Anomalous poleward advection facilitates episodic range expansions of pelagic red crabs in the eastern North Pacific

The episodic stranding of millions of pelagic red crabs (Pleuroncodes planipes) along California beaches is a striking and puzzling phenomenon. Pleuroncodes planipes are usually abundant off Baja California, Mexico, and their appearance in central California is thought to coincide with anomalously warm waters and northward advection related to El Nino. This anecdotal association has stimulated many hypotheses, but no hypothesis has gained clear and convincing support. Motivated by an unprecedented number of P. planipes strandings and at-sea observations in 2015-2019, we compiled 10 P. planipes datasets spanning 1950-2019, tested the anomalous advection hypothesis using a transport analysis from 1981 to 2010, and explored other compelling hypotheses. We found P. planipes presence off central California was related to anomalous advection of waters from Mexico, sometimes but not always associated with El Nino events, with P. planipes likely remaining residents of northern waters for several years without additional anomalous transport but potentially facilitated by warm waters. By identifying a mechanism behind episodic P. planipes range expansions, we show that a source water index could provide an early indicator for anomalous events in the future.

Automated summary

The stranding of millions of pelagic red crabs along California beaches is related to anomalously warm waters and northward advection associated with El Nino. Research suggests that the pelagic red crabs may remain residents of northern waters for several years, with a source water index potentially serving as an early indicator for anomalous events in the future.