NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, He - Ho
(5/17/01)
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TAPHOFACIES ANALYSIS OF UPPER CARBONIFEROUS MICROFOSSILS
(HUGHES CREEK SHALE, EAST-CENTRAL KANSAS)
HEATH, Winfield S., and Roger L. Kaesler, Dept. of Geology, University
of Kansas, Lawrence, KS, USA
Taphofacies analysis has become a crucial tool in paleoenvironmental
analysis, but microfossils have largely been overlooked in this field.
To remedy this, we examined the Hughes Creek Shale Member of the Foraker
Limestone (Upper Carboniferous) of the Midcontinent. We applied Brett
and Baird's (1986) methods of taphofacies analysis to the study of both
macro- and microfossils. Comparing the taphonomy of the ostracodes, fusulinids,
and smaller foraminifera with that of the macroinvertebrates allowed us
to define microtaphofacies that are correlative with those of the macrofossils.
We show that, with some limitations, microfossils lend
themselves readily to taphofacies analysis. For example, reorientation
cannot be considered because of the disruptive methods necessary to disaggregate
shale samples. Interpretation of the biostratinomy of microfossils is
further complicated by such diagenetic effects as chemical alteration
and compaction. However, where macrofossils are absent or destroyed, as
in cuttings from boreholes, microfossils may provide the only means of
analyzing taphofacies.
We assessed fragmentation and disarticulation, both of
which may have been partially introduced during disaggregation of the
shales, as well as corrosion, epibiont activity, and pyritization. All
types of damage except pyritization in the foraminifera were present in
the samples studied. A system of ranks allowed us to compute factors indicating
the extent of taphonomic alteration of the microfossils and to distinguish
between relative amounts of biostratinomy and diagenesis. Results indicate
similarity in taphonomy of foraminifera, ostracodes, and all organic shells
combined; but significant differences occur between the relative amounts
of biostratinomy and diagenesis in each of these groups.
CONODONT CLINES AND PUNCTUATED EVOLUTION AT
PERMIAN SERIES BOUNDARIES
HENDERSON, Charles M., Dept. of Geology and Geophysics, University of
Calgary, Calgary, AB, Canada; and Shilong Mei, Dept. of Geology and Geophysics,
University of Calgary, Calgary, AB, Canada, and China University of Geosciences,
Beijing, China
Recognition of geographic clines in Permian neogondolellids
provides a new context in which to characterize the evolution of Permian
conodonts. During the Kungurian and Guadalupian, a large cusp, low, narrow
and frequently discrete posterior carinal denticles, low and discrete
anterior blade denticles, and usually an elongate platform represent neogondolellids
from higher latitudes such as the Sverdrup Basin. In contrast, a relatively
small cusp, tightly spaced and relatively large posterior denticles, high
and strongly fused anterior blade denticles, and a relatively short platform
characterize neogondolellids from equatorial areas such as South China
and West Texas. Neogondolellids from mid-latitudes such as the Phosphoria
Basin are intermediate in morphology. Late Kungurian populations are represented
by Mesogondolella idahoensis in cool-water faunas and M. siciliensis
in warm-water faunas. Differences in the cusp, carina, and blade should
be recognized at the subspecies level since gradational morphotypes suggest
gene flow across the entire region. A punctuated evolutionary event occurs
at the Kungurian-Roadian boundary with the introduction of the serrated
Jinogondolella nankingensis. A cline develops in the Early Roadian
from Jinogondolella nankingensis nankingensis (Ching) in equatorial
areas to Jinogondolella nankingensis gracilis (Clark and Ethington)
in mid to high latitudes. However, with continued climatic change and
corresponding development of conodont provincialism this gene flow was
cut off and evolution of these subpopulations proceeded along different
paths. A series of Guadalupian Jinogondolella species developed
in equatorial regions by phyletic gradualism. Another punctuated evolutionary
event characterizes the Guadalupian-Lopingian boundary with the evolution
of Clarkina. In the Sverdrup Basin the Jinogondolella lineage
ends quickly because of cooling in northwest Pangea and the evolution
of Mesogondolella proceeds along a very gradualistic path until
the Permian-Triassic boundary when global warming allows an influx of
new neogondolellids.
