Dinoflagellate cyst population evolution throughout past interglacials: Key features along the Iberian margin and insights from the new IODP Site U1385 (Exp 339)
Abstract
IODP 339 Site U1385 ("Shackleton site", e.g. Hodell et al., 2013a), from the SW Iberian
margin, offers the opportunity to study marine microfossil population dynamics by
comparing several past interglacials and to test natural shifts of species that occurred across
these warm periods, in a subtropical context. Here, more specifically, we present results
obtained for the dinoflagellate cyst (dinocyst) population integrated at a regional scale
thanks to the addition of data from proximal sites from southern Iberian margin. When
possible, observations made using the dinocyst bio-indicator are compared to additional
proxies from the same records in order to test the synchronicity of the marine biota
response. Pollen data available for some of the compiled marine sequences also offer the
opportunity to directly compare marine biota with terrestrial ecosystem responses. This
spatio-temporal compilation reveals that, over the last 800 ka, surface waters around Iberia
were tightly coupled to (rapid) climate changes and were characterised by coherent dinocyst
assemblage patterns, highlighting a permanent connection between Atlantic and
Mediterranean waters as evidenced through a continuous exchange of dinocyst populations.
Some index species well illustrate the evolution of the regional hydrographic context along
time, as for instance Spiniferites and Impagidinium species, together with Lingulodinium
machaerophorum, Bitectatodinium tepikiense and heterotrophic brown cysts. They
constitute key bio-indicators in context of natural environmental shifts at long and short
timescales.
Origin : Files produced by the author(s)