Stable oxygen isotope. Mg/Ca and Temperature record of Caribbean and Pacific sediments, supplement to: Groeneveld, Jeroen; Hathorne, Ed C; Steinke, Stephan; DeBey, Henry; Mackensen, Andreas; Tiedemann, Ralf (2014): Glacial induced closure of the Panamanian Gateway during Marine Isotope Stages (MIS) 95-100 (~2.5 Ma). Earth and Planetary Science Letters, 404, 296-306

• Main Authors: Groeneveld, Jeroen, Hathorne, Ed C, Steinke, Stephan, DeBey, Henry, Mackensen, Andreas, Tiedemann, Ralf
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2014
• Subjects: Center for Marine Environmental Sciences MARUM; Ocean Drilling Program ODP; Andreas; Pacific; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.834677; https://doi.pangaea.de/10.1594/PANGAEA.834677

The final phase of the closure of the Panamanian Gateway and the intensification of Northern Hemisphere Glaciation (NHG) both occurred during the Late Pliocene. Glacial-interglacial (G-IG) variations in sea level might, therefore, have had a significant impact on the remaining connections between th...