Dienerian (Early Triassic) ammonoids from the Candelaria Hills (Nevada, USA) and their significance for palaeobiogeography and palaeoceanography
A well-preserved ammonoid fauna of Early Dienerian age has long been known from the lower portion of the Candelaria Formation in the old Candelaria silver mining district in Mineral and Esmeralda Counties, Nevada, but for a number of reasons, this fauna has never been studied in detail nor illustrat...
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Veröffentlicht in: | Swiss Journal of geosciences 2011-05, Vol.104 (1), p.161-181 |
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Zusammenfassung: | A well-preserved ammonoid fauna of Early Dienerian age has long been known from the lower portion of the Candelaria Formation in the old Candelaria silver mining district in Mineral and Esmeralda Counties, Nevada, but for a number of reasons, this fauna has never been studied in detail nor illustrated. Previous authors assigned this ammonoid fauna to the Early Dienerian
Proptychites candidus
Zone of Canada. In reality, it more closely resembles the Tethyan faunas than the higher palaeolatitude Canadian faunas, thus indicating the presence of some degree of equatorial faunal exchange between opposite sides of the Panthalassic Ocean during Early Dienerian time. It also indicates the onset of a provincialism, which contrasts with the cosmopolitan Griesbachian faunas. A rigorous taxonomic analysis of the Candelaria fauna allows us to differentiate the following ten species, which include two new species and one new genus (
Mullericeras
nov. gen.) belonging to the new family Mullericeratidae:
Ambites lilangensis
(K
rafft
, 1909),
Ambites
aff.
radiatus
(B
rühwiler
, B
rayard
, B
ucher
and
G
uodun
,
2008
),
Ussuridiscus
sp. indet., “
Koninckites
” aff.
kraffti
Spath,
1934
,
Mullericeras spitiense
(K
rafft
, 1909),
Mullericeras
fergusoni
nov. sp.,
Mullericeras
sp. indet.,
Proptychites haydeni
(K
rafft
, 1909),
Proptychites pagei
nov. sp.,
Vavilovites
sp. indet. and
Parahedenstroemia kiparisovae
S
higeta
and
Z
akharov
,
2009
. This Early Dienerian fauna correlates with the
Ambites
fauna known from the base of the Ceratite Marls in the Salt Range and from the base of the “
Meekoceras
” beds in Spiti (northern Gondwanian margin). The fauna also permits the precise dating of a shelfal anoxic episode on the equatorial North American margin. This anoxic event correlates in time with similar palaeoceanographic changes in the southern Tethys, which indicates that the Early Triassic biotic recovery was at least partly shaped by such discrete, short events rather than by pervasive and lingering adverse environmental conditions. |
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ISSN: | 1661-8726 1661-8734 |
DOI: | 10.1007/s00015-011-0055-3 |