Across the Pacific; climate evolution in the middle Miocene

Online Access: Get full text
http://meetingorganizer.copernicus.org/EGU2014/EGU2014-790.pdf
Author(s): Fox, Lyndsey; Wade, Bridget; Holbourn, Ann; Leng, Melanie
Author Affiliation(s): Primary:
University of Leeds, Leeds, United Kingdom
Other:
University College London, United Kingdom
Christian-Albrechts-Universität zu Kiel, Germany
NERC Isotope Geosciences Laboratory, United Kingdom
Volume Title: European Geosciences Union general assembly 2014
Source: Geophysical Research Abstracts, Vol.16; European Geosciences Union general assembly 2014, Vienna, Austria, April 27-May 2, 2014. Publisher: Copernicus GmbH on behalf of the European Geosciences Union (EGU), Katlenburg-Lindau, Germany. ISSN: 1029-7006
Note: In English
Summary: We present the first high-resolution (3 kyr) astronomically-tuned record of δ18O and δ13C from planktonic foraminifera for the equatorial Pacific Ocean (16.5-13.5 Myr). Our data provides exciting new information on sea surface temperatures and primary productivity changes at the tropics during the middle Miocene at a resolution not achieved in any previous study, which sheds new light on the middle Miocene climatic transition (MMCT) and associated carbon-isotope excursion. Reliable sea surface temperature estimates are crucial to any reconstruction and modeling of past ocean salinity and density, water column stratification, thermohaline circulation, and ice volume. Despite extensive studies of benthic foraminifera, existing planktonic foraminiferal records of this interval are extremely scarce and of low resolution, with samples representing time intervals of 2 × 105 and 5 × 105 years. Previous studies have been hindered by the absence of biogenic carbonate (e.g., Leg 199). Consequently the impact of global warming and cooling on tropical surface waters and the propagation of orbital cycles in the Earth System are unknown. In 2009 Integrated Ocean Drilling Program Expedition 320/321 recovered lower-middle Miocene sediments with high sedimentation rates (30m/myr), continuous recovery, and orbital cyclicity from the east equatorial Pacific Ocean. At Site U1338 planktonic foraminifera are abundant and diverse in the lower and middle Miocene sediments and exceptionally well preserved. Scanning electron microscope studies revealed open pore spaces, little evidence of calcitic overgrowth on the wall surface and in many cases preserved spines (Fox and Wade, 2013). We compare our data from Site U1338 to Site 1146 in the western equatorial Pacific Ocean, to reconstruct bottom and surface water conditions and changes in ocean dynamics across the equatorial Pacific during this highly complex interval of climate history. [Copyright Author(s) 2014. CC Attribution 3.0 License: https://creativecommons.org/licenses/by/3.0/legalcode]
Year of Publication: 2014
Research Program: IODP Integrated Ocean Drilling Program
ODP Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Cenozoic; Climate change; Cores; East Pacific; Expedition 321; Expeditions 320/321; IODP Site U1338; Integrated Ocean Drilling Program; Leg 184; Marine sediments; Middle Miocene; Miocene; Neogene; North Pacific; Northeast Pacific; Northwest Pacific; ODP Site 1146; Ocean Drilling Program; Pacific Equatorial Age Transect; Pacific Ocean; Paleoclimatology; Sediments; South China Sea; Tertiary; West Pacific
Coordinates: N023028 N023028 W1175811 W1175811
N192724 N192724 E1161622 E1161622
Record ID: 2019066767
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from European Geosciences Union, Munich, Germany