Sr/Ca and δ18O seasonality in a Porites coral from the MIS 9 (339-303 ka) interglacial
Past changes in the seasonal distribution of insolation across the Earth's surface are thought to play a critical role in Quaternary climate cycles. In this study we use Sr/Ca and δ18O as geochemical proxies in the skeleton of a fossil Porites coral to r
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|Source:||Earth and Planetary Science Letters|
|01_Ayling_Sr/Ca_and_δ18O_seasonality_in_2006.pdf||839.75 kB||Adobe PDF||Request a copy|
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