Extended Data Fig. 6: Spawning would occur earliest in the southern part of the study area but probably has shifted earlier due to warming throughout the region.
From: Wrong-way migrations of benthic species driven by ocean warming and larval transport
Maps show long-term averages (a-d) and temporal trends (e-h) in onset dates for spawning at four temperature thresholds (t8, t10, t12, t14) in the Northwest Atlantic region. Onset dates were calculated from corrected HC climatology, and trends were calculated from linear regression of onset dates versus year at each grid point. Regions with no color are always below the indicated temperature threshold.
