Tracing the signature of various frontal systems in stable isotopes (oxygen and carbon) of the planktonic foraminiferal species Globigerina bulloides in the Southern Ocean (Indian Sector)

• Main Authors: Kumar Chaturvedi, Neloy Khare Subodh
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2012
• Subjects: Foraminifera; Globigerina bulloides; Stable isotopes; Southern Ocean; Frontal systems; Oceanography; GC1-1581; Indian
• Online Access: https://doaj.org/article/826f3acab3d945fbb4ee26d1b1e48b99

Twenty-five surficial sediment samples, collected on board ORV Sagar Kanya during her 199th and 200th cruises along a north-south transect betweenlatitudes 9.69°N and 55.01°S, and longitudes 80°E and 40°E were studied for isotopic variations (values of Δ 18 O and Δ 13 C) of the indicator planktonic species Globigerina bulloides . The results indicate that from latitudes 9.69°N to 15°S both these isotopes (Δ 18 O and Δ 13 C) fluctuated significantly. Between latitudes from around15°S to 30-35°S Δ 18 O values steadily increased, whereas $delta^{13}$C showed a decreasing trend. However, to the south of latitudes 30-35°S, both isotope values showed a similar response with a gradual increase up to latitude 50°S,beyond which $delta^{18}$O continued to increase while $delta^{13}$C declined. The characteristic patterns of the values of both isotopes indicatesthat the signatures of different water masses are associated with various frontal systems and/or water masses across the transect. The signature ofthe Polar Front at around latitude 50^{circ}S shows the specific response of the isotopic values (Δ 18 O and Δ 13 C) of G. bulloides . Such a response beyond 50°S latitude is ascribable to the general decrease in the ambient temperature, resultingin a continuous increase in Δ 18 O values, while Δ 13 C values decrease as a result of reduced photosynthesis in regions approaching higherlatitudes owing to low light penetration. To further corroborate our results, those of many such transects from geographically distinct regions need to bestudied for isotopic variations in the calcareous shells of planktonic foraminiferal species. The results have the potential to be used as a proxy to assess the movement of frontal systems in southern high latitude regions.