Planktonic foraminiferal ecozones: response of the pelagic environment to palaeoclimatic changes in the eastern Mediterranean Sea

Abstract

A detailed study of the planktonic environment of the eastern Mediterranean Sea has permitted the reconstruction of the climatic history of this part of the basin during the time span from 9.7 to 6.6 Ma. The eastern Mediterranean Sea is confirmed as having a strong sensitivity to the climatic changes that occurred during that timespan. One of the very few complete hemipelagic successions of the Upper Miocene in Mediterranean is found in Gavdos island (SW Crete). Quantitative and qualitative modifications of the planktonic foraminiferal communities observed in Metochia section exhibit a sequence of biological events summarized in 11 successive main time intervals. The bioevents are defined by frequency peaks and/or local (re)-occurrences or (temporary) disappearances of some of the taxa, in association with more or less important fluctuations of the more common species. The planktonic foraminifera show a strong correlation with sea surface temperature variations and with changes in the physical and chemical properties of the upper water column caused by the climatic instability. Two prominent shifts in faunal parameters divide the period recorded in Metochia section into three major time slices that are discussed in chronological order: a cooling trend from 9,7 to 7,6 Ma, a warmer period from 7,6 to 7,2 Ma and then a cooling trend which finishes at the Messinian.

Foraminiferal Analysis Related to Paleoceanographic Changes of Arafura Sea and Surrounding During Holocene

“…The nutrient enrichment at this site during the last 9 ky BP is also Globigerinoides bulloides, Neogloboquadrina dutertrei, Globorotalia menardii, and Pulleniatina obliqueloculata, which are known to be species prefer to live in high nutrient level (e.g. Barmawidjaja et al, 1989;Baohua, 1997;Ding et al, 2006;Drinia et al, 2003;Mohtadi et al, 2009;Sijinkumar et al, 2011;Spooner et al, 2005;Tedesco et al, 2007). High nutrient might be resulted from enhance upwelling that fluently occurred nearby Arafura Sea.…”

“…For example group of Bulimina, Bolivina, and Uvigerina commonly abundant in dysoxic condition, Neogloboquadrina dutertrei, Globigerina bulloides, and Pulleniatina obliqueloculata are abundant in thermocline layer and prefer to live in eutrophic condition, which might be related to upwelling process, in contrast Globigerinoides ruber and Globigerinoides sacculifer will be dominant in mixed layer and thrived in warm and oligotrophic condition (e.g. Baohua et al, 1997;Barmawidjaja et al, 1993;Ding et al, 2006;Drinia et al, 2003). Its large population in marine sediment and its relatively simple and cheap preparation are the superiority of this method.…”