Sclerochronology and geochemical variation in limpet shells (Patella vulgata): A new archive to reconstruct coastal sea surface temperature

TY - JOUR

T1 - Sclerochronology and geochemical variation in limpet shells (Patella vulgata): A new archive to reconstruct coastal sea surface temperature

AU - Fenger, Tracy

AU - Surge, Donna

AU - Schoene, Bernd

AU - Milner, Nicky

PY - 2007/7/4

Y1 - 2007/7/4

N2 - [1] Climate archives contained in shells of the European limpet, Patella vulgata, accumulated in archaeological deposits can potentially provide much needed information about Holocene environmental change in midlatitude coastal areas. Before reconstructing climate information preserved in these zooarchaeological records, we studied the controls on oxygen and carbon isotope ratios (delta O-18 and delta C-13, respectively) in modern specimens. We tested the hypothesis that P. vulgata precipitates its shell in isotopic equilibrium with the ambient water by comparing delta O-18(SHELL) with predicted values. Predicted delta O-18(SHELL) was constructed using observed sea surface temperature (SST) records and the equilibrium fractionation equation for calcite and water. We assumed a constant delta O-18(WATER) value of +0.10 parts per thousand (VSMOW) based on published regional measurements. Comparison of delta O-18(SHELL) with predicted values revealed that delta O-18(SHELL) values were higher than expected by +1.01 +/- 0.21 parts per thousand. Consequently, estimated SST calculated from delta O-18(SHELL) was 4.2 +/- 2.3 degrees C lower than observed SST. However, because of the relatively uniform offset between observed and expected d18 O, an adjustment can be made to account for this predictable vital effect. Thus past climate can be reliably reconstructed using this temperature proxy once the offset is taken into account. delta C-13 values have a similar cyclicity to the delta O-18 variation and therefore vary seasonally. However, delta C-13 is slightly out of phase relative to delta O-18. An overall negative shift in delta C-13(SHELL) over the lifetime of the individual indicates a vital effect associated with ontogeny. Further study of environmental and ecological factors that influence shell delta C-13 is required to evaluate fully the potential of carbon isotope ratios as a useful environmental proxy.

AB - [1] Climate archives contained in shells of the European limpet, Patella vulgata, accumulated in archaeological deposits can potentially provide much needed information about Holocene environmental change in midlatitude coastal areas. Before reconstructing climate information preserved in these zooarchaeological records, we studied the controls on oxygen and carbon isotope ratios (delta O-18 and delta C-13, respectively) in modern specimens. We tested the hypothesis that P. vulgata precipitates its shell in isotopic equilibrium with the ambient water by comparing delta O-18(SHELL) with predicted values. Predicted delta O-18(SHELL) was constructed using observed sea surface temperature (SST) records and the equilibrium fractionation equation for calcite and water. We assumed a constant delta O-18(WATER) value of +0.10 parts per thousand (VSMOW) based on published regional measurements. Comparison of delta O-18(SHELL) with predicted values revealed that delta O-18(SHELL) values were higher than expected by +1.01 +/- 0.21 parts per thousand. Consequently, estimated SST calculated from delta O-18(SHELL) was 4.2 +/- 2.3 degrees C lower than observed SST. However, because of the relatively uniform offset between observed and expected d18 O, an adjustment can be made to account for this predictable vital effect. Thus past climate can be reliably reconstructed using this temperature proxy once the offset is taken into account. delta C-13 values have a similar cyclicity to the delta O-18 variation and therefore vary seasonally. However, delta C-13 is slightly out of phase relative to delta O-18. An overall negative shift in delta C-13(SHELL) over the lifetime of the individual indicates a vital effect associated with ontogeny. Further study of environmental and ecological factors that influence shell delta C-13 is required to evaluate fully the potential of carbon isotope ratios as a useful environmental proxy.

KW - gastropoda

KW - oxygen

KW - carbon

KW - climate

KW - temperature proxy

KW - STABLE-ISOTOPE COMPOSITION

KW - SEAWATER CARBONATE CONCENTRATION

KW - MOLLUSK CHIONE-CORTEZI

KW - GULF-OF-CALIFORNIA

KW - BIVALVE MOLLUSK

KW - OXYGEN ISOTOPES

KW - GROWTH BANDS

KW - ENVIRONMENTAL CONTROLS

KW - MERCENARIA-MERCENARIA

KW - BIOLOGICAL CARBONATES

U2 - 10.1029/2006GC001488

DO - 10.1029/2006GC001488

M3 - Article

SN - 1525-2027

VL - 8

SP - -

JO - Geochemistry geophysics geosystems

JF - Geochemistry geophysics geosystems

IS - 7

M1 - Q07001

ER -