Figures & data
![Figure 1 A, Geographic distribution range of Macruronus magellanicus around South America and main oceanic currents in the SE Pacific. B, Study area showing the 1×1° cells and specific geographical domains used to compute SSTA averages along the Chilean coast. WWD-B = west wind drift bifurcation, HC = Humboldt Current, CHC = Cape Horn Current, ACC = Antarctic Circumpolar Current, ONA = oceanic nursery area (hypothetical), ENA = estuarine nursery area, MSA = main spawning area.](/cms/asset/13eb804f-f092-49fe-9b64-eb4134e72f92/tnzm_a_846920_f0001_b.jpg)
![Figure 2 A, Time series of SSB. B, One-year-old fish recruitment of Macruronus magellanicus off southern Chile (1980–2010). Dotted lines are indicative of regime shifts identified in Table 1.](/cms/asset/836fcd40-d131-464e-a6f6-1e6946113926/tnzm_a_846920_f0002_b.jpg)
![Figure 3 Annual averages of SSTA in coastal waters of the SE Pacific Ocean (35°S–47°S) from 1981 to 2010. Data intended to represent the first months of life of Macruronus magellanicus, from July to December. Colour scale on the right indicates temperature anomaly in °C.](/cms/asset/753c22c9-5b50-4850-8659-1850237235f8/tnzm_a_846920_f0003_c.jpg)
Table 1 Detection of shifts in sea-surface temperature anomaly (SSTA), latitudinal position of the west wind drift bifurcation (WWDL), southern oscillation index (SOI), spawning stock biomass (SSB) and recruitment time series (1981–2010).
![Figure 4 A, Observed relationships between hind-cast recruitment rates (R/SSB) of Macruronus magellanicus and SSTA in its main fishing area 1981–2008 and predicted values from an auto-regressive linear regression model. B, Relationship between hind-cast recruitment (R, in millions) and SSB (in tonnes) during the same period, and predictions from a non-linear conditional Ricker's (Citation1954) S-R model. Year 2008 is highlighted in both panels as an anomalous year, although it was not excluded from any analysis.](/cms/asset/1120d090-0cda-4e38-813a-37a7d68b55bc/tnzm_a_846920_f0004_b.jpg)