Results 71 to 80 of about 1,279 (147)

Connecting Warming Patterns of the Paleo‐Ocean to Our Future

open access: yesAGU Advances, Volume 6, Issue 5, October 2025.
Abstract The evolution of the spatial pattern of ocean surface warming affects global radiative feedback, yet different climate models provide varying estimates of future patterns. Paleoclimate data, especially from past warm periods, can help constrain future equilibrium warming patterns.
Xiaoqing Liu   +4 more
wiley   +1 more source

Sea surface temperature reconstruction based on TEX86 for sediment core TTR12_293G

open access: yes, 2015
Sea surface temperature reconstruction based on TEX86 for sediment core ...
Marta Rodrigo-Gámiz (6958991)   +25 more
core   +1 more source

Unusually low TEX86 values in the transitional zone between Pearl River estuary and coastal South China Sea: Impact of changing archaeal community composition

open access: yes, 2015
TEX86, calculated based on the distribution of isoprenoid glycerol dialkyl glycerol tetraethers (GDGTs), is used worldwide for paleotemperature reconstruction in marine and lacustrine environments. Recently, however, increasing evidence showed that TEX86
Wei, Yuli   +5 more
core   +1 more source

(Tabele S3) TEX86 data of IODP Site 356-U1463

open access: yes, 2018
TEX86 data for Site U1463. TEXH86 is calculated from Hopmans et al. [2000] and BAYSPAR TEX86 temperature estimates are calculated from Schouten et al. [2002].
Castañeda, Isla S   +27 more
core   +1 more source

A TEX86 surface sediment database and extended Bayesian calibration [PDF]

open access: yes, 2015
© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Data 2 (2015): 150029, doi:10.1038/sdata.2015.29.Quantitative estimates of past temperature
Tierney, Jessica E., Tingley, Martin P.
core   +1 more source

TEX86 values and temperature estimation for sediment trap samples

open access: yes, 2006
The newly introduced temperature proxy, the tetraether index of archaeal lipids with 86 carbon atoms (TEX86), is based on the number of cyclopentane moieties in the glycerol dialkyl glycerol tetraether (GDGT) lipids of marine Crenarchaeota.
Stuart G Wakeham (6958055)   +7 more
core   +1 more source

Sea surface temperature reconstruction based on TEX86 for sediment core MD98-2195

open access: yes, 2013
Sea surface temperature reconstruction based on TEX86 for sediment core MD98 ...
Yamamoto, Masanobu   +7 more
core   +1 more source

Sea surface temperature differences (UK'37-TEX86) for sediment core 346-U1425, Japan Sea

open access: yes, 2017
Sea surface temperature differences (UK'37-TEX86) for sediment core 346-U1425, Japan ...
Wittkopp, Frederike   +11 more
core   +1 more source

(Table S2) TEX86 index values and sea surface temperture reconstruction for ODP Site 189-1172

open access: yes, 2009
(Table S2) TEX86 index values and sea surface temperture reconstruction for ODP Site 189 ...
James C Zachos (6958619)   +11 more
core   +1 more source

(Table S1) TEX86 and BIT record from sediment core PBBC-1

open access: yes, 2011
A molecular organic geochemical proxy (TEX86) for sea surface temperature (SST) is compared with a foraminifera-based SST proxy (Mg/Ca) in a decadal-resolution marine sedimentary record spanning the last 1000 years from the Gulf of Mexico.
Flower, Benjamin P   +7 more
core   +1 more source

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