1-20 OF 579 RESULTS FOR

MIS 5e

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
×Close Modal
Sort by
Journal Article
Journal: GSA Bulletin
Published: 01 July 2011
GSA Bulletin (2011) 123 (7-8): 1275-1287.
... reconstructions through the Holocene up to A.D. 2005, through the Last Interglacial sensu stricto (marine isotope stage or MIS 5e), and a portion of the penultimate interglacial (MIS 7). Chironomid-inferred temperatures are warmest for the early Holocene and MIS 5e, two periods with enhanced Northern Hemisphere...
FIGURES | View All (6)
Image
View looking east from near the lighthouse at Heraion of the <b>MIS</b> <b>5e</b> and (in...
Published: 01 September 2007
Fig. 3.  View looking east from near the lighthouse at Heraion of the MIS 5e and (interpreted) 7a/c terraces and cliffs near the west end of Perachora Peninsula. The locations of Figures 1 and 2 are indicated, plus the mapped MIS 5e shoreline of Leeder et al . (2005) . The area of broken
Image
Ipswichian (<b>MIS</b> <b>5e</b>) beach shingle overlain by chalky colluvium banked again...
Published: 01 May 2007
Fig. 7. Ipswichian (MIS 5e) beach shingle overlain by chalky colluvium banked against the Ipswichian buried cliff, Sewerby (Photo. J.A. Catt).
Journal Article
Journal: Geology
Published: 08 December 2017
Geology (2017) 46 (2): 99-102.
... and questions. Here, for the first time, we use a soil formation model together with a climate model to identify the main factors that control the paleosol formation. A case study has been performed on paleosols in the Chinese Loess Plateau of the last interglacial (Marine Isotope Stage [MIS] 5e...
FIGURES | View All (4)
Journal Article
Journal: Geology
Published: 01 November 2011
Geology (2011) 39 (11): 1015-1018.
...O.E. Romero; G.E.A. Swann; D.A. Hodell; P. Helmke; D. Rey; B. Rubio Abstract The Last Interglacial (LIG), corresponding to Marine Isotope Stage (MIS) 5e, provides a reference of interglacial climate variability in the absence of anthropogenic forcing. Using an expanded section of the LIG gained...
FIGURES
Journal Article
Journal: Geosphere
Published: 01 August 2010
Geosphere (2010) 6 (4): 379-395.
... Pleistocene triggered cyclical sedimentation events in the cave. All the interglacial periods show calcite deposition but with growth phases postdating the warmest events of MIS 11 and MIS 5e. The position of the cave halfway up the side of a glacial trough resulted in very distinctive sediment during...
FIGURES | View All (13)
Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.255.01.05
EISBN: 9781862395039
... On ecological grounds, Rivularia haematites mounds in the Heraion area of western Perachora Peninsula may be interpreted as forming in Lake Corinth during MIS 6; they were subject to rapid uplift and some faulting (to create caves) prior to marine flooding in MIS 5e. Alternatively, evidence from...
FIGURES | View All (9)
Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP398.10
EISBN: 9781862396746
... of 181±6 ka based on the age model for MD04-2822. We briefly review the occurrence of silicic tephra in the North Atlantic region from MIS 7 to MIS 5e inclusive and find potential correlatives to the MD04-2822 MIS 6 ash layer in the Norway Basin and Irminger Sea. The giant piston core MD04-2822...
FIGURES | View All (7)
Journal Article
Journal: Palynology
Published: 01 December 2014
Palynology (2014) 38 (2): 195-206.
... into their response to an abrupt and extensive deterioration in climate. Here we present the results of a new sedimentary sequence from the southern Bekaa Valley, Lebanon, which spans the late Last Interglacial marine isotope stage (MIS) 5e to early MIS 5c of the Last Glacial. High-resolution analyses for pollen...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 January 2016
GSA Bulletin (2016) 128 (1-2): 81-93.
... to regional variations in sea levels. In this study, we compiled the elevations of marine isotope stage (MIS) 5e (ca. 119–129 ka), 5c (ca. 106 ka), and 5a (ca. 84 ka) terraces across the Pacific coast of central North America and compared these regional variations in elevation with model predictions of glacio...
FIGURES | View All (7)
Journal Article
Journal: Geology
Published: 01 June 1998
Geology (1998) 26 (6): 499-502.
