Orbitally-paced climate evolution during the middle Miocene Monterey carbon-isotope excursion

One of the most enigmatic features of Cenozoic long-term climate evolution is the long-lasting positive carbon-isotope excursion or Monterey Excursion, which started during a period of global warmth after 16.9 Ma and ended at similar to 13.5 Ma, approximately 400 kyr after major expansion of the Antarctic ice-sheet. We present high-resolution (1-9 kyr) astronomically-tuned climate proxy records in two complete sedimentary successions from the northwestern and southeastern Pacific (ODP Sites 1146 and 1237), which shed new light on the middle Miocene carbon-isotope excursion and associated climatic transition over the interval 17.1-12.7 Ma. We recog,nize three distinct climate phases with different imprints of orbital variations into the climatic signals (1146 and 123 7 delta O-18, delta C-13; 1237 XRT Fe, fraction > 63 pm): (1) climate optimum prior to 14.7 Ma characterized by minimum ice volume and prominent 100 and 400 kyr variability, (2) long-term cooling from 14.7 to 13.9 Ma, principally driven by obliquity and culminating with rapid cryosphere expansion and global cooling at the onset of the last and most pronounced delta C-13 increase, (3) Icehouse mode after 13.9 Ma with distinct 100 kyr variability and improved ventilation of the deep Pacific. The Monterey carbon-isotope excursion (16.9-13.5 Ma) consists overall of nine 400 kyr cycles, which show high coherence with the long eccentricity period. Superposed on these low-frequency oscillations are high-frequency variations (100 kyr), which closely track the amplitude modulation of the short eccentricity period. In contrast to delta C-13, the delta O-18 signal additionally shows significant power in the 41 kyr band, and the 1.2 Myr amplitude modulation of the obliquity cycle is clearly imprinted in the 1146 delta O-18 signal. Our results suggest that eccentricity was a prime pacemaker of middle Miocene climate evolution through the modulation of long-term carbon budgets and that obliquity-paced changes in high-latitude seasonality favored the transition into the Icehouse climate. (c) 2007 Elsevier B.V. All rights reserved.