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Abstract Sea level and deep-sea temperature variations are key indicators of global climate changes. For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O (δc) records are indispensable because they reflect changes in both deep-sea temperature and seawater δ18O (δw); the latter are related to ice volume and, thus, to sea level changes.
Abstract Boron isotopic and elemental analysis of coral aragonite can give important insights into the calcification strategies employed in coral skeletal construction. Traditional methods of analysis have limited spatial (and thus temporal) resolution, hindering attempts to unravel skeletal heterogeneity.
A 29-year old with a heart attack presents the opportunity to consider patient-specific risk factors, such as racial background. This case demonstrates the genetic/cultural risk factors increasing cardiovascular risk amongst South Asian populations.
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