Faunal turnover at the end of the Cretaceous in the North Pacific region: Implications from combined magnetostratigraphy and biostratigraphy of the Maastrichtian Senpohshi Formation in the eastern Hokkaido Island, northern Japan

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 271, Issue 1-2, 2009, Pages 84-95

  Nifuku, Ko ^a   Kodama, Kazuto ^b   Shigeta, Yasunari ^c   Naruse, Hajime ^d  

^a KYOTO UNIVERSITY   (Japan)

^b KOCHI UNIVERSITY   (Japan)

^c DEPARTMENT OF BOTANY   (Japan)

^d CHIBA UNIVERSITY   (Japan)

Author keywords

Inoceramids; Maastrichtian; Magnetostratigraphy; Nemuro Group; North Pacific

Indexed keywords

AGE DETERMINATION; AMMONITE; BIOSTRATIGRAPHY; BIVALVE; COCCOLITH; CRETACEOUS; GEOCHRONOLOGY; GEOMAGNETISM; MAGNETOSTRATIGRAPHY; MASS EXTINCTION; MUDSTONE; NANOFOSSIL; PALEOGENE; PALEONTOLOGY; TURNOVER;

ASIA; BENELUX; EURASIA; EUROPE; FAR EAST; HOKKAIDO; JAPAN; LIMBURG [NETHERLANDS]; MAASTRICHT; NEMURO; NETHERLANDS; PACIFIC OCEAN; PACIFIC OCEAN (NORTH); WESTERN EUROPE;

AMMONOIDEA; BIVALVIA; INOCERAMIDAE; INOCERAMUS; PACHYDISCUS;

EID: 57749169280     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2008.09.012     Document Type: Article

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