Abstract The late Paleozoic Ice Age (LPIA) was one of Earth's most important Phanerozoic
climatic events lasting for over 100 Mys. Despite its importance, its history is controversial …

The deep time (pre-Quaternary) glacial record is an important means to understand the
growth, development, and recession of the global cryosphere on very long timescales (106 …

The southwestern margin of South America offers a complete record of the Late Paleozoic
Ice Age (LPIA) that affected the Gondwana supercontinent. The tripartite division of LPIA …

Upper‐flow‐regime bedforms, including upper‐stage‐plane beds, antidunes, chutes‐and‐
pools and cyclic steps, are ubiquitous in glacigenic depositional environments characterized …

Fjords are glacially carved estuaries that profoundly influence ice-sheet stability by draining
and ablating ice. Although abundant on modern high-latitude continental shelves, fjord …

Abstract The Ordovician of North and West Africa comprises three main transgressive–
regressive sequences understood as 'second-order'cycles of 10–15 myr duration. Tide-to …

Sediments deposited by glacial meltwaters (for example, ice‐contact delta deposits) form
permeable packages in the subsurface that can act as reservoirs for both water and …

Glacier and ice sheet mass loss as a result of climate change is driving important coastal
changes in Arctic fjords. Yet limited information exists for Arctic coasts regarding the …

In the eastern part of the Karoo Basin of South Africa, the sedimentary record of the Late
Palaeozoic Ice Age, the Dwyka Group, consists of an up to 200 m thick accumulation of …

Assessment of sediment redistribution by end-Ordovician ice sheets is crucial for the
reconstruction of Lower Paleozoic source-to-sink patterns. Focusing on the ice-distal …