What status for the Quaternary?

@article{Gibbard2005WhatSF,
  title={What status for the Quaternary?},
  author={Philip L. Gibbard and Alan G. Smith and Jan A. Zalasiewicz and Tiffany L. Barry and David J. Cantrill and Angela L. Coe and John C.W. Cope and Andrew Scott Gale and F. John Gregory and John H Powell and Peter Franklin Rawson and Philip Stone and Colin N. Waters},
  journal={Boreas},
  year={2005},
  volume={34}
}
Gibbard, P. L., Smith, A. G., Zalasiewicz, J. A., Barry, T. L., Cantrill, D., Coe, A. L., Cope, J. C. W., Gale, A. S., Gregory, F. J., Powell, J. H., Rawson, P. F., Stone, P. & Waters, C. N. 2005 (February): What status for the Quaternary?Boreas, Vol. 34, pp. 1–6. Oslo. ISSN 0300–9483. 
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42 Citations
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6
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42 Citations

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The Quaternary is here to stay
The proposals to drop the name Quaternary, to extend the Neogene Period to the present day, and to confirm the base of the Pleistocene at 1.8 Ma are reviewed. It is concluded that there is no…
Defining the Quaternary: Where do we go from here?
In GTS2004, the Quaternary was omitted from the formal hierarchy of the time scale, and designated as an informal climatostratigraphic unit spanning the last ~2.6 Ma of the Neogene System/Period.…
Formal Definition of the Quaternary System/Period and Redefinition of the Pleistocene Series/Epoch
The base of the Quaternary System is formally defined for the first time at the base of the Gelasian Stage as defined by the Global Boundary-Stratotype Section and Point (GSSP) at San Nicola, Sicily,…
The Definition of the Quaternary System/Era and the Pleistocene Series/Epoch
The Quaternary is characterised by the development of widespread glaciations in temperate northern regions, and by associated physical and biotic readjustments. As a chronostratigraphical term it has…
The Quaternary Period
Establishing Quaternary as a Formal International Period/System
Despite being the most widely used unit in field mapping and having the greatest number of active researchers, the interval known as Quaternary is unique among the chronostratigraphic subdivisions of…
Paleoindians and the Younger Dryas in the New England-Maritimes Region
Are we now living in the Anthropocene
The term Anthropocene, proposed and increasingly employed to denote the current interval of anthropogenic global environmental change, may be discussed on stratigraphic grounds. A case can be made…
Neogene and Quaternary coexisting in the geological time scale: The inclusive compromise
Contributions to the history of geomorphology and Quaternary geology: an introduction
This Special Publication deals with various aspects of the histories of geomorphology and Quaternary geology in different parts of the world. Geomorphology is the study of landforms and the processes…
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References

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Proposal to redefine the Quaternary
The following proposal has been circulated, via the Executive of the International Union for Quaternary Research (INQUA), to all INQUA members for discussion. It also appears on the ICS web site…
Defining the Quaternary
Reassessment of the position of the Plio-Pleistocene boundary: Is there a case for lowering it to the Gauss-Matuyama palaeomagnetic reversal?
Definition the Pliocene-Pleistocene Boundary
THE question of defining the Pliocene - Pleistocene boundary has become important in recent years, because the practices of different geologists have varied to such an extent that deposits described…
The deep-sea sediment record and the Pliocene-Pleistocene boundary
The Quaternary System
Pliocene-Pleistocene Boundary in Deep-Sea Sediments
TLDR
The uplifted Pliocene-Pleistocene marine sediments of the Mediterranean region are used to define the beginning of the Pleistocene by the first appearance of Anomalina baltica, a species of benthic Foraminifera tolerant of cool water.
Glacial and Pleistocene geology
STUDENTS of glaciology and of Pleistocene or Quaternary times in all its aspects are all too well aware of the tremendous rate of publication of the results of research activity. Quite outstanding…
Variations in the Earth's Orbit: Pacemaker of the Ice Ages
TLDR
It is concluded that changes in the earth's orbital geometry are the fundamental cause of the succession of Quaternary ice ages and a model of future climate based on the observed orbital-climate relationships, but ignoring anthropogenic effects, predicts that the long-term trend over the next sevem thousand years is toward extensive Northern Hemisphere glaciation.
TOWARDS THE LOWERING OF THE PLIOCENE/PLEISTOCENE BOUNDARY TO THE GAUSS-MATUYAMA REVERSAL
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