Results 41 to 50 of about 1,279 (147)
Cenozoic Biomarker (TEX86) Temperature Estimates from ODP Hole 198-1209A
This table includes temperatures calculated from organic biomarker (TEX86) measurements performed on Paleocene, Eocene and Oligocene sediment material from Ocean Drilling Program (ODP) Hole 198-1209A, Shatsky ...
Auderset, Alexandra +8 more
core +1 more source
Archaeal Tetraether Lipids as Tracers for Past Marine Environmental Change
Abstract Archaea are single‐celled microorganisms that are abundant in marine environments and play a key role in the carbon and nitrogen cycles. Archaea can biosynthesize a wide variety of isoprenoid membrane lipids, including isoprenoid glycerol dibiphytanyl glycerol tetraethers (isoGDGTs).
Felix J. Elling +39 more
wiley +1 more source
Biomarkers (TEX86) of IODP Hole 356-U1459B
Biomarkers (TEX86) of IODP Hole 356 ...
Benjamin F Petrick (7881512) +5 more
core +1 more source
Abstract The Valanginian positive carbon isotope excursion (Weissert Event, ca. 135 million years ago) documents a major global carbon cycle and climate perturbation. Radioisotopic dating suggests that this event was broadly contemporaneous with an interval of profoundly enhanced volcanic activity during the emplacement of the Paraná–Etendeka Large ...
K. Krishnaswamy +7 more
wiley +1 more source
TEX86' rather than TEX86 was proposed to reconstruct SST for uppermost Paleocene strata of Core 302-4A-32X, as abundances of the glycerol dialkyl glycerol tetraether (GDGT) lipid containing three cyclopentanemoieties (GDGT-3) were unusually high.
Timme H Donders (6970535) +19 more
core +1 more source
Evidence for Limited Atmospheric CO2 Rise at the Miocene Climatic Optimum
Abstract The Miocene Climatic Optimum (MCO; 16.9–14.7 Ma) was a relatively warm period with atmospheric CO2 averaging ∼500 μatm but CO2 change across its onset is poorly documented. We present a record of algal 13C‐fractionation covering the Early to Middle Miocene (∼18.5–15 Ma), with a gap at the MCO onset, from Ocean Drilling Program Site 959 in the ...
Evi Wubben +9 more
wiley +1 more source
This table includes temperatures calculated from organic biomarker (TEX86) measurements performed on middle Miocene sediment material from Ocean Drilling Program (ODP) Hole 189-1171C, South Tasman ...
Auderset, Alexandra +4 more
core +1 more source
The TEX86 paleotemperature proxy
The TEX86 paleothermometer is based upon the distribution of archaeal membrane lipids (“GDGTs”) in marine sediments. GDGTs are ubiquitous, abundant and relatively resistant to degradation; as such, the TEX86 paleothermometer has been used to reconstruct ...
Inglis, Gordon, Tierney, Jessica E.
core +1 more source
UK'37 and TEX86 on suspended matter collected during POSEIDON cruise POS396 off NW Africa
UK'37 and TEX86 on suspended matter collected during POSEIDON cruise POS396 off NW ...
Mollenhauer, Gesine +9 more
core +1 more source
Abstract The Paleocene‐Eocene thermal maximum (PETM, ∼56 Ma) is marked by a massive and rapid rise in atmospheric CO2 and ∼5°C of global warming. It is globally characterized by a negative carbon isotope excursion (CIE), and, at least locally, is preceded by a pre‐onset excursion (POE).
Debra A. Willard +6 more
wiley +1 more source

