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    Dating climatic episodes of the holocene

    The climatic variation during the Lateglacial and Holocene is reflected in the changing lake levels and vegetation, and in the formation of a complex hydrographical network that set the stage for the Medieval Warm Period and the Little Ice Age of the past millennium.

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    In Europe and North America, the Holocene is subdivided into Preboreal, Boreal, Atlantic, Subboreal, and Subatlantic stages of the Blytt–Sernander time scale.Despite this, some questions remain concerning both the chronologies of the transgression–regression phases of the prehistoric Baltic Sea basins and their spatial characteristics.Nevertheless, the long-term change in environmental conditions does provide information about the magnitude of natural climate and environmental variability, both that resulting from external climate drivers and that internally generated.The 'Anthropocene' is not a formally defined geological unit.The Subcommission on Quaternary Stratigraphy quotes Gibbard and van Kolfschoten in Gradstein Ogg and Smith in stating the term 'Recent' as an alternative to Holocene is invalid and should not be used and also observe that the term Flandrian, derived from marine transgression sediments on the Flanders coast of Belgium has been used as a synonym for Holocene by authors who consider the last 10 000 years should have the same stage-status as previous interglacial events and thus be included in the Pleistocene.

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