SAUKIID-DIKELOCEPHALID TRILOBITES AND THEIR
IMPLICATIONS FOR LATE CAMBRIAN PALEOGEOGRAPHIC AND PALEOENVIRONMENTAL
RECONSTRUCTIONS
HENDERSON, Wayne G., and Nigel C. Hughes, Dept. of Earth Sciences, University
of California, Riverside, CA, USA
Genera assigned to the Saukiidae and the Dikelocephalidae
have long been considered closely related. Among the Dikelocephalidae,
a markedly expanded cephalic doublure is synapomorphic for dikelocephalids,
and Saukiidae, as currently defined, is likely paraphyletic. Nevertheless,
the saukiid cranidium has a distinct morphology and, while the Dikelocephalidae
are exclusively Laurentian, trilobites with the saukiid glabellar morphotype
occur globally in equatorial regions. This distribution is particularly
surprising as Cambrian polymerid trilobites are generally considered to
show high degrees of continental endemism, and saukiids are known for
their preference for near shore habitats. Ulrich and Resser (1933) first
described the Saukiidae in detail, erecting 104 species in five genera
from the Upper Mississippi Valley. An additional 25 genera and 200 species
of saukiids have since been described, occurring across equatorial core
and outboard Gondwana, Laurentia, Siberia, and Kazakhstan, and they have
been extensively used for biostratigraphic zonation. Saukiid species and
genera have frequently been described as endemic to these regions even
though there are few, if any, morphological features to distinguish them
from species found on other paleocontinents. Accordingly, there is critical
need to refine species concepts. We are: (1) evaluating character variation
within large collections from single bedding planes to establish the bounds
of intrapopulational variation, and (2) constructing a character matrix
for phylogenetic analysis of all well-preserved saukiids based strictly
on morphological criteria. Such analysis will point to the resolution
of taxonomic relationships within these groups and provide the basis for
evaluating Late Cambrian endemism and biogeographic links.
WITHIN-SPECIES ADAPTIVE RESPONSES TO MID-PLEISTOCENE
CLIMATE CHANGE: ISOTOPE SCLEROCHRONOLOGICAL ANALYSES OF SUBTROPICAL NEOGASTROPODS
OF FLORIDA
HERBERT, Gregory S., Dept. of Geology, University of California, Davis,
CA, USA
A stable isotope sclerochronological analysis was carried
out on Pleistocene fossil and Recent Urosalpinx perrugatus (Conrad),
a predatory gastropod from the west coast of Florida, in order to understand
the underlying developmental basis of evolutionary size decrease in this
species in the context of Pleistocene climate change. Early Pleistocene
shells attain 40 mm in shell length, whereas middle Pleistocene and Recent
shells attain only 25 mm. Isotope profiles were generated for early Pleistocene
(Bermont Fm., 1.61.1 Ma), middle Pleistocene (Fort Thompson Fm.,
0.90.2 Ma), and modern shells. Living populations were also observed
throughout the year to aid in the interpretation of periodicities in isotope
profiles.
The results show that while there is no change in hatching
season, annual growth rates, or season of growth cessation, total duration
of shell growth shifted from two years in Bermont shells to one year in
Fort Thompson and modern shells. The presence of a single size class in
modern populations suggests a one-year life span in post-Bermont fossil
and modern populations. Similar size decreases were found to occur within
other neogastropod species with the same timing suggesting the possibility
of direct adaptation to a common forcing mechanism operating across lineages.
