%0 Journal Article
%A Fernández López, Sixto Rafael
%A Sha, Jingeng
%T Invertebrate Palaeontology and Sequence Stratigraphy:complementary methods and evidence to explain the geologicalrecord
%D 2013
%@ 0254-055X
%U https://hdl.handle.net/20.500.14352/33452
%X The fossil record and the stratigraphic record are two components of the geological record different in nature, and theycan be separately interpreted and tested in many cases of Invertebrate Palaeontology. Abundance, diversity and stratigraphicpersistence are outstanding features of the fossil invertebrates. Therefore, the complementarity (as the capacity of twocontrasted theories together to explain a body of phenomena, although each separately accounts for only some aspects) or theconsilience (as the fact or condition of being inferred from different phenomena) between Palaeontology and SequenceStratigraphy through the study of fossil invertebrates is specially useful for the interpretation of the geological record and thepalaeoenvironmental changes.
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