Stable carbon and oxygen isotope ratios of Paleogene planktonic foraminifera from the Maud Rise, supplement to: Stott, Lowell D; Kennett, James P; Shackleton, Nicholas J; Corfield, Richard M (1990): The evolution of Antarctic surface waters during the Paleogene: inferences from the stable isotopic composition of planktonic foraminifers, ODP Leg 113. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 849-863

• Main Authors: Stott, Lowell D, Kennett, James P, Shackleton, Nicholas J, Corfield, Richard M
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 1990
• Subjects: Drilling/drill rig; Composite Core; Leg113; Joides Resolution; Ocean Drilling Program ODP; Antarctic; The Antarctic; Weddell Sea; Shackleton; Weddell; Maud Rise; Kennett; Antarc*; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.726370; https://doi.pangaea.de/10.1594/PANGAEA.726370

The oxygen and carbon isotopic composition has been measured for numerous Paleogene planktonic foraminifer species from Maud Rise, Weddell Sea (ODP Sites 689 and 690), the first such results from the Antarctic. The results provide information about large-scale changes in the evolution of temperature...