The Bermont/Ft. Thompson boundary coincides with the
mid-Pleistocene climate transition (~0.9 Ma), a period when glacial-interglacial
cycles shifted from 41-kyr to 100-kyr cycles. The much larger ice sheets
formed during the 100-kyr cycles would have resulted in dramatic increases
in the frequency and severity of winter storms reaching the northern Gulf
of Mexico and accompanying increases in juvenile mortality in nearshore
marine organisms. Early maturation as an adaptive response would have
allowed rapid population replacement under these conditions. This study
illustrates the value of targeted sclerochronological analyses of life
history evolution for understanding the biological effects of Pleistocene
climate change.
CONIFER POLLEN CONES FROM THE EARLY TERTIARY
OF BRITISH COLUMBIA, CANADA
HERNÁNDEZ-CASTILLO, Genaro R., and Ruth A. Stockey, Dept. of Biological
Sciences, University of Alberta, Edmonton, AB, Canada
Large number of fossil conifers have been described from
the Upper Cretaceous and Early Tertiary of North America. Most of these
conifer species correspond to taxa within the Cupressaceae/Taxodiaceae.
However, the internal anatomy of cones is only known for a few of these
taxa. Two fossil pollen cones have been collected at the Late Eocene Appian
Way Locality, just south of Shelter Point on the coast of Vancouver Island,
British Columbia. The fossils are permineralized, and were studied using
the cellulose acetate peel technique and Scanning Electron Microscopy.
Cones are attached to stems that bear oppositely arranged leaves with
a single vascular bundle and an adaxial resin canal. The cone axis bears
decussately scale- like leaves that subtend and enclose the microsporophylls.
Microsporophylls are peltate with upturned distal tips and a central resin
canal. Three abaxial pollen sacs are born on each sporophyll. The walls
of pollen sacs are composed of thick rectangular elongated cells, and
contain abundant non-saccate, papillate pollen grains. These cones show
closest similarities to those in the Cupressaceae/Taxodiaceae. Curved
papillae on pollen grains, the opposite arrangement of scale leaves, and
the number of pollen sacs per microsporophyll suggest affinities with
the genus Metasequoia. These cones are associated with numerous
taxodiaceous leaf and twig remains at the locality that show similar anatomical
characters to those of pollen cones, and will be the subject of further
study in the attempt to reconstruct this conifer as a whole plant.
THE FINAL EPISODE OF EARLY CAMBRIAN METAZOAN REEF-BUILDING
IN WESTERN LAURENTIA: HIGH-DIVERSITY ARCHAEOCYATHAN-CALCIMICROBE REEFS
IN THE UPPER HARKLESS FORMATION OF ESMERALDA COUNTY, NEVADA
HICKS, Melissa, and Stephen M. Rowland, University of Nevada, Las Vegas,
NV, USA
Archaeocyathan-calcimicrobe reefs occurred globally in
low-latitude settings in the Early Cambrian. In western Great Basin, Nevadella
Zone (late Atdabanian to early Botomian) reefs are well known in the Campito
and Poleta Formations. Previously unstudied reefs also occur in the overlying
Bonnia-Olenellus Zone in the Harkless Formation. Here, we describe
patch reefs in the upper Harkless Formation that are late Botomian or
early Toyonian in age, approximately coeval with the well-studied reefs
of the Forteau Formation of eastern Canada.
The patch reefs range in size from 1 m long and 0.5 m
high to 15 m long and 1 m high. They were constructed in shallow water
by a consortium of archaeocyaths and calcimicrobes (Renalcis),
and they contain the remains of a diverse assemblage of organisms. Archaeocyaths
comprise an estimated 50% or greater of the reefs by volume, apparently
creating a rigid framework conducive for extensive lateral and vertical
growth. Renalcis is found pervasively within the reefs, acting
as a binding entity that added strength and stability to the archaeocyathan
framework.
A surprising diversity of benthic and nektonic organisms
occur within the framestones and surrounding packstones. Trilobites, which
are the most abundant benthic organisms found, are commonly fragmented
and have micritic envelopes. Echinoderm plates, ostracods, brachiopods,
Salterella, Chancelloria, and (in one locality) corallomorphs
are all found in varying quantities within and surrounding the reefs.
