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Highlighting the latest research on Actualistic Taphonomy (AT),
this book presents the outcomes of a meeting that took place in
Montevideo, Uruguay, in October 2017. Its respective chapters offer
valuable insights into South American archaeology, invertebrate and
vertebrate fauna, and flora. In recent years, there has been a
surge of new research on AT, as evidenced by numerous papers,
talks, theses, etc. However, there are still very few AT books or
even dedicated journal articles. Reflecting the discipline's
newfound maturity, this book, written by South American authors,
offers a unique resource for academics and students of
Paleontology, Geology, and Biology around the world.
Highlighting the latest research on Actualistic Taphonomy (AT),
this book presents the outcomes of a meeting that took place in
Montevideo, Uruguay, in October 2017. Its respective chapters offer
valuable insights into South American archaeology, invertebrate and
vertebrate fauna, and flora. In recent years, there has been a
surge of new research on AT, as evidenced by numerous papers,
talks, theses, etc. However, there are still very few AT books or
even dedicated journal articles. Reflecting the discipline's
newfound maturity, this book, written by South American authors,
offers a unique resource for academics and students of
Paleontology, Geology, and Biology around the world.
The Quaternary comprises a brief time in the Earth's history, and
apart from a few exceptions, molluscan assemblages recovered from
exposures along the coast of Southwestern South America (Southern
Brazil, Uruguay, Argentina) are essentially the same than those
that inhabit the region today, leading to the assumption that no
important change in the distribution of the faunas since
Pleistocene times has occurred. However, the good taxonomic and
temporal resolution reached in the last years, allowed us to detect
some biogeographic changes, although traditional biogeographic
units remain the same (i.e. Magellanic and Argentinean Provinces).
These modifications involve mainly variations in the taxonomic
composition of the assemblages and in the southern boundaries of
some species distributions (extralimital species), today retracted
northwards. These changes are related to southward shifts of the
warm waters of the Brazilian Current, correlated with global warm
peaks. This phenomenon was more intense in the Late Pleistocene
(MIS 5e) and in the Holocene between ca. 6500-3500 14C yr.
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