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      Formal subdivision of the Holocene Series/Epoch: a Discussion Paper by a Working Group of INTIMATE (Integration of ice-core, marine and terrestrial records) and the Subcommission on Quaternary Stratigraphy (International Commission on Stratigraphy)

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          A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates

          G Randall Bond (1997)
          Article 0 comments Cited 694 times – based on 0 reviews     Review now
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            Southward migration of the intertropical convergence zone through the Holocene.

            G H Haug, K A Hughen, D M Sigman … (2001)
            Titanium and iron concentration data from the anoxic Cariaco Basin, off the Venezuelan coast, can be used to infer variations in the hydrological cycle over northern South America during the past 14,000 years with subdecadal resolution. Following a dry Younger Dryas, a period of increased precipitation and riverine discharge occurred during the Holocene "thermal maximum." Since approximately 5400 years ago, a trend toward drier conditions is evident from the data, with high-amplitude fluctuations and precipitation minima during the time interval 3800 to 2800 years ago and during the "Little Ice Age." These regional changes in precipitation are best explained by shifts in the mean latitude of the Atlantic Intertropical Convergence Zone (ITCZ), potentially driven by Pacific-based climate variability. The Cariaco Basin record exhibits strong correlations with climate records from distant regions, including the high-latitude Northern Hemisphere, providing evidence for global teleconnections among regional climates.
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              The Holocene Asian monsoon: links to solar changes and North Atlantic climate.

              Yongjin Wang, Hai Cheng, R. Lawrence Edwards … (2005)
              A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years. Although the record broadly follows summer insolation, it is punctuated by eight weak monsoon events lasting approximately 1 to 5 centuries. One correlates with the "8200-year" event, another with the collapse of the Chinese Neolithic culture, and most with North Atlantic ice-rafting events. Cross-correlation of the decadal- to centennial-scale monsoon record with the atmospheric carbon-14 record shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.
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                Author and article information

                Journal
                Title: Journal of Quaternary Science
                Abbreviated Title: J. Quaternary Sci.
                Publisher: Wiley-Blackwell
                ISSN: 02678179
                Publication date Created: October 2012
                Publication date (Print): October 2012
                Volume: 27
                Issue: 7
                Pages: 649-659
                Article
                DOI: 10.1002/jqs.2565
                SO-VID: 796500a9-74f7-4bf7-b4a6-8e374c405c29
                Copyright © © 2012
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                http://doi.wiley.com/10.1002/tdm_license_1.1

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