Euryhaline ecology of early tetrapods revealed by stable isotopes
Ecologia de Euryhalina dos primeiros tetrápodes revelada por isótopos estáveis
Abstract
The
fish-to-tetrapod transition—followed later by
terrestrialization—represented a major step in vertebrate evolution that
gave rise to a successful clade that today contains more than 30,000
tetrapod species. The early tetrapod Ichthyostega was discovered
in 1929 in the Devonian Old Red Sandstone sediments of East Greenland
(dated to approximately 365 million years ago). Since then, our
understanding of the fish-to-tetrapod transition has increased
considerably, owing to the discovery of additional Devonian taxa that
represent early tetrapods or groups evolutionarily close to them.
However, the aquatic environment of early tetrapods and the vertebrate
fauna associated with them has remained elusive and highly debated. Here
we use a multi-stable isotope approach (δ13C, δ18O and δ34S)
to show that some Devonian vertebrates, including early tetrapods, were
euryhaline and inhabited transitional aquatic environments subject to
high-magnitude, rapid changes in salinity, such as estuaries or deltas.
Euryhalinity may have predisposed the early tetrapod clade to be able to
survive Late Devonian biotic crises and then successfully colonize
terrestrial environments.
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