However, significant changes in δ 13 C shell through time can also indicate broad shifts in ocean carbonate chemistry, as documented by a negative trend in modern δ 13 C shell in M . californianus relative to δ 13 C shell of archival and archaeological M . californianus shells collected in Washington State [ 58 ].
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Interpreting life-history traits, seasonal cycles, and coastal climate from an intertidal mussel species: Insights from 9000 years of synthesized stable isotope data.
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