Matches in Nanopublications for { ?s ?p <https://doi.org/10.1016/j.earscirev.2024.104936> ?g. }
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- Up%20to%202.6%20km%20of%20bedrock%20was%20glacially%20removed%20from%20the%20northern%20Barents%20Shelf%20to%20the%20shelf%20margins%20over%20the%20last%202.74%20million%20years. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20mean%20rate%20of%20glacial%20erosion%20across%20the%20Eurasian%20Arctic%20declines%20over%20the%20Quaternary%2C%20but%20the%20efficacy%20of%20glacial%20erosion%20has%20a%20more%20complex%20timeline. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Initially%2C%20glacial%20erosion%20was%20highly%20effective%20due%20to%20the%20transition%20from%20subaerial%20exposure%20to%20marine%20conditions%20around%202%20Ma. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Erosional%20efficacy%20decreased%20after%202%20Ma%20as%20the%20landscape%20became%20less%20responsive%20to%20successive%20glaciations. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- After%201%20Ma%2C%20erosional%20efficacy%20increased%20as%20a%20dynamic%2C%20marine-based%20ice%20sheet%20expanded%2C%20selectively%20eroding%20large%20outlet%20troughs%20to%20the%20shelf%20edge. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Enhanced%20preferential%20erosion%20opened%20up%20the%20Barents%20Seaway%20at%20approximately%200.69%20Ma%2C%20establishing%20a%20new%20circulation%20pathway%20between%20the%20Atlantic%20and%20Arctic%20Oceans. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- A%20net%20volume%20of%201%2C548%2C180%20km%C2%B3%20of%20sediment%20was%20excavated%20and%20deposited%20on%20the%20continental%20shelf%20edge%20over%20the%2047%20glaciations%20spanning%20the%20last%202.74%20Ma. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20mean%20erosion%20depth%20across%20the%20entire%20glaciated%20area%20of%20the%20Barents%20Shelf%20is%20181%20meters. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20pre-glacial%20topography%20of%20the%20Eurasian%20Arctic%20at%202.74%20Ma%20was%20primarily%20subaerial%2C%20with%20elevations%20exceeding%20500%20meters%20in%20northern%20sectors. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Major%20troughs%20such%20as%20Bear%20Island%2C%20Saint%20Anna%2C%20and%20Storfjorden%20experienced%20headward%20deepening%20and%20expansion%20after%201%20Ma%20due%20to%20selective%20glacial%20erosion. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Isostatic%20uplift%20due%20to%20focused%20glacial%20erosion%20in%20troughs%20elevated%20adjacent%20bank%20areas%2C%20enhancing%20topographic%20relief%20across%20the%20Barents%20Sea. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- A%20revised%20total%20late%20Plio-Pleistocene%20volume%20of%20376%20%C3%97%2010%C2%B3%20km%C2%B3%20for%20the%20Bear%20Island%20trough-mouth%20fan%20is%20estimated%2C%20around%2012%25%20lower%20than%20previous%20estimates. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Erosion%20of%20the%20Barents%20Shelf%20and%20its%20terrestrial%20hinterland%20equated%20to%201%2C548%2C180%20km%C2%B3%20over%20the%20entire%2047%20glacial-interglacial%20cycles%20spanning%20the%20late%20Plio-Pleistocene. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20net%20erosion%20volume%20of%20the%20Barents%20Shelf%20represents%20a%2023%25%20increase%20over%20the%201%2C259%2C000%20km%C2%B3%20volume%20constrained%20within%20off-shelf%20trough%20mouth%20fan%20depocentres. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- A%20maximum%20of%202.59%20km%20of%20bedrock%20was%20eroded%20along%20the%20northern%20margin%20of%20the%20Barents%20Shelf%20between%20Svalbard%20and%20Franz%20Josef%20Land%20during%20the%20late%20Plio-Pleistocene. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Over%201%20km%20of%20bedrock%20was%20eroded%20within%20the%20Bear%20Island%20Trough%20in%20the%20southern%20Barents%20Sea. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Most%20of%20the%20denudation%20of%20the%20southern%20Barents%20Sea%20occurred%20within%20the%20last%201.5%20Ma. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20opening%20of%20the%20Barents%20Seaway%20developed%20after%20~0.94%20Ma%20%28MIS%2025%29%20following%20the%20erosion%20of%20the%20land%20bridge%20connecting%20northern%20Novaya%20Zemlya%20to%20the%20archipelagos%20of%20Franz%20Josef%20Land%20and%20Svalbard. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20Barents%20Seaway%20has%20remained%20fully%20open%20since%20~0.69%20Ma%20%28MIS%2017%29. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20development%20of%20the%20bathymetric%20relief%20of%20the%20Barents%20Shelf%20as%20recognisable%20today%20accelerated%20during%20the%20most%20recent%20shelf-wide%20glaciations%20%3C1%20Ma. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Mean%20erosion%20rates%20show%20a%20general%20decrease%20through%20time%2C%20from%20a%20peak%20of%200.43%20mm%20a%E2%81%BB%C2%B9%20in%20the%20early%20phases%20of%20GI%20to%20%3C0.15%20mm%20a%E2%81%BB%C2%B9%20during%20the%20mid-Pleistocene%20Transition%20and%20the%20most%20recent%20Weichselian%20glacial. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- The%20switch%20to%20more%20intense%2C%20selective%20erosion%20beneath%20large%2C%20fast-flowing%20ice%20streams%20increased%20the%20efficacy%20of%20erosion%20within%20glacial%20troughs. obtainsSupportFrom j.earscirev.2024.104936 assertion.
- Enhanced%20isostatic%20uplift%20of%20trough-adjacent%20bank%20areas%20across%20the%20southern%20Barents%20Sea%20was%20driven%20by%20selective%20erosion%20beneath%20ice%20streams. obtainsSupportFrom j.earscirev.2024.104936 assertion.