Results 91 to 100 of about 4,963 (203)

Chemical weathering proxies: An assessment of their robustness to reconstruct Paleozoic climate conditions

Evolving Earth
Several chemical weathering proxies for siliciclastic sedimentary deposits have been proposed over the last fifty years. However, only a few studies have evaluated their robustness for paleoclimate interpretation.
Franciele Agnesa Trentin, Joice Cagliari, Karlos G.D. Kochhann, Tracy Frank   +3 more
doaj   +1 more source

A Global Evaluation of Lithology‐Dependent Marine Sediment Compaction Parameters and Their Uncertainties

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 3, March 2026.
Abstract Tectonic subsidence, sea level, and paleoclimate reconstructions using marine records rely on accurate decompaction of the sediment column. Over time, increased overburden pressure from burial decreases sediment porosity with depth. The porosity‐depth relationship is lithology‐dependent and can be represented by an exponential function ...
Haley Svadlenak, Ross Parnell‐Turner, Margaret Morris   +2 more
wiley   +1 more source

An observation-based causal framework linking Barents–Kara sea ice to European heatwaves

Environmental Research: Climate
European summers have become increasingly dominated by severe and persistent heatwaves (HWs), with major societal and economic consequences. While progress has been made in the last decade in linking Arctic sea ice decline to midlatitude extremes, the ...
P Vaideanu, D R Nichita, L Boboc, B Antonescu, M Ionita   +4 more
doaj   +1 more source

Climate and Tectonic Forcing of Depositional Evolution in the Southern North China Basin Since ∼3 Ma

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 3, March 2026.
Abstract Marginal basins provide sensitive yet incomplete records of climate and tectonic forcing, and the southern North China Basin provides an ideal setting to decode these interactions since the late Pliocene. A 135.6‐m borehole sequence, the XiaoQian (XQ) core, recovered from the Fuyang region, was dated using AMS 14C, OSL, and ESR, supplemented ...
Ting Wang, Yujia Liu, Dianbao Chen, Longjiang Mao, Xiaoqian Deng, Chunhui Zou, Huichuan You, Fangtou Tang, Duowen Mo   +8 more
wiley   +1 more source

Issue Information

The Depositional Record, Volume 12, Issue 2, April 2026.
wiley   +1 more source

Revealing the Internal Structure of Mars‐Analog Glaciers From Drone‐Based Radar Sounding

Journal of Geophysical Research: Planets, Volume 131, Issue 3, March 2026.
Abstract Martian debris‐covered glaciers (DCGs) contain large quantities of water ice beneath a protective layer of rock and dust. Properties of the overlying regolith such as density and depth to ice are critical parameters for guiding in situ resource utilization (ISRU) of water and coring missions targeting potential habitats.
Roberto J. Aguilar, John W. Holt, Michael S. Christoffersen, Tyler M. Meng, Stefano Nerozzi   +4 more
wiley   +1 more source

Variations in Arctic Ocean Dynamics and Hydrography Under 127 ka Last Interglacial Conditions and Future Warming

Paleoceanography and Paleoclimatology, Volume 41, Issue 3, March 2026.
Abstract Using outputs from eight Coupled Model Intercomparison Project Phase 6/Paleoclimate Model Intercomparison Project phase 4 models, we compare the hydrography and surface ocean circulation in the Arctic and sub‐Arctic regions across three climate states: the pre‐industrial (PI; 1850 CE), the Last Interglacial (LIG; 127 ka BP), driven by strong ...
Marie Sicard, Agatha M. de Boer, Helen K. Coxall, Torben Koenigk, Mehdi Pasha Karami, René Gabriel Navarro Labastida, Martin Jakobsson, Matt O’Regan, Flor Vermassen   +8 more
wiley   +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

Paleoceanography 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, Mei Nelissen, Appy Sluijs, Henk Brinkhuis, Tammo Reichgelt, Marci Robinson, Jean M. Self‐Trail   +6 more
wiley   +1 more source

Central European Hydroclimate Since the Younger Dryas Inferred From Vegetation‐Corrected Sedimentary Plant Wax δ2H Values

Paleoceanography and Paleoclimatology, Volume 41, Issue 3, March 2026.
Abstract Plant wax hydrogen isotopes (δ2H) preserved in lake sediments provide valuable insights into past climatic changes. However, lake catchments often experience local shifts in vegetation type that can yield distinct isotopic signatures in the sediments, potentially obscuring hydroclimatic signals.
R. N. Santos, D. B. Nelson, A. Klatt, C. J. Schubert, N. Dubois, C. De Jonge, S. N. Ladd   +6 more
wiley   +1 more source

Quantifying Multi‐Source Sediment Supply in a Tropical Foreland Basin (Oligocene‐Miocene Nyalau Formation, Borneo)

Basin Research, Volume 38, Issue 2, March/April 2026.
Detrital zircon unmixing identifies three sediment sources for the Oligocene–Miocene Nyalau Formation, including a previously unrecognised syn‐depositional component characterised by Oligocene–Miocene volcanic zircons and Neoproterozoic populations absent from established sources.
Ekundayo J. Adepehin, Yi N. Fong, Eduardo Garzanti, Hariri M. Arifin   +3 more
wiley   +1 more source