The role of foraminifera as indicators of the Late Pleistocene–Holocene palaeoclimatic fluctuations on the deltaic environment: The example of Tiber delta succession (Tyrrhenian margin, Italy)

Author:

Di Bella Letizia,Bellotti Piero,Milli Salvatore

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference97 articles.

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2. Holocene climatic instability: a prominent, widespread event 8200 yr ago;Alley;Geology,1997

3. Scaling percentages and distributional patterns of benthic foraminifera with flux rates of organic carbon;Altenbach;Journal of Foraminiferal Research,1999

4. Late Pleistocene-Holocene paleoclimate and related paleoenvironmental changes as recorded by calcareous nannofossils and planktonic foraminifera assemblages in the southern Tyrrhenian sea (Cape Palinuro, Italy);Amore;Marine Micropaleontology,2004

5. Plio-Pleistocene geological evolution of the geothermal area of Tuscany and Lazio;Barberi;Memorie Descrittive della Carta Geologica Italiana,1994

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