Fig. 2
From: Seasonal trophic controls drive population variability in a foundational marine copepod

Mean spring and fall interannual trends of C. finmarchicus (Calfin) in Wilkinson Basin (a) and Jordan Basin (c), with dots representing the average seasonal abundance (units of ln[abundance m− 3 + 1]) and lines representing the LOESS smooth curve for easier visualization of trends. CCM results for Wilkinson Basin (b) and Jordan Basin (d) indicate significant evidence for Spring Calfin → Fall Calfin causality.