Spatial coherences revealed a highly significant relationship at periods around 12 years (g) and on average over long timescales (left p -value on panel g, long timescales defined as > 4 years) but no relationship (right p -value) for short timescales (< 4 years).
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Synchrony is more than its top-down and climatic parts: interacting Moran effects on phytoplankton in British seas.
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