A dynamic climate and ecosystem state during the Paleocene-Eocene Thermal Maximum; inferences from dinoflagellate cyst assemblages on the New Jersey Shelf

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http://www.biogeosciences.net/6/1755/2009/bg-6-1755-2009.pdf
Author(s): Sluijs, Appy; Brinkhuis, Henk
Author Affiliation(s): Primary:
Utrecht University, Institute of Environmental Biology, Palaeoecology, Utrecht, Netherlands
Volume Title: Biogeosciences
Source: Biogeosciences, 6(8), p.1755-1781. Publisher: Copernicus GmbH on behalf of the European Union, Katlenburg-Lindau, International. ISSN: 1726-4170
Note: In English. Published in Biogeosciences Discussion: 20 May 2009, http://www.biogeosciences-discuss.net/6/5163/2009/bgd-6-5163-2009.html; includes supplement, http://www.biogeosciences.net/6/1755/2009/bg-6-1755-2009-supplement.zip; doi:10.5194/bg-6-1755-2009; accessed in May, 2010. 97 refs.; illus., incl. 11 plates, 1 table, sketch map
Summary: Late Paleocene and Early Eocene climates and ecosystems underwent significant change during several transient global warming phases, associated with rapidly increasing atmospheric carbon concentrations, of which the Paleocene-Eocene Thermal Maximum (PETM; ∼55.5 Ma) is best studied. While biotic response to the PETM as a whole (∼170 kyrs) has been relatively well documented, variations during the PETM have been neglected. Here we present organic dinoflagellate cyst (dinocyst) distribution patterns across two stratigraphically expanded PETM sections from the New Jersey Shelf, Bass River and Wilson Lake. Many previously studied sites show a uniform abundance of the thermophilic and presumably heterotrophic taxon Apectodinium that spans the entire carbon isotope excursion (CIE) of the PETM. In contrast, the New Jersey sections show large variations in abundances of many taxa during the PETM, including the new species Florentinia reichartii that we formally propose. We infer paleoecological preferences of taxa that show temporal abundance peaks, both qualitative and absolute quantitative, from empirical as well as statistical information, i.e., principle (PCA) and canonical correspondence analyses (CCA). In the CCAs, we combine the dinocyst data with previously published environmental proxy data from these locations, such as TEX86 paleothermometry, magnetic susceptibility and sedimentary size fraction. The combined information supports previous inferences that sea level rose during the PETM, but also indicates a (regional) increase in fresh-water runoff that started ∼10 kyr after the onset of the CIE, and perhaps precession-paced cycles in sea surface productivity. The highly variable dinocyst assemblages of the PETM contrast with rather stable Upper Paleocene assemblages, which suggests that carbon input caused a dynamic climate state, at least regionally.
Year of Publication: 2009
Research Program: ODP Ocean Drilling Program
Key Words: 09 Paleontology, Paleobotany; 24 Surficial Geology, Quaternary Geology; Apectodinium; Areoligera; Assemblages; Atlantic Coastal Plain; Bass River; C-13/C-12; Carbon; Cenozoic; Continental shelf; Dinoflagellata; Eocene; Eutrophication; Florentinia reichartii; Geologic thermometry; Gloucester County New Jersey; Isotope ratios; Isotopes; Leg 174AX; Lower Eocene; Lycopodium; Lycopsida; Microfossils; New Jersey; New Jersey Shelf; Ocean County New Jersey; Ocean Drilling Program; Paleocene; Paleocene-Eocene Thermal Maximum; Paleoclimatology; Paleoecology; Paleoenvironment; Paleogene; Paleosalinity; Paleotemperature; Palynomorphs; Plantae; Pteridophyta; Sea-level changes; Spiniferites; Stable isotopes; Statistical analysis; Tertiary; United States; Upper Paleocene; Vincentown Formation; Wilson Lake
Coordinates: N393642 N393642 W0742612 W0742612
N393900 N393900 W0750300 W0750300
Record ID: 2010086274
Copyright Information: GeoRef, Copyright 2017 American Geosciences Institute. Reference includes data from Copernicus Gesellschaft, Katlenburg-Lindau, Germany