Synsedimentary cementation and early lithification occurred in all reefs.
This early lithification facilitated the formation of cryptic niches,
thereby enhancing the diversity of reef dwellers.
These late Early Cambrian reefs represent the final stage
of metazoan reef-building prior to the resurgence of microbialite reefs
in the Middle and Late Cambrian. Our data suggest that the diversity of
the reef ecosystems was at its Lower Cambrian peak just before metazoan
reefs disappeared for approximately forty million years.
LATE CRETACEOUS LEAF COMPRESSIONS FROM SOUTHEAST
MISSOURI
HILDERBRAND, John, and Bruce L. Stinchcomb, Dept. of Geology, St. Louis
Community College at Florissant Valley, St. Louis, MO
Leaf-bearing Cretaceous clays are exposed in the northern
part of the Gulf Embayment on Crowley's Ridge as well as in a structurally
complex area to the north at Marble Hill, Bollinger County, Missouri.
Angiosperm leaf compressions in brown clay are found near Ardeola Missouri
on Crowley's Ridge which include the puzzling genus Banksia sp.,
as well as other genera which have related species in the overlying Eocene
Wilcox Group. These plants are in the McNairy Formation of Maestrichtian
age and represent some of the youngest angiosperm compressions found in
the Gulf Series. A different flora is found in clays associated with a
graben at Marble Hill, Mo., where representatives of the genus Ficus
sp. and Magnolia sp. are suggestive of the earlier Tuscaloosa flora
of E.W. Berry. Geologists in the 1940s, who discovered Cretaceous clays
in the southeastern Ozarks suggested that some or all of them might be
Lower Cretaceous in age. The angiosperm flora present in the Marble Hill
area would negate against this, as angiosperms are rare in the Lower Cretaceous.
These leaf-bearing clays may correlate with vertebrate bearing clays of
the Chronister Site, seven kilometers to the Northwest. The exact age
of the Chronister Site is unknown, however based upon recently found hadrosaur
material is thought to be Campanian.
EVIDENCE FOR PREDATORY DRILLING IN LATE PALEOZOIC
BRACHIOPODS AND BIVALVE MOLLUSKS FROM WEST TEXAS
HOFFMEISTER, Alan P., Michal Kowalewski, and Richard K. Bambach, Geological
Sciences, Virginia Polytechnic Institute and State University, Blacksburg,
VA, USA; and Tomasz K. Baumiller, Museum of Paleontology, University of
Michigan, Ann Arbor, Michigan, USA
Bored invertebrates have been described from every period
of the Paleozoic. Although many of these borings are non-predatory in
nature, good evidence exists for the parasitic and/or predatory origin
of mid-Paleozoic (especially Devonian) borings in pelmatozoans and brachiopods.
There is, however, little information on the frequency and nature of Late
Paleozoic drill holes. Silicified fossils bulk collected by G.A. Cooper
from Permian strata in the Glass Mountains of West Texas provide an ideal
opportunity to look for evidence of predatory drilling during this interval.
The collections contain numerous drilled brachiopods
and bivalve mollusks. The drill holes are perpendicular to the shell,
smooth sided, often beveled in a manner similar to drill holes produced
by naticid gastropods today, and have other characteristics consistent
with a predatory/parasitic origin. Among 3140 brachiopods examined, 58
specimens contain unquestionable drill holes (frequency of 1.8%) and 15
specimens questionable drill holes (frequency of 2.3%). The 654 bivalve
mollusks examined included 23 specimens with unquestionable drill holes
(frequency of 3.5%) and 5 specimens with questionable drill holes (frequency
of 4.3%). Drilling intensity is significantly higher in bivalves than
in brachiopods (Fisher's exact test, p=0.02). Drilled brachiopods occur
throughout the section (Upper Pennsylvanian-Upper Permian), but drilling
frequencies vary notably through time and among sampled facies.
