1999
DOI: 10.1080/00288306.1999.9514852
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Belemnite biostratigraphy of the New Zealand Late Jurassic Mangaoran (Early Puaroan) Substage and the Puaroan Stage revisited

Abstract: Challinor, currently used to define the base of the Puaroan Stage, is a composite taxon some members of which are here re-identified as H. arkelli and H. mangaoraensis. The remainder are re-described as Hibolithes sp A. Its morphology and stratigraphic range are poorly known and the species is unsuitable as a stage boundary marker. Hibolithes arkelli regularly appears near the base of the Puaroan Stage as presently defined and a formal re-definition based on that taxon is proposed. Although this alters the fau… Show more

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Cited by 9 publications
(31 citation statements)
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“…The base of the Puaroan Stage and of the Mangaoran Substage is now recognised by the first appearance of Hibolithes arkelli Stevens (Challinor 1999), although the original position of the base of the stage remains unaltered. The indicator fossil of the Late Puaroan (Mangaoran) Substage {Belemnopsis aucklandica) remains unchanged, although the reinterpretation of a single belemnite specimen has altered the extent of the Waikatoan type section (see below).…”
Section: Introductionmentioning
confidence: 99%
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“…The base of the Puaroan Stage and of the Mangaoran Substage is now recognised by the first appearance of Hibolithes arkelli Stevens (Challinor 1999), although the original position of the base of the stage remains unaltered. The indicator fossil of the Late Puaroan (Mangaoran) Substage {Belemnopsis aucklandica) remains unchanged, although the reinterpretation of a single belemnite specimen has altered the extent of the Waikatoan type section (see below).…”
Section: Introductionmentioning
confidence: 99%
“…Fossils of restricted Puaroan age are known from above those of Ohauan age on Okahu Stream (Challinor 1974) and a few more belemnites have since become available. More importantly, studies of the ammonites (Stevens 1997) and belemnites (Challinor 1996(Challinor , 1999 have been published. These allow a more confident assessment of the fossil succession, age determinations, and lithological correlations.…”
Section: Introductionmentioning
confidence: 99%
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