Paleoecological evidence for decadal increase in phytoplankton biomass off northwestern Australia in response to climate change.

In comparison, STARS did not detect a significant shift in annual river discharge of the Fitzroy River during 1963–2011, despite a slightly increasing trend after the 1990s (Figure 3 c).

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In summary, the paleoecological evidence from Cygnet Bay demonstrated that SST and terrestrial input have significantly increased since 1997 in the Kimberley region, and the biomasses of diatoms and dinoflagellates corresponded to these changes with an increasing trend.

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