Results 301 to 310 of about 267,963 (391)

Phenolic Iron Complexes Protect Glacier Ice Algae (Zygnematophyceae) Against Excessive UV and VIS Irradiation. [PDF]

Environ Microbiol Rep
Procházková L, Mojzeš P, Ráček J, Nedbalová L, Remias D.   +4 more
europepmc   +1 more source

Glaciation of alpine valleys: The glacier – debris-covered glacier – rock glacier continuum

Geomorphology, 2018
R. Anderson, L. Anderson, W. Armstrong, M. Rossi, S. Crump   +4 more
semanticscholar   +1 more source

New age‐estimate data and implications for marine isotope stage 7 and 5e sea levels in Fenland, eastern England

Journal of Quaternary Science, EarlyView.
ABSTRACT Only one last interglacial relative sea‐level indicator point (SLIP) has been recognised for Fenland, eastern England, and the nearest penultimate interglacial SLIP is located on the north Norfolk coast. Such limited information restricts the regional input to, and hence the relevance of, global reconstructions of late Middle and Late ...
H. E. Langford, M. D. Bateman, R. M. Briant, D. J. Horne, K. L. Knudsen, K. E. H. Penkman, L. Wheeler, J. Whittaker   +7 more
wiley   +1 more source

Machine Learning-Based probabilistic prediction of glacial lake formation using erosional and topographic features. [PDF]

Sci Rep
Vashistha A, Dashora A, Shah AA.
europepmc   +1 more source

The local paleoenvironment of Kalavan‐2 based on small‐vertebrate remains and its implications for human‐environment‐dynamics between 60 and 35 ka in the Armenian Highlands

Journal of Quaternary Science, EarlyView.
ABSTRACT Kalavan‐2, a high‐altitude (∼1640 m a.s.l.) open‐air site in Armenia, preserves stratified Middle Paleolithic occupations with a rich small‐vertebrate record. Luminescence dating has placed site formation between ~60 and 45 ka, but without independent chronological control of the microvertebrate accumulation.
Dominik L. Rogall, Monika V. Knul, Hugues‐Alexandre Blain, Boris Gasparyan, Ariel Malinsky‐Buller   +4 more
wiley   +1 more source

Irreversible glacier change and trough water for centuries after overshooting 1.5 °C. [PDF]

Nat Clim Chang
Schuster L, Maussion F, Rounce DR, Ultee L, Schmitt P, Lacroix F, Frölicher TL, Schleussner CF.   +7 more
europepmc   +1 more source

Glaciological, glacier-hydrological and climatological investigations around 66°N, West Greenland

, 1983
O.B Olesen, Jørn-Ole Andreasen
openalex   +2 more sources

Integrating Aegean Last Interglacial faunas into the Mediterranean palaeobiogeographic framework: New evidence from Karpathos (Greece)

Journal of Quaternary Science, EarlyView.
ABSTRACT The Last Interglacial (LIG) or Marine Isotope Stage (MIS) 5e, spanning 129 to 116 kyrs ago, is recognised as one of the warmest periods in the Quaternary, with global sea surface temperatures (SSTs) 1°C–2°C higher than today, sea levels 5–10 m above the current level and biogeographical range expansion of specific tropical species into the ...
Christos Psarras, Danae Thivaiou, Frédéric Quillévéré, Jean‐Jacques Cornée, Pierre Moissette, Mélody Philippon, Jan Fietzke, Delphine Bosch, Michel Condomines, Olivier Bruguier, Efterpi Koskeridou   +10 more
wiley   +1 more source

Relative sea level projections constrained by historical trends at tide gauge sites. [PDF]

Sci Adv
Perrette M, Mengel M.
europepmc   +1 more source

Intensification of the Southern Hemisphere westerly winds during the last deglaciation (18.5–14.0 cal ka BP): Evidence from Pearly Beach wetland on the southern Cape coast of South Africa

Journal of Quaternary Science, EarlyView.
ABSTRACT The southwestern Cape of South Africa experiences a complex and dynamic climate, shaped by the interplay between the temperate Southern Hemisphere westerly winds and the subtropical easterlies. Despite the climatic sensitivity of the region, relatively few studies have examined how conditions have varied since the last deglaciation in response
Marc Humphries, Rachel Mey, Paula Reimer, Lynne J. Quick   +3 more
wiley   +1 more source