TY - JOUR
T1 - Reorganization of Pacific Deep Waters Linked to Middle Miocene Antarctic Cryosphere Expansion: A Perspective from the South China Sea
AU - Tian, Jun
AU - Shevenell, Amelia E.
AU - Wang, Pinxian
AU - Li, Qianyu
AU - Cheng, Xinrong
PY - 2009/12/1
Y1 - 2009/12/1
N2 - Changes in intermediate and deep ocean circulation likely played a significant role in global carbon cycling and meridional heat/moisture transport during the middle Miocene climate transition (∼ 14 Ma). High-resolution middle Miocene (16–13 Ma) benthic foraminifer stable isotope records from the South China Sea reveal a reorganization of regional bottom waters, which preceded the globally recognized middle Miocene ∼ 1‰ δ 18 O increase (13.8 Ma) by 100,000 years. An observed reversal of the benthic foraminifera δ 13 C gradient between ODP Sites 1146 (2092 m) and 1148 (3294 m; 13.9–13.5 Ma) is interpreted to reflect an increase in the southward flux of low δ 13 C deep (> 2000 m) Pacific Ocean waters (Flower and Kennett, 1993; Shevenell and Kennett, 2004). Large-scale changes in Pacific intermediate and deep ocean circulation, coupled with enhanced global carbon cycling at the end of the Monterey Carbon Isotope excursion, likely acted as internal feedbacks to the Earth's climate system. These feedbacks reduced the sensitivity of Antarctica to lower latitude-derived heat/moisture and facilitated the transition of the Earth's climate system to a new, relatively stable glacial state.
AB - Changes in intermediate and deep ocean circulation likely played a significant role in global carbon cycling and meridional heat/moisture transport during the middle Miocene climate transition (∼ 14 Ma). High-resolution middle Miocene (16–13 Ma) benthic foraminifer stable isotope records from the South China Sea reveal a reorganization of regional bottom waters, which preceded the globally recognized middle Miocene ∼ 1‰ δ 18 O increase (13.8 Ma) by 100,000 years. An observed reversal of the benthic foraminifera δ 13 C gradient between ODP Sites 1146 (2092 m) and 1148 (3294 m; 13.9–13.5 Ma) is interpreted to reflect an increase in the southward flux of low δ 13 C deep (> 2000 m) Pacific Ocean waters (Flower and Kennett, 1993; Shevenell and Kennett, 2004). Large-scale changes in Pacific intermediate and deep ocean circulation, coupled with enhanced global carbon cycling at the end of the Monterey Carbon Isotope excursion, likely acted as internal feedbacks to the Earth's climate system. These feedbacks reduced the sensitivity of Antarctica to lower latitude-derived heat/moisture and facilitated the transition of the Earth's climate system to a new, relatively stable glacial state.
KW - Middle Miocene
KW - Monterey carbon isotope excursion
KW - Oceanic circulation reorganization
KW - Global cooling
UR - https://digitalcommons.usf.edu/msc_facpub/586
UR - https://doi.org/10.1016/j.palaeo.2009.10.019
U2 - 10.1016/j.palaeo.2009.10.019
DO - 10.1016/j.palaeo.2009.10.019
M3 - Article
VL - 284
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
ER -