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 Ostracod crustaceans, common microfossils in marine and
freshwater sedimentary records, supply evidence of past climatic
conditions via indicator species, transfer function and mutual
climatic range approaches as well as the trace element and stable
isotope geochemistry of their shells. As methods of using ostracods
as Quaternary palaeoclimate proxies have developed, so too has a
critical awareness of their complexities, potential and
limitations. This book combines up-to-date reviews (covering
previous work and summarising the state of the art) with
presentations of new, cutting-edge science (data and
interpretations as well as methodological developments) to form a
major reference work that will constitute a durable bench-mark in
the science of Ostracoda and Quaternary climate change. 
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