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| Polished, gold coated coral
sample for ion microprobe analysis. |
The Effect of Algal Symbionts
on the Accuracy of Sr/Ca Paleotemperatures from Coral
Anne L. Cohen, Kathryn E. Owens, Graham D.
Layne, Nobumichi Shimizu
Originally published in Science Express as
10.1126/science.109330 on March 7, 2002
Science, Vol. 296, Issue 5566, 331-333, April 12, 2002
The strontium-to-calcium ratio (Sr/Ca) of reef coral
skeleton is commonly used as a paleothermometer to estimate sea
surface temperatures (SSTs) at crucial times in Earth's climate
history. However, these estimates are disputed, because uptake of
Sr into coral skeleton is thought to be affected by algal symbionts
(zooxanthellae) living in the host tissue. Here, we show that significant
distortion of the Sr/Ca temperature record in coral skeleton occurs
in the presence of algal symbionts. Seasonally resolved Sr/Ca in
coral without symbionts reflects local SSTs with a temperature sensitivity
equivalent to that of laboratory aragonite precipitated at equilibrium
and the nighttime skeletal deposits of symbiotic reef corals. However,
up to 65% of the Sr/Ca variability in symbiotic skeleton is related
to symbiont activity and does not reflect water temperature.
Complete text version
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Kinetic Control of Skeletal
Sr/Ca in a Symbiotic Coral: Implications for the Paleotemperature
Proxy
Anne L. Cohen, Graham D. Layne, and Stanley
R. Hart, Woods Hole Oceanographic Institution
Philip S. Lobel, Boston University Marine Program
Paleoceanography, Vol. 16, No. 1, Pages 20-26,
February 2001
Modeling of past climates is critically dependent on estimates of
past sea surface temperatures (SSTs) for which one of the principal
techniques used is the measurement of Sr/Ca ratios in corals (Guilderson
et al. 1994, McCulloch et al., 1999; Hughen et al., 1999). The link
between coral Sr/Ca and SST is not well understood and there have
beena number of descrepant observations (de Villiers et al., 1995;
Alivert, 1998). Corals with symbiotic zooxanthellae are known to
show large diurnal fluctuations in calcification rate associated
with the photosynthetic activity of their symbionts. Using detailed
measurements with the ion microprobe, we compared the Sr/Ca content
of discrete daytime and nighttime skeletal structures in the massive
hermatypic coral Porites lutea over the course of 1 year and a seasonal
temperature range of 4ęC. The Sr/Ca content of daytime skeleton
is always lower thatn that of adjacent nighttime skeleton. While
the slope of the nighttime Sr/Ca-SST correlation is close to that
seen in inorganic aragonite precipitates, that of the daytime correlation
is>4 times as steep. We attribute these differences to the role
of photosynthesis in calcification and conclude that bulk Sr/Ca
is related principally to daytime calcification rate rather than
directly to SST. More reliable estimates of past SST may be arrived
at through selective analysis of nighttime skeleton.
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| Porites skeleton in thin
section. |
Diurnal Changes in Microstructure and Microscale
Chemistry of Reef Coral Skeleton
Anne L. Cohen, Graham D. Layne, Nobumichi Shimizu
Poster #1 presented at AGU in 2001
Calcification by corals with symbiotic zooxanthellae occurs 3 times
faster in daylight than it does at night. We investigated the effects
of light enhanced calcification on the microstructure and elemental
chemistry of the aragonite skeleton over the diurnal cycle. The morphology
of nighttime crystals accreted in the absence of photosynthesis imitates
that of slow growing inorganic cements in a high CO2 environment.
The morphology of daytime crystals accreted during the photosynthetic
period imitates that of fast growing inorganic cements in a low CO2
environment. We used an Cameca IMS 3f ion microprobe to measure changes
in the strontium-calcium content (Sr/Ca) of the growing skeleton of
the tropical reef coral, Porites lutea, over the diurnal cycle. Sr/Ca
in nighttime skeleton is close to equilibrium values but a large decrease
in Sr/Ca is observed as the daytime crystals grow to fill the extracellular
calcifying space in summer. The amplitude of change in skeletal Sr/Ca
between night and day is as large as the annual cycle in Sr/Ca. During
summer, at peak water temperature and symbiont photosynthesis, the
amplitude of the diurnal Sr/Ca cycle is 3 times greater than that
incurred only by the diurnal change in water temperature. During winter,
the amplitude of the diurnal Sr/Ca cycle is equivalent to that incurred
by temperature alone. Our data show that processes linked to symbiont
photosynthesis exert significant influence on both skeletal microstructure
and microchemistry, and that temperature is not the primary control
of diurnal Sr/Ca variability in reef coral skeleton.
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| Astrangia skeleton. |
The Biological Nature of Geochemical Proxies:
Algal Symbionts Control Coral Chemistry
Kathryn E. Owens, Anne L. Cohen, Graham D. Layne,
Nobumichi Shimizu
Poster #2 presented at AGU in 2001
The strontium/calcium ratio (Sr/Ca) of reef coral skeleton is used
as a paleothermometer to estimate sea surface temperatures (SSTs)
at crucial times in the earths climate history. However, these
estimates are disputed because uptake of Sr into coral skeleton is
thought to be affected by algal symbionts (zooxanthellae) living in
the host tissue. Here we show for the first time that significant
distortion of the Sr/Ca temperature record in coral skeleton occurs
in the presence of algal symbionts. Microscale measurements of skeletal
Sr/Ca in co-occuring symbiotic and asymbiotic colonies of Astrangia
poculata were made using SIMS ion microprobe. Seasonally-resolved
Sr/Ca in asymbiotic skeleton reflects local SSTs with a temperature
sensitivity equivalent to laboratory aragonite precipitated at equilibrium,
and the nighttime skeletal deposits of symbiotic reef corals. However,
up to 65% of the Sr/Ca variability in symbiotic skeleton is related
to the symbiosis and does not reflect water temperature. Our data
indicate that Sr/Ca in asymbiotic species and nighttime accretions
of tropical reef corals should be targeted for accurate estimates
of past SSTs.
Full poster PDF version
(Acrobat 5.0 - 1.3 MB)
(You will need Acrobat Reader 5.0 - a free version is available
for download
here) |
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