been used to reconstruct sea surface temperature (SST) since the 1980s. However,
alkenone-based SST reconstructions in the northern high latitude oceans show significant
bias towards warmer temperatures in core-tops, diverge from other SST proxies in down
core records, and are often accompanied by anomalously high relative abundance of the
C37 tetra-unsaturated methyl alkenone (% C37: 4). Elevated% C37: 4 is widely interpreted …