RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES5004, doi:10.2205/2018ES000634, 2018
Figure 4. Distribution of CaCO$_3$, N. pachyderma (s) and IRD in the studied core during the last 45,000 years (a), and during the Holocene (b). Heinrich (a) and Bond (b) events with well-known ages are marked by blue bars; cooling events observed in the AI-3359 core are marked by hatched bars; MIS – marine isotope stage.
Citation: Savkina K. E., L. D. Bashirova, E. A. Novichkova (2018), Changes in surface conditions east of the Reykjanes Ridge (North Atlantic) during the Late Pleistocene to Holocene cold events, Russ. J. Earth Sci., 18, ES5004, doi:10.2205/2018ES000634.
Copyright 2018 by the Geophysical Center RAS.
Generated from LaTeX source by ELXpaper, v.1.5 software package.