ABSTRACT Fossilized tests of foraminifera are arguably the most important archives of past climate, and many of the longest paleoclimate records have been compiled by the measurement of the oxygen and carbon isotope composition of foraminiferal tests collected from seafloor sediments. Since the analytical methodology was established in the late 1940s, multiple tests are pooled and analyzed, resulting in a single oxygen and carbon isotope value representing their mean composition. These records compiled by multi-test analysis provide, in most scenarios, a faithful picture of the Earth’s past climate. However, foraminiferal tests feature isotopic heterogeneity on micrometer scales and thus record a wealth of additional information that can be assessed by secondary ion mass spectrometry (SIMS) using spots of 10 µm or less. This paper provides a history of in situ stable isotope measurements in foraminifer tests by SIMS, discusses landmark studies, and offers an outlook on future research.
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