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We presented here two 2700 years' long records from the Santa Barbara Basin of ENSO/PDO proxies based on coccolithophores: one resulting from the relative abundance in the assemblage of one warm species Gephyrocapsa oceanica and the other from the degree of calcification of a group of three abundant species (Emiliania huxleyi, G. ericsonii, G. muellerae).
By contrast, many southern "warm" species can survive the cold summer temperatures in the north.
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Under global warming species assemblages are expected to shift upwards in altitude, whereby lowland species will be important to sustain natural forests at mid-altitudes (Colwell et al. 2008; Feeley and Silman 2010).
As the planet warms, species around the world are engaged in a race against time to either adapt or move to cooler habitats.
The warming displaces warmer species northward and affects species distribution and local diversity.
Atlantic bottlenose dolphins like Stormy, though, are a warm water species usually found off Florida and in the Gulf of Mexico.
Xt is the total number of warm transitional species (Thalassionema nitzschioides, Thalassiosira oestrupii, and Coscinodiscus radiatus) and Xc is the total number of subarctic to arctic (cold-water) species.
Nevertheless earlier studies (e.g. Grima et al. 1995;Otero et al. 1997 Carvalho and Malcata 2005 Huerlimann et al. 2010) addressing the potential for EPA/DHA mass production focused primarily on warm (temperate) species.
This relatively warm water species get into the Santa Barbara Basin in higher relative abundance when the California current relaxes (De Bernardi et al. 2005; De Bernardi et al. 2008; Grelaud et al. 2009b).
The detection of IncA/C plasmids in three of the isolates recovered from warm water species was noteworthy.
Significant elements in this flora (e.g., Chondria baileyana) are warm temperate species with disjunct distributions south of the Bay of Fundy that became trapped in the Gulf of St. Lawrence during the postglacial hypsithermal interval.
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