Formal Subdivision of the Holocene Series/Epoch : A Summary

The Holocene Series/Epoch is the most recent series/epoch in the geological timescale, spanning the interval from 11,700 yr to the present day. Together with the subadjacent Pleistocene, it comprises the Quaternary System/Period. The Holocene record contains diverse geomorphological, biological, cli...

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Bibliographic Details
Published in:Journal of the Geological Society of India
Main Authors: Walker, Mike, Gibbard, Phil, Head, Martin J., Berkelhammer, Max, Björck, Svante, Cheng, Hai, Cwynar, Les C., Fisher, David, Gkinis, Vasilios, Long, Antony, Lowe, John, Newnham, Rewi, Rasmussen, Sune Olander, Weiss, Harvey
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of India 2019
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Online Access:https://lup.lub.lu.se/record/8509fbe6-fb4a-484a-b7ea-a59ef7e5dd22
https://doi.org/10.1007/s12594-019-1141-9
Description
Summary:The Holocene Series/Epoch is the most recent series/epoch in the geological timescale, spanning the interval from 11,700 yr to the present day. Together with the subadjacent Pleistocene, it comprises the Quaternary System/Period. The Holocene record contains diverse geomorphological, biological, climatological and archaeological evidence, within sequences that are often continuous and extremely well-preserved at decadal, annual and even seasonal resolution. As a consequence, the Holocene is perhaps the most intensively-studied series/epoch within the entire Geological Time Scale. Yet until recently little attention had been paid to a formal subdivision of the Holocene. Here we describe an initiative by the Subcommission on Quaternary Stratigraphy (SQS) of the International Commission on Stratigraphy (ICS) to develop a formal stratigraphical subdivision of the Holocene, with three new stages/ages, two underpinned by Global Boundary Stratotype Sections and Points (GSSPs in an ice core, and a third in a speleothem. These stages/ages are defined together with their equivalent subseries/subepochs. The new stages/ages are the Greenlandian with its GSSP in the Greenland NGRIP2 ice core and dated at 11,700 yr b2k (before 2000 CE); the Northgrippian with its GSSP in the Greenland NGRIP1 ice core and dated to 8236 yr b2k; and the Meghalayan, with its GSSP in a speleothem from Mawmluh Cave, northeastern India, with a date of 4250 yr b2k. This subdivision was formally ratified by the Executive Committee of the International Union of Geological Sciences (IUGS) on 14 th June 2018.