(Table 1) Paleocoordinates of deep-sea drilling sites in Neogene, supplement to: Ivanova, Elena V; Ivanova, Alexandra A (1996): Reconstruction of climatic zonation and features of the surface water circulation in the Indian Ocean in Neogene from planktonic foraminifera. Translated from Okeanologiya, 1996, 36(4), 622-633, Oceanology, 36(4), 586-597

• Main Authors: Ivanova, Elena V, Ivanova, Alexandra A
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 1996
• Subjects: Event label; Latitude of event; Longitude of event; Elevation of event; Age, minimum/young; Age, maximum/old; Paleolatitude; Paleolongitude; Composite Core; Calculated; Leg22; Leg23; Leg24; Leg25; Leg26; Leg27; Leg28; Leg29; Leg115; Leg119; Leg120; Leg122; Glomar Challenger; Joides Resolution; Archive of Ocean Data ARCOD; Indian; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.759496; https://doi.pangaea.de/10.1594/PANGAEA.759496

Reconstruction of climatic zonation and features of surface water circulation in the Indian Ocean for seven selected time intervals is presented based on DSDP/ODP data on distribution of planktonic foraminifera species in Neogene sediments of the Indian Ocean with regard to new palinspastic reference schemes. In Neogene two climatic signs are recognized: at the end of Early Miocene and in Early Pliocene. The equatorial divergence and the monsoon-related Hindustan upwelling presumably existed since Early Miocene, and the Arabian-Somalian upwelling is traced at least since Middle Miocene. In Late Miocene, latitudinal zonation was established over the entire area of the ocean, while in Early-Middle Miocene its northwestern part significantly differed from the northeastern one. : Coordinates have been calculated for moments corresponding to deposits with planktonic foraminiferal fauna.