Results 41 to 50 of about 1,279 (147)

Cenozoic Biomarker (TEX86) Temperature Estimates from ODP Hole 198-1209A

open access: yes, 2021
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

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 7, July 2026.
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

open access: yes, 2019
Biomarkers (TEX86) of IODP Hole 356 ...
Benjamin F Petrick (7881512)   +5 more
core   +1 more source

Minimal Perturbation of the Global Mercury Cycle by the Paraná–Etendeka Large Igneous Province (PE–LIP) During the Onset of the Valanginian Weissert Event

open access: yesGeochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
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

Branched and isoprenoid tetraether (BIT) index, TEX86 and sea surface temperatures of IODP Hole 302-M0004A

open access: yes, 2010
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

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 6, June 2026.
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

Temperatures from TEX86 measurements performed on middle Miocene sediment material from ODP Hole 189-1171C

open access: yes, 2020
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

open access: yes, 2020
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

open access: yes, 2014
UK'37 and TEX86 on suspended matter collected during POSEIDON cruise POS396 off NW ...
Mollenhauer, Gesine   +9 more
core   +1 more source

Terrestrial Ecosystem Response to Changing Temperature and Seasonality in the Paleocene‐Eocene Thermal Maximum: Shallow Marine Records From the Salisbury Embayment, USA

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 3, March 2026.
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

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