Kamikuri, Shin-ichi et al. (2013): Early and middle Eocene radiolarian assemblages in the eastern Equatorial Pacific Ocean (IODP Leg 320 Site U1331); faunal changes and implications for paleoceanography
Leg/Site/Hole:
Related Expeditions:
IODP 320 IODP 320 U1331
Identifier:
ID:
2013-033816
Type:
georefid
ID:
10.1016/j.marmicro.2012.09.004
Type:
doi
Creator:
Name:
Kamikuri, Shin-ichi
Affiliation:
Kochi University, Center for Advanced Marine Core Research, Kochi, Japan
Role:
author
Name:
Moore, Theodore C.
Affiliation:
University of Michigan, United States
Role:
author
Name:
Lyle, Mitchell
Affiliation:
Texas A&M University, United States
Role:
author
Name:
Ogane, Kaoru
Affiliation:
National Museum of Nature and Science, Japan
Role:
author
Name:
Suzuki, Noritoshi
Affiliation:
Tohoku University, Japan
Role:
author
Identification:
Title:
Early and middle Eocene radiolarian assemblages in the eastern Equatorial Pacific Ocean (IODP Leg 320 Site U1331); faunal changes and implications for paleoceanography
Year:
2013
Source:
Marine Micropaleontology
Publisher:
Elsevier, Amsterdam, Netherlands
Volume:
98
Issue:
Pages:
1-13
Abstract:
Quantitative faunal analyses of radiolarians were used to reconstruct paleoceanographic conditions spanning the interval from Zones RP8 (Early Eocene) to RP16 (Middle Eocene) in pelagic sequences recovered at Integrated Ocean Drilling Program (IODP) Site U1331 in the eastern equatorial Pacific Ocean. On the basis of relative abundance data from the low to high latitudes reported in the previous literature, paleoceanographic indices were identified: (1) species indicative of warmer conditions include Stylosphaera coronata coronata, Phormocyrtis embolum, Dendrospyris didiceros, Phormocyrtis cf. proxima, and Thyrsocyrtis triacantha; (2) species indicative of cooler conditions include: the Lophocyrtis aspera group, the Lithocyclia ocellus group, Hexacontium sp. A, Hexacontium sp. B, Thecosphaerella glebulenta, and Lithelius sp. A. Two warming and at least six cooling events in the Early to Middle Eocene were identified from radiolarian assemblage variations. The paleoclimatic trends can be summarized as follows: warming in C23n.2n to C21r ( approximately 51.5-49.0 Ma), and C18n (40.2-39.0 Ma); cooling in C21r (48.5-47.8 Ma), lower C20r (46.2-45.2 Ma), top C20r to C20n (44.0-43.0 Ma), top C20n to C19r (43.0-41.7 Ma), C19n to C18r (41.7-40.2 Ma), and C18n.1n (39.0-38.5 Ma). These cooling events corresponded to the ELi and BLi events, which were identified in benthic foraminiferal delta (super 18) O of the Southern Ocean. In general, radiolarian and opal mass accumulation rates (MARs) in the eastern equatorial Pacific had higher values in cooling conditions during the Middle Eocene. The changes in biological productivity in the eastern equatorial Pacific were associated with cooling of tropical surface water. The change in relative abundance of radiolarians and CaCO (sub 3) content at Site U1331 indicated that Middle Eocene carbonate events (carbonate accumulation events [CAEs]; Lyle et al., 2005) coincided with the cooling events of tropical surface water. At least CAE-2 and CAE-3 were associated with high biological productivity as well as cooling. Abstract Copyright (2013) Elsevier, B.V.
Language:
English
Genre:
Serial
Rights:
URL:
Coverage: Geographic coordinates: North:12.0405 West:-142.0942 East:
-142.0942 South:12.0405
Keywords: Stratigraphy; assemblages; biostratigraphy; biozones; Cenozoic; East Pacific; Eocene; Equatorial Pacific; Expedition 320; Expeditions 320/321; Integrated Ocean Drilling Program; Invertebrata; IODP Site U1331; lithostratigraphy; lower Eocene; microfossils; middle Eocene; morphology; North Pacific; Northeast Pacific; Pacific Ocean; paleo-oceanography; paleoclimatology; paleoecology; paleoenvironment; Paleogene; pelagic environment; Protista; quantitative analysis; Radiolaria; Tertiary;
.