Benthic foraminifera as indicators of hydrologic and environmental conditions in the Ross Sea (Antarctica). E. Bertoni 1,2* , L. Bertello 1,3 , L. Capotondi 1 , C. Bergami 1 , F. Giglio 1 , M. Ravaioli 1 , C. Rossi 1,3 , and A. Ferretti 2
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Benthic foraminifera as indicators of hydrologic and environmental conditions in the Ross Sea (Antarctica)
E. Bertoni 1,2*, L. Bertello 1,3, L. Capotondi 1, C. Bergami 1, F. Giglio 1, M. Ravaioli 1, C. Rossi 1,3, and A. Ferretti 2
1Institute of Marine Science (ISMAR), National Research Council, Bologna, Italy
2 Università di Modena & Reggio Emilia, Dipartimento Scienze della Terra, Modena, Italy
3 Università di Bologna, Dipartimento Scienze dellaTerra & Geologico Ambientali, Bologna, Italy
In general, the benthicforaminiferaldistributionisrelatedtonumerousphysical, chemical, and biologicalfactorssuchassedimentgrain-size, water temperature and salinity, oxygen and organicmattercontents.
Particularly, Antarcticwaters are characterizedby the unusualfeaturesof a low annualprimaryproductivity in spiteof a largepopulationofconsumers, and high accumulationratesofsilica and organiccarbon (Dunbar & Leventer, 1989; Nelson, 1992).
Moreover, the preservationofcalcareousforaminiferaltests in surface marine sedimentsisdirectlydependentfrom the CaCO3concentration in bottomwaters. The Ross Sea is characterized by a shallow calcium carbonate solution boundary at a depth of 500-550 m (Kennett, 1966; 1968) mostly due to low temperatures (0° to -2°C) and high salinities (34.75 to 35.00 ‰) of the bottom waters.
Knowledge of the distribution of modern population in these areas is an useful tool for interpreting fossil assemblages, thus for reconstructing paleoceanographic history of Antarctica (Violanti, 1996).
This study, present data on benthic foraminiferal assemblages from four box cores collected in different areas of the Ross Sea (Fig. 1) during the 2005 oceanographic cruise in the framework of the Italian Antarctic Research National Programme (PNRA).
Results and discussion
Sedimentlithologiesrangebetweendiamictonto surficial diatomaceous mud, the intermediate levels being glacial-marine sediment. The sedimentary sections include diatomaceous glacial-marine deposit over transitional (proximal grounding zone) glacial-marine sediment (Fig.2).
The study revealed that the Ross Sea contains typical Antarctic foraminifera fauna with the dominance of agglutinated taxa (Fig. 3). Relatively elevated abundances, richness and diversity were common in the northernmost site, where the water column was characterized by relatively warmer intermediate waters and by the presence of the colder High Salinity Shelf Water (HSSW)occupying the deepest part of the basin. Here, the assemblage was dominated by Miliamminaarenaceaandthe more abundant species were Trochamminaquadricamerata and Lagenamminadifflugiformis. In the southernmost site, richness and diversity were low and the most significant species were Trochammina sp., and Reophax sp. Moreover, elevated abundances, richness and diversity were common in the upper portion of the cores which represents the youngest climatic phase characterized by the presence of some calcareous specimens too. This may indicate a deeper Carbonate Compensation Depth, probably due to relatively stable and warmer environmental conditions.
M. arenacea was ubiquitous in all the samples and sites, confirming its tolerance to cold corrosive bottom waters and salinity fluctuations as well as its uniquely high preservation potential..
Results document that diversity of benthic foraminifera, number of specimens and variations in test morphology are related to regional differences in water properties (temperature, salinity, carbonate chemistry).
Changes in foraminiferals distributions and in biogenic silica content (Fig. 4), had lead to the identification of three different intervals, that documents the transition from Ice-shelf to open marine conditions, and that may be corrrelated with the facies succession proposed by Domack (Fig. 3, 5).
Radiocarbon dating are in progress, however a cronological frame, based on Domack et. al. allowed to set the transition from Ice-shelf to open marine conditions (intervals III/II in this study) in the Joides basin, at approximately 11 kyr BP. (Fig. 6).
Materials and Methods
Sedimentssampleswerecollectedusing a box corer, and then sub. All the coreswerescannedformagneticsusceptibility and radiographed, thenopened and decribedforvisualsedimentologicalcharacteristics.
Onehalfwassampledevery 0.5 cm. Biogenicasilicacontentsweredeterminedby the progressive dissolutionmethods (DeMaster, 1981). Quantitative analyses on benthic foraminifera were performed on samples washed through a 63 µm sieve. The sieved samples were subsequently divided by a microsplitter and for each sample micropalaeontological analyses have been performed on the benthic foraminifera assemblage (>125µm). At least 300 specimens of benthic foraminifera were counted and identified.
Depth in core (cm)
Modified by Domack et. al., 1999
Modified by Domack et. al., 1999
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Violanti D., (1996): “Taxonomy and distributionofrecentbenthicforaminifersfrom Terra Nova Bay (Ross Sea, Antarctica), OceanographicCampaign 1987/1988”. Paleontographia Italica 1996; v. 83, PP. 25-71, tavv. 1-10.
S.E.M images of benthic foraminiferal fauna, from the four cores .