This study confirms that drilling predators and/or parasites
were present in the Late Paleozoic. However, drilling intensity at that
time rarely exceeded 5%, and thus was much lower than the Late Mesozoic
and Cenozoic intensities that typically exceeded 20%. The Late Paleozoic
intensities are consistent with those for the rest of the Paleozoic and
suggest that the intensity of drilling predation/parasitism in marine
benthic ecosystems remained low throughout the Paleozoic and did not increase
until some time in the Mesozoic.
BODYPLAN OF THE PROBLEMATIC METAZOAN MACHAERIDIA
HÖGSTRÖM, Anette, Dept. of Earth Sciences, University of California,
Riverside, CA, USA
Enigmatic scleritome-bearing metazoans such as the Machaeridia
constitute formidable challenges from several perspectives. All scleritomes
suffer the same preservational problems in that they very easily disarticulate
after the organism dies making isolated sclerites and sclerite fragments
the most common form of preservation and a limiting factor when reconstructing
morphology and anatomy of the organism.
Machaeridian scleritomes range from relatively straightforward
types forming a dorsal cover to complex ones, more or less enveloping
the entire animal. However, all scleritomes are composed of 24 longitudinal
series of calcitic sclerites. The complex scleritome of lepidocoleid machaeridians
closes and opens along the ventral side and also allows the animal to
enroll spirally for protection, suggesting a segmented bodyplan, although
not strictly metameric.
Epimorphic development of the machaeridian scleritome,
with all sclerite segments present initially, is supported by the uniform
appearance of ornamentation and growth lines, and the presence of occasional
growth increments traceable between sclerites in articulated specimens.
This is in contrast to the adding of sclerites through development in
other scleritome-bearing taxa, as seems to be the case in coeloscleritophorans,
but Halkieria does also exhibit shells growing by accretion.
The bodyplan of machaeridians does not agree with the
concept of Ecdysozoa as a clade of moulting animals and thus rules out
possible affinities with the arthropods. However, an inclusion within
the Lophotrochozoa clade does not resolve the problem of machaeridian
affinities to a higher degree, but tentatively places machaeridians as
a stem group to the molluscs or the annelids.
PHYLOGENY OF THE APLODONTIDAE (MAMMALIA:RODENTIA)
AND SOME IMPLICATIONS FOR OLIGO-MIOCENE BIOGEOGRAPHY
HOPKINS, Samantha S.B., Museum of Paleontology and Dept. of Integrative
Biology, University of California, Berkeley, CA, USA
Aplodontid rodents today are represented by only a single
extant species, Aplodontia rufa, but they have a particularly extensive
and diverse fossil record in the late Oligocene and Miocene of northwestern
North America. Extensive studies of North American aplodontids, particularly
those from the John Day basin of Oregon, have indicated relatively rapid
in situ evolution of molar morphology within genera. Less forthcoming
have been intrafamilial relationships between genera, in part because
cladistic methods have not previously been applied to interpreting the
systematics of the group. Here a first attempt at phylogenetic interpretation
is presented, focused around understanding the evolutionary and biogeographic
relationships of a new mid-Miocene aplodontid from Hepburn's Mesa, MT.
The new species differs greatly in both size and cusp morphology from
other material known from the Miocene of North America, which is limited
to derived, hypsodont forms, such as Allomys and Liodontia.
A phylogenetic reconstruction of aplodontid relationships shows that the
Hepburn's Mesa material falls within the Ansomyinae, a group previously
known only from Eurasia. This group is sister to the taxon that includes
the Allomyinae, Meniscomyinae, Aplodontinae, and Mylagaulidae, which are
the groups that took part in the radiation of hypsodont aplodontids in
the late Oligocene and were the most abundant aplodontid clades in the
mid-Miocene. The relationships among aplodontid groups suggest that several
higher taxa, including the Prosciurinae and the Meniscomyinae, may be
paraphyletic. The phylogeny also has implications for the biogeographic
history of aplodontids, as they appear to have immigrated multiple times
between Europe, Asia, and North America in the Oligocene and Miocene.
