Kiseong Hyeong
1, Chan-Min Yoo
1, Tsuyoshi Watanabe
2, Tomohisa Irino
2, and Woong-Seo Kim
11
Korea Ocean Research and Development Institute, Ansan, 426-744, Korea,
2