Abstract

Fossils of marine microorganisms like plank tic order Foraminifera area unit among the cornerstones of palaeoclimatological studies. It’s typically assumed that the proxies derived from their shells represent ocean conditions higher than the placement wherever they were deposited. Planktic order Foraminifera, however, area unit carried by ocean currents and, looking on the life traits of the species, doubtless incorporate distant ocean conditions. Here we tend to use high-resolution ocean models to assess the footprint of Planktic order Foraminifera and validate our technique with proxy analyses from 2 locations. Results show that order Foraminifera, and therefore recorded palaeoclimatic conditions, might originate from areas up to many thousands of kilometres away, reflective associate RI considerably completely different from the core web site. Within the jap equatorial regions and therefore the western boundary current extensions, the offset might reach one.5°C for species living for a month and three.0°C for longer-living species. Oceanic transport therefore seems to be a vital facet within the interpretation of proxy signals.