... Holocene wet period in southern Arabia extending from some time prior to 9.7 ka and ending at 6.2 ka; (2) demonstrate a second period of wetness closely coinciding with the last interglacial period, marine isotope stage (MIS) 5e; (3) indicate that during MIS 5e, southern Arabia was considerably wetter than...
Journal Article
Published: 01 September 2015
Journal of Sedimentary Research (2015) 85 (9): 1019-1036.
... Expedition 325 Hole M0058A (Hole 58A), recovered 82% of a 40.4 m hole on the upper slope east of Noggin Passage on the central GBR margin near Cairns, Australia. Hole 58A provides a detailed sedimentary record during Termination II (TII), Marine Isotope Stage 6/5e (MIS-6/5e), deglacial transition...
FIGURES | View All (13)
Series: Geological Society, London, Memoirs
Published: 01 January 2013
DOI: 10.1144/M37.6
EISBN: 9781862396371
... , L 3 and U II (in stratigraphic order). They are the ravinement surfaces formed at the onset of MIS 7.3 (F 1 ), MIS 5e (U I ) and MIS 5c interglacial peaks (L 3 ), and the subaerial unconformity formed during the MIS 5a sea-level fall up to the emplacement of Brown Tuffs (U II...
FIGURES | View All (12)
Journal Article
Journal: GSA Bulletin
Published: 01 November 2005
GSA Bulletin (2005) 117 (11-12): 1379-1386.
... 6 to MIS 5E) was a complex multicyclic sequence of paleoenvironments, implying that climates oscillated between high and low effective moisture. MIS 4 (ca. 73−61 ka) was a spring discharge supported wetland complex. During MIS 2 (ca. 20−12 ka) the hydrologic settings were variable, although...
FIGURES | View All (4)
Journal Article
Published: 01 May 2007
Proceedings of the Yorkshire Geological Society (2007) 56 (3): 177-207.
...Fig. 7. Ipswichian (MIS 5e) beach shingle overlain by chalky colluvium banked against the Ipswichian buried cliff, Sewerby (Photo. J.A. Catt). ...
FIGURES | View All (9)
Journal Article
Published: 01 February 2018
Canadian Journal of Earth Sciences (2018) 55 (2): 154-171.
...Brigitte Van Vliet-Lanoë; Jean-Luc Schneider; Águst Guðmundsson; Hervé Guillou; Sébastien Nomade; Gilles Chazot; Céline Liorzou; Solène Guégan Central southern Iceland is one of the main outlets of the Icelandic Ice Sheet where a MIS 5e sedimentary complex, the Rangá Formation, is extensively...
FIGURES | View All (12)
Journal Article
Journal: GSA Bulletin
Published: 01 September 2013
GSA Bulletin (2013) 125 (9-10): 1554-1568.
... from historical leveling and from mapping of the stage 5e Quaternary marine terrace (ca. 120 ka). Average vertical deformation in the Holocene is highest for the shortest studied time period, from ca. A.D. 250 to 600, and it is several times faster than rates for marine oxygen isotope stage (MIS) 5e...
FIGURES | View All (7)
Series: GSA Special Papers
Published: 01 January 2011
DOI: 10.1130/2011.2473(09)
... (marine isotope stage [MIS] 5e). Although sea levels were higher than at present, a review of the stratigraphic and geomorphic data suggests that the peninsula was not detached from the mainland. During the last glacial period (MIS 5d–MIS 2), conditions fluctuated between steppe and tree growth in warmer...
Journal Article
Published: 15 August 2016
Journal of Micropalaeontology (2016) 36 (1): 127-135.
... part of the picture? The facies of the MIS 11 and MIS 9 sediments always seems to indicate a sandy substrate, as does MIS 5e. Unfortunately, we have little of the original sediment from Aveley (there is none left of the original sediment that Robinson studied so extensively), and the brick pit is now...
FIGURES
Journal Article
Published: 01 October 2018
Italian Journal of Geosciences (2018) 137 (3): 349-368.
..., but the bluffs marking the inner edges of marine terraces are not normal fault scarps; thus, they suggested a staircase of 12 marine terraces that formed during different marine highstands during the Pleistocene; the final two (B=MIS 5e, inner edge at 40 m; A=MIS 5a, inner edge at 25 m) were consistent...
FIGURES | View All (15)