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      The fire, human and climate nexus in the Sydney Basin, eastern Australia

      , ,
      The Holocene
      SAGE Publications

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          Shcal04 Southern Hemisphere Calibration, 0–11.0 Cal Kyr BP

          Recent measurements on dendrochronologically-dated wood from the Southern Hemisphere have shown that there are differences between the structural form of the radiocarbon calibration curves from each hemisphere. Thus, it is desirable, when possible, to use calibration data obtained from secure dendrochronologically-dated wood from the corresponding hemisphere. In this paper, we outline the recent work and point the reader to the internationally recommended data set that should be used for future calibration of Southern Hemisphere 14 C dates.
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            An 15,000-Year Record of El Niño-Driven Alluviation in Southwestern Ecuador

            D. Rodbell (1999)
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              Fire-southern oscillation relations in the southwestern United States.

              Fire scar and tree growth chronologies (1700 to 1905) and fire statistics (since 1905) from Arizona and New Mexico show that small areas burn after wet springs associated with the low phase of the Southern Oscillation (SO), whereas large areas burn after dry springs associated with the high phase of the SO. Through its synergistic influence on spring weather and fuel conditions, climatic variability in the tropical Pacific significantly influences vegetation dynamics in the southwestern United States. Synchrony of fire-free and severe fire years across diverse southwestern forests implies that climate forces fire regimes on a subcontinental scale; it also underscores the importance of exogenous factors in ecosystem dynamics.
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                Author and article information

                Journal
                The Holocene
                The Holocene
                SAGE Publications
                0959-6836
                1477-0911
                July 27 2016
                July 27 2016
                : 17
                : 4
                : 469-480
                Article
                10.1177/0959683607077024
                ce32eaa9-7853-44ee-bd53-8b0449417404
                © 2016
                History

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