Post-pleistocene colonisation rather than the contemporary environment has most influenced the current population structure of Scottish Atlantic salmon (Salmo salar). [PDF]
Cowell F, Gaggiotti OE, Cauwelier E.
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This site features visual resources that illustrate the deglaciation of North America after the last glacial maximum. Animations and supporting text demonstrate glacial retreat and the flooding of the Bering Land Bridge between Alaska and Russia.
core
Early Holocene vigorous Black Sea outflow and the onset of sluggish Aegean deep-water convection. [PDF]
Evangelinos D +10 more
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Synchronous mid-Holocene marine and terrestrial deglaciation in the Ross Sea, Antarctica. [PDF]
Parker RL +16 more
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Deglaciation of the Norwegian fjords
Melting glaciers and ice sheets are perhaps the most visible signs of a warming cli- mate. Glaciers are retreating on every continent, ice sheets are shedding icebergs into a warming ocean at an accelerating rate, and the atmosphere melts more ice as tempera- tures rise.
openaire +1 more source
Meeting Review of the Cryospheric Ecosystems Conference, 1-4 September 2025, Poznań, Poland. [PDF]
Skoczeń K +6 more
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Monsoon differences in South Asia and East Asia during the penultimate deglaciation revealed by speleothem oxygen isotopes. [PDF]
Zhao J +7 more
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Antarctic rocky outcrops as microbial diversity and biogeochemical hotspots. [PDF]
Arias-Real R +5 more
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Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf. [PDF]
Pambianco C +16 more
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Redox Dynamics of the Atmosphere and Oceans Induced by the Paleoproterozoic Snowball Earth Events. [PDF]
Harada M, Miura Y, Watanabe Y, Ozaki K.
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