Titlebook: Coccolithophores; From Molecular Proce Hans R. Thierstein,Jeremy R. Young Book 2004 Springer-Verlag Berlin Heidelberg 2004 Ocean.Oceanograp

Peristalsis

Alter Session Set Current_Schemad to shelf and epeiric sea environments. They spread into the open ocean in the Cretaceous, and with this became a major factor in governing the carbonate cycle in the sea. With the development of dissolution-resistant forms, such as ., the coccolithophores perturbed the carbonate system and switche

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https://doi.org/10.1007/978-1-4612-1510-3rine phytoplankton group in the production of dimethyl sulfide ((CH.).S; DMS). Our aim here is to provide some general background information on DMS for non-specialists, but also to highlight current knowledge and what we believe to be significant gaps, for those with a specific interest in coccolithophores, other haptophytes and DMS.

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Dimethyl sulfide production: what is the contribution of the coccolithophores?rine phytoplankton group in the production of dimethyl sulfide ((CH.).S; DMS). Our aim here is to provide some general background information on DMS for non-specialists, but also to highlight current knowledge and what we believe to be significant gaps, for those with a specific interest in coccolithophores, other haptophytes and DMS.

wall-stress

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What is new in coccolithophore biology?ospheres in wild samples. It has been confirmed that holococcolithophores and other “anomalous” coccolithophores are not autonomous but stages in the life cycle of oceanic heterococcolithophores. The existence of such heteromorphic life cycles linking former “species” has far reaching consequences o

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Pigment diversity of coccolithophores in relation to taxonomy, phylogeny and ecological preferences. Cultured haptophytes have played a relevant role in advances in this analytical field and many pigments described in the literature were first detected in members of this algal group. The present chapter provides an historical overview of pigment detection in the Haptophyta and contains new data o

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Coccolithophores and the biological pump: responses to environmental changes formation of calcite skeletons in the surface layer and their subsequent sinking to depth modifies upper-ocean alkalinity and directly affects air/sea CO. exchange. Recent work indicates that the productivity and distribution of coccolithophores are sensitive to CO.-related changes in environmental