Brunhes Epoch paleoclimates of Japan and Israel

Fuji, Norio; Horowitz, Aharon

doi:10.1016/0031-0182(89)90133-8

Cited by 16 publications

(7 citation statements)

References 5 publications

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“…At first glance, the observed reduction of winter precipitation in our climate reconstruction based on the micromammal assemblages from Qesem seems to be inconsistent with the results of Horowitz (Fuji and Horowitz, 1989;Horowitz, 1989). However, as discussed above (Fig.…”

contrasting

confidence: 63%

“…The glacial phases here seem to be manifested by periods of somewhat lower temperatures but higher rainfall, some in the summertime, which allows for an increase in the frequency of trees, whereas interglacials were hot and dry causing a reduction of tree stands. Fuji and Horowitz (1989) describe the Levantine vegetation explicitly of MIS 8 as having been very much like today but slightly more humid and with more dense vegetation. Bassinot et al (1994).…”

Section: Discussionmentioning

confidence: 98%

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Palaeoecological and biostratigraphical implications of the microvertebrates of Qesem Cave in Israel

Maul¹,

Bruch

Smith

et al. 2016

Quaternary International

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contrasting

confidence: 63%

Section: Discussionmentioning

confidence: 98%

Palaeoecological and biostratigraphical implications of the microvertebrates of Qesem Cave in Israel

Maul¹,

Bruch

Smith

et al. 2016

Quaternary International

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“…A long record (last 800 kyr) is preserved in the Biwa sequence from Japan [Fuji and Horowitz, 1989]. The Biwa sequence shows that the vegetation succession during the different interglacials was similar to present conditions ( Fig.…”

Section: Introductionmentioning

confidence: 91%

“…Two additional long sequences from the Mediterranean area come from Hula in northern Israel and Amazyabu 1 in southern Israel. In these sequences interglacials correspond to interpluvial periods with a strong influence of the Sahara and therefore few rains originating from the Mediterranean [Fuji and Horowitz, 1989;Horowitz, 1989]. The terrestrial equivalent of MIS 11 was identified in pollen zone QVI.…”

Section: Introductionmentioning

confidence: 97%

The continental record of stage 11: A review

Rousseau

2003

Earth's Climate and Orbital Eccentricity: The Marine Isotope Stage 11 Question

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The review of terrestrial records of marine isotope stage 11 indicates that they are mostly yielded by pollen and loess sequences. They occur in different locali ties around the world and show different time resolution and environmental con ditions. Other records are discussed which correspond to more particular condi tions, i.e., the Lake Baikal deposits, or the terrestrial malacofauna from tufa de posits in Western Europe. If almost all the records indicate moister conditions than present, the temperature estimates vary from similar to the present, to warmer from place to place. Another problem related to the interpretation of ter restrial deposits of stage 11 is the time resolution and the sampling interval of the related deposits that makes correlation with other proxies even more difficult due to the long duration of this interglacial. However, a scenario is proposed to link the different reviewed record based on a general warm climate of MIS 11. 1.

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“…along the worldwide coasts (Steinen et al, 1973;Chappell, 1974;Chappell and Veeh, 1978;Murray-Wallace, 2002;Simms et al, 2009), while the highest sea levels during MIS 3 were estimated to be -15 to -10 m a.s.l. on the West Pacific coasts around Japan and New Guinea (Chappell and Shackleton, 1986;Fuji and Horowitz, 1989;Shi et al, 2001) and to be -10 to -5 m a.s.l. in the Chinese marginal seas (Wang and Wang, 1980;Huang et al, 1986;Shi and Yu, 2003;, respectively.…”

Section: Introductionmentioning

confidence: 99%

Terrestrial-marine sedimentary cycles in the South Yellow Sea, China: implications for paleoenvironmental reconstruction since MIS 5

Yu¹,

Liao²,

Hu³

et al. 2017

Turkish J Earth Sci

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Sedimentary records of the continental shelves since Marine Isotope Stage (MIS) 5 are valuable for paleoenvironmental reconstruction and decipherment of land-sea interactions. Since the 1990s, different perspectives on global glacioclimate magnitudes and the associated evolution of major sedimentary environments during the Late Pleistocene have caused a distinctive understanding of marine transgressions and coastal deposits during MIS 3 and MIS 5. Moreover, the chronology of sediment sequences from this region was primarily determined based on radiocarbon dating, which might be problematic for deposits of 40-50 ka BP or older. In this study, we used both a 150-m-long sedimentary core (YZ07) as a typical record and 12 collected regional boreholes as a synthesis to resolve the issues. On the basis of an age model of accelerator mass spectrometry (AMS) radiocarbon and optically stimulated luminescence (OSL) dating, the sedimentary sequences during the period from MIS 5 up to MIS 1 were documented by Core YZ07 drilled from the western coast of the South Yellow Sea (SYS), and the marine sediments were recognized by the paleontological fossils. The results indicate three terrestrial-marine sedimentary cycles since MIS 5, including the MIS 5, MIS 3, and MIS 1 marine transgressions as well as the MIS 2 and MIS 4 marine regressions in the coastal plain and offshore area of the SYS. Meanwhile, there was a major sedimentary hiatus during MIS 2 and MIS 4 due to strong erosions. Different dating methods on these regional cores, including AMS 14 C and OSL, have confirmed the existence of the MIS 3 marine transgression in the SYS. The intensity of marine transgression and the height of sea levels during MIS 3 and MIS 5 recorded in sediments were dominated by the changes of global climate-driven glaciers and regional tectonic movement.

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Brunhes Epoch paleoclimates of Japan and Israel

Cited by 16 publications

References 5 publications

Palaeoecological and biostratigraphical implications of the microvertebrates of Qesem Cave in Israel

Palaeoecological and biostratigraphical implications of the microvertebrates of Qesem Cave in Israel

The continental record of stage 11: A review

Terrestrial-marine sedimentary cycles in the South Yellow Sea, China: implications for paleoenvironmental reconstruction since MIS 5

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