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Multidecadal, centennial, and millennial variability in sardine and anchovy abundances in the western North Pacific and climate–fish linkages during the late Holocene
- Kuwae, Michinobu, Yamamoto, Masanobu, Sagawa, Takuya, Ikehara, Ken, Irino, Tomohisa, Takemura, Keiji, Takeoka, Hidetaka, Sugimoto, Takashige
- Progress in oceanography 2017 v.159 pp. 86-98
- Engraulis japonicus, anchovies, climate change, ecosystems, fisheries, pelagic fish, sardines, snow, surface water temperature, time series analysis, trees, winter, Japan
- Paleorecords of pelagic fish abundance could better define the nature of fishery productivity dynamics and help understand responses of pelagic fish stocks to long-term climate changes. We report a high-resolution record of sardine and anchovy scale deposition rates (SDRs) from Beppu Bay, Southwest Japan, showing multidecadal and centennial variability in the abundance of Japanese sardine and Japanese anchovy during the last 2850years. Variations in the sardine SDR showed periodicities at ∼50, ∼100, and ∼300yr, while variations in the anchovy SDR showed periodicities at ∼30 and ∼260yr. Comparisons between and correlation analyses of the time series of the sardine and anchovy SDRs demonstrate that there is not a consistent out-of-phase relationship during the last 2850years. This indicates that the multidecadal alternations in the sardine and anchovy populations commonly seen in the 20th century did not necessarily occur during earlier periods. The Japanese sardine SDR record shows a long-term decreasing trend in the amplitudes of the multidecadal to centennial fluctuations. This decreasing trend may have resulted from an increasing trend in the winter sea surface temperature in the western North Pacific. The multicentennial variability in sardine abundance during the last millennium is consistent with the variabilities in the abnormal snow index in East Asia and the American tree ring-based Pacific Decadal Oscillation index, suggesting a basin-wide or regional climate–marine ecosystem linkage.