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Cambridge Quaternary, Cambridge » Della Murton
https://www.quaternary.group.cam.ac.uk/people/murton/In the Vale of York, ice extended no further south than the Escrick moraine ridge, attaining its maximum extent between 23.50 and 21.60 ka. ... The dynamics of the eastern sector of the BIIS between 41.00 to 15.80 ka were strongly coupled with movements -
Cambridge Quaternary, Cambridge » Early / Middle Pleistocene…
https://www.quaternary.group.cam.ac.uk/events/landocean/Orbital obliquity at 41 ka cycles which had dominated the earlier part of the Pleistocene was superceded progressively about a million years ago by a 100 ka rhythm of orbital eccentricity, -
Cambridge Quaternary, Cambridge » North West European Rivers
https://www.quaternary.group.cam.ac.uk/research/projects/nweurorivers/cromerian.htmlIndeed the change from the 40 ka to the 100 ka cyclicity appears to be accompanied by an important increase in the intensity of supply of sedimentary detritus and thus a -
Cambridge Quaternary, Cambridge » Quaternary Discussion Group
https://www.quaternary.group.cam.ac.uk/seminars/previous.htmlcover. We found that a gradual removal of terrestrial sediment from the Northern Hemisphere continent by glacial processes is sufficient to explain transition from 40-ka to 100-ka worlds around -
ISSUE 25
https://www.quaternary.group.cam.ac.uk/camqua/25.pdf28 Apr 2003: Orbital obliquity at 41 ka cycles which haddominated the earlier part of the Pleistocene wassuperceded progressively about a million years ago by a100 ka rhythm of climate change and increased-amplitudeclimatic ... The first talk, by Mark Maslin (UCL, -
POSTERSTRAT_v2019-ZAGWIJN-NJG
https://www.quaternary.group.cam.ac.uk/images/hoog2019zagwijninmemoriamnjg.pdf13 Jan 2020: Termination I - 14 ka. Termination IV - 337 ka. Termination V - 424 ka 11. ... 9e. 7e7a. 19. 15a. 103. 63. 9a. 5. 15e. 4. Termination VI - 533 ka. -
Cambridge Quaternary, Cambridge » Kim Cohen
https://www.quaternary.group.cam.ac.uk/people/cohen/21-15 ka BP) can be assessed for a specific moment in time (e.g. ... Timeframes shown: 10,000 - 7,000 - 6,500 - 6,000 - 5,500 ka BP. -
Cambridge Quaternary, Cambridge » Events
https://www.quaternary.group.cam.ac.uk/events/gibbardretirement/explaining the strong 100,000-year ice age cycles at the end of the Middle Pleistocene transition (700 ka) and, c) the interactions between millennial and orbital climate variability as the ... 220 ka. The sediment profile is marked by alternations of -
Cambridge Quaternary, Cambridge » Becky Briant
https://www.quaternary.group.cam.ac.uk/people/briant/thesis.htmlfills. The Nene and Welland rivers were both active throughout the Devensian Stage, with lower-energy deposition in the Early Devensian Substage (50-115 ka) than in the later Middle and ... An significant hiatus in sedimentation during the Late Devensian -
Cambridge Quaternary, Cambridge » Controls on interglacial…
https://www.quaternary.group.cam.ac.uk/research/projects/interglacialrivers/analogue.htmlIn contrast, a somewhat different regime seems to have occurred during the warm phase of the Late-glacial (Windermere) Interstadial (13-11 Ka). -
ISSUE 12
https://www.quaternary.group.cam.ac.uk/camqua/12.pdf24 Apr 2003: the late survival ofNeanderthals in other parts of southern Iberia, for examplethe skeletal remains dated to perhaps 27 ka (U-series) fromthe cave of Zafarraya. ... 45 ka, with the earliest-dated Upper Palaeolithic (pre-. sumed to be associated with -
Cambridge Quaternary, Cambridge » Staff and students
https://www.quaternary.group.cam.ac.uk/people/leszczynska/There, the substantial London Clay bedrock ridge (Danbury-Tiptree ridge) formed a major, insurmountable barrier to the Anglian ice sheet (Middle Pleistocene, Anglian Stage, 480-420 ka BP) at its southern -
European rivers evolution project EREP 2005 Record of a ...
https://www.quaternary.group.cam.ac.uk/research/projects/eurorivers/erep2005.doc28 Apr 2005: 14-15 ka or 'Younger loess' times) to be compiled by LM. -
issue 32
https://www.quaternary.group.cam.ac.uk/camqua/32.pdf19 Oct 2005: Holocene (6-8 ka BP) glaciers were even smaller than they are now (after the 2003 extreme summer). -
Cambridge Quaternary, Cambridge » Phil Gibbard
https://www.quaternary.group.cam.ac.uk/people/gibbard/2019. 'Missing Glaciations' of the Middle Pleistocene: examining controls on global glacier extent during 100 ka glacial cycles. ... Hughes, P., & Gibbard, P. 2018. Global glacier dynamics during 100 ka Pleistocene glacial cycles. -
issue 33
https://www.quaternary.group.cam.ac.uk/camqua/issue%2033%20FINAL.pdf20 Jan 2006: Low-amplitude 41 ka climate cycles, dominating the earlier part of the Pleistocene, gave way progressively to a 100 ka rhythm of increased amplitude that characterizes our present glacial-interglacial world. -
Document2
https://www.quaternary.group.cam.ac.uk/camqua/Camqua34.pdf4 May 2006: Echets, near Lyon, which span the last 140 ka. -
ISSUE 20
https://www.quaternary.group.cam.ac.uk/camqua/20.pdf24 Apr 2003: Lake Malawi, for example, has already provideda 25 ka record, and plans are afoot for a much deeperborehole which may go back to 1 Ma.
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