Stable carbon and oxygen isotope ratios of planktonic foraminifera in upper Miocene to Holocene sediments of ODP Leg 105 sites ...

• Main Authors: Aksu, Ali E, Hillaire-Marcel, Claude
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA 1989
• Subjects: Composite Core; Drilling/drill rig; Leg105; Joides Resolution; Ocean Drilling Program ODP; Labrador Sea; Neogloboquadrina pachyderma; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.744963; https://doi.pangaea.de/10.1594/PANGAEA.744963

Oxygen and carbon isotopic compositions of planktonic foraminifers Neogloboquadrina pachyderma and N. atlantica were determined at approximately 150-cm intervals through late Pliocene to Holocene sediments in Hole 647A and late Miocene to Holocene sediments in Hole 646B. The isotopic record shows an overall enrichment of about 4.0 per mil in d18O and 1.0 per mil in d13C from the base to top of Hole 646B. In general, this enrichment probably represents the progressive climatic cooling that started in the middle and late Miocene, continued throughout the Pliocene, and led to the Pleistocene glaciations. The d18O values in sediments from approximately 2.66 to 2.42 Ma show a considerable enrichment (~2.5 per mil) and little change in the d13C values, which probably reflects significant long-term ice storage in the Northern Hemisphere. We interpreted enrichments of ~1.5 per mil in d18O and ~1.0 per mil in d13C at -3.2 Ma, associated with minor ice-rafted material, as substantial cooling of surface waters in the ... : Supplement to: Aksu, Ali E; Hillaire-Marcel, Claude (1989): Upper Miocene to Holocene oxygen and carbon isotopic stratigraphy of sites 646 and 647, Labrador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 689-704 ...