
What status for the Quaternary?
Author(s) -
GIBBARD PHILIP L.,
SMITH ALAN G.,
ZALASIEWICZ JAN A.,
BARRY TIFFANY L.,
CANTRILL DAVID,
COE ANGELA L.,
COPE JOHN C. W.,
GALE ANDREW S.,
GREGORY F. JOHN,
POWELL JOHN H.,
RAWSON PETER F.,
STONE PHILIP,
WATERS COLIN N.
Publication year - 2005
Publication title -
boreas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.95
H-Index - 74
eISSN - 1502-3885
pISSN - 0300-9483
DOI - 10.1111/j.1502-3885.2005.tb01000.x
Subject(s) - quaternary , geology , pleistocene , paleontology , period (music) , holocene , archaeology , physical geography , geography , philosophy , aesthetics
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. The status of the Quaternary, long regarded as a geological period effectively coincident with the main climatic deterioration of the current Ice Age, has recently been questioned as a formal stratigraphic unit. We argue here that it should be retained as a formal period of geological time. Furthermore, we consider that its beginning should be placed at the Gauss‐Matuyama magnetic chron boundary at about 2.6 Ma, rather than at its current position at about 1.8 Ma. The Quaternary would be formally subdivided into the Pleistocene and Holocene epochs. The global chronostratigraphical correlation table proposed is enclosed at the back of this issue.