Potential and limitations of applying the mean temperature approach to fossil otolith assemblages.

However, MTO based on pelagic species shows a decreasing trend along the Israeli depth gradient: the MTO at 10-m depth is 17.3 °C, but only 13.6 °C at 40-m depth (Table 4 ), while the sea surface temperature for this area is estimated at 24 °C on average (Avnaim-Katav et al. 2019 ; Castañeda et al. 2010 ; Essallami et al. 2007 ).

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