PALYNOFLORAL DIVERSITY AND PROVINCIALITY IN THE
LATE TRIASSIC NEWARK SUPERGROUP
FOWELL, S. J., OLSEN, P.E., and KENT, D.V., Lamont-
Doherty Earth Observatory of Columbia University,
Palisades, NY 10964
During the Late Triassic, rift basin lakes of the Newark Supergroup
spanned more than 10° of paleolatitude and straddled a paleoclimatic
boundary. Basins at the southern end of the supergoup were subject
to a humid equatorial climate, whereas the northern basins occupied a
sub-equatorial arid zone. Such variations in paleolatitude and
paleoclimate among tectonically similar basins render the Newark
Supergroup ideal for examining the relationship between paleoclimate
and Triassic palynomorph assemblage composition and diversity.
The cyclostratigraphy and magnetic reversal stratigraphy of
continuous cores from the Late Triassic portion of the Newark basin
has established a rigorous temporal and paleogeographic framework
that permits high-resolution correlation of palynologically productive
units from basins in the United States, Canada, and Morocco.
Correlation of 400 kyr cycles between southern and northern Newark
Supergroup basins allows comparison of palynomorph assemblages
from different paleolatitudes during four time slices: the Carnian and
Norian of the Taylorsville, Newark, and Argana basins; the Rhaetian
of the Culpeper and Newark basins; and the Triassic/Jurassic
boundary of the Culpeper, Newark, Argana, and Fundy basins.
Preliminary results indicate that percentages of monosaccate and
bisaccate genera increased over 7° of paleolatitude from the
Taylorsville basin to the Fundy basin. In addition, the average size of
widely distributed species decreases from south to north, suggesting
that size reduction may be an adaptation for arid environments. The
generic diversity within and between separate basins is currently
being determined in order to assess the significance of variations in
assemblage composition along the paleolatitudinal/paleoclimatic
gradient.
Despite changes in palynofloral composition between the
southern and northern basins, a decline in species diversity is
observed at the Triassic/Jurassic boundary throughout the Newark
Supergroup. This pandemic extinction of Late Triassic species
suggests that the low diversity of early Jurassic palynofloras was the
result of overarching environmental changes that superseded regional
paleoclimatic boundaries.
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