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Titel Do biosiliceous laminated sediments reveal sea ice seasonality in the middle Eocene Arctic Ocean?
VerfasserIn C. E. Stickley, N. Koc, R. B. Pearce, A. E. S. Kemp
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250020412
 
Zusammenfassung
We present initial microfabric analyses of finely laminated middle Eocene biosiliceous sediments from the IODP Expedition 302 “ACEX” cores (central Arctic, Lomonosov Ridge). Backscattered electron imagery (BSEI) of polished thin sections and scanning electron microscope secondary electron imagery (SEI) of lamina-parallel fracture surfaces are used to analyse the laminations in 2 short intervals dated at approximately 46 Ma. Our data offer insight into the cryospheric history of the central Arctic from a siliceous microfossil perspective during a significant phase in Cenozoic climate evolution—the start of the transition from a greenhouse to an icehouse world. Importantly, the BSEI technique offers the detail of information which can not be achieved by bulk sediment analysis. These organic-rich sediments, deposited under an anoxic benthic environment, are also rich in heavily silicified endemic marine to brackish (diatoms, ebridians, silicoflagellates) and in situ freshwater (chrysophyte cysts) siliceous microfossils. They also contain the weakly silicified needle-like diatom Synedropsis spp., an indicator of sea ice and the world’s oldest known fossil record of sea ice dwelling diatoms (Stickley et al., in press; Stickley and Koc, Session CL33 this conference). Their presence highlights an exceptional preservational environment along the Lomonosov Ridge at this time. Synedropsis spp. show the Arctic Ocean supported sea ice-based life from 47 Ma, yet episodes of melting must have occurred to allow their preservation in the sediments. Initial investigations indicate Synedropsis spp. form mono-specific laminations or elongate lenses of, on average, 25