With the cessation of this immigration in the mid- to late Miocene and
the extirpation of aplodontids from Asia and Europe, aplodontids and mylagaulids
began to decline in diversity, and were reduced to the single extant species
by the late Pleistocene.
CAN ANALYSES OF THE CARBON ISOTOPE RATIOS
OF HORSE TEETH AND BONES BE USED TO PRECISELY RECONSTRUCT THE C3/C4
RATIO OF LOCAL GRASSLANDS?
HOPPE, Kathryn A., and Ronald Amundson, Div. of Ecosystem Sciences, University
of California, Berkeley, CA, USA
Researchers are increasingly using analysis of the carbon
isotope ratios of herbivore teeth and bone collagen to reconstruct paleoecological
conditions. The carbon isotope ratio of grazing herbivores directly reflects
the abundance of C3 vs. C4 grasses in their diet,
and has been used to reconstruct the abundance of C4 grasses
in ancient grasslands. Additionally, since the C3/C4
ratio of local grasses correlates with changes in growing season temperature,
analysis of the carbon isotope values of herbivore teeth and/or bones
may also serve as a proxy for paleoclimatic conditions. However, the precision
of such reconstructions is currently limited because the correlation between
the isotope ratios of modern equids and the C3/C4
ratio of local grasslands has not been quantified. Of particular concern
is the contribution of other C3 plants (e.g., trees, shrubs
and herbs) to the diet, and thus the carbon isotope ratio, of equids.
We quantify this relationship through analyses of the isotope values and
average diets of modern feral horses from grasslands in Oregon (100% C3)
and New Mexico (>95% C4). The carbon isotopes of tooth enamel
and bone collagen are compared with the isotope values of local plants
and microhistological analyses of fecal samples. Analysis of fecal samples
demonstrates that horses from both locations consumed significant amounts
(5% to 25%) of shrubs and/or herbs. The carbon isotope values of Oregon
horses are consistent with a diet of 100% C3 plants. Values
for New Mexico horses suggest that the diets of these horses consisted
of 80% to 100% C4 grasses, with an average of 93%. It therefore
appears that while analyses of the carbon isotope of horse teeth can be
used to identify regions where C4 grasses are present, this
proxy is likely to underestimate the percentage of C4 grasses
in an ecosystem.
THE SPECIES OF AMPHISTEGINA (FORAMINIFERIDA)
IN THE LATE NEOGENE OF THE DOMINICAN REPUBLIC
HOTTINGER, Lukas, Naturhistorisches Museum Basel, Basel, Switzerland
Seven species of the foraminiferal genus Amphistegina
were described from the Late Miocene Cercado and Gurabo for mations of
the Dominican Republic by Bermudez in 1949. They are defined by exterior
characters. Their morphology ranges from very thick, tuberculate shells
with an almost rectangular outline in axial section (A. tuberculata)
to much flattened-lenticular shells (A. guraboensis). A revision
of the taxa must take into account internal characters in order to reveal
the strong dimorphism of generations in this group. The particular preservation
of the material from the Dominican Republic admits splitting techniques,
as used in nummulites, to open the shells in appropriate quantities. The
revised taxa are distributed in the sedimentary sequence with overlapping-echeloned
ranges from thick shells at the bottom to thin shells at the top until
their disappearance from the foraminiferal assemblages. The relay of ranges
in the sedimentary succession is interpreted as reflecting deepening-upward
environmental change during deposition rather than an evolutionary process.
This is supported by the occurrence of the porcelaneous archaiasinids
and soritids at the shallow end of the gradient and by the dominance of
the larger agglutinated forms (Textulariella and consorts) at the
deep end. Similar relations between depth of deposition and shell morphology
are known from similarly diverse Amphistegina communities in the
extant environmental gradient of the Indopacific Ocean.
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