NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Br - Bu
(5/17/01)
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| Brewster-Wingard | Brochu
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G | Bush | Butts-Matheson
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GRAPHIC DISPLAY OF THE UPPER DEVONIAN BIOSTRATIGRAPHY
IN THE CENTRAL-SOUTHERN APPALACHIAN BASIN
BRAME, Roderic I., Dept. of Geological Sciences, Wright State University,
Dayton, OH, USA
24,000 macrofossils were collected from Upper Devonian
nearshore clastic marine sediments in the Valley and Ridge Province of
the Central-Southern Appalachian basin in Virginia. One hundred fifty
taxa were identified and cataloged. Taxa include: brachiopods (83), bivalves
(39), gastropods (16), cephalopods, tentaculitids, echinoderms, and arthropods.
Collections were made at eight of the most complete sections that could
be found in the region. The field data were then converted into an electronic
format that can be easily followed in future studies. The biostratigraphic
data from each section was combined to produce a composite standard reference
section. The standard reference section and additional data are displayed
on an Excel spreadsheet. The spreadsheet contains the biostratigraphic
elevation of each sample, the range of each taxon, the total number of
individuals of each taxon for each elevation, and the total number of
individuals of all the taxa for each elevation. Sixteen local biozones
were chosen based on first occurrences except for zones with significant
numbers of last occurrences. The graph offers a spectacular high resolution
and highly detailed view of the Frasnian/Famennian extinction event. The
graph shows two distinctive events just before the Frasnian/Famennian
boundary that I believe are equivalent to the timing of the Kellwasser
events recognized in Germany by E. Schindler (1993). 50% of the brachiopods
go extinct during the two events while the bivalves do not seem to be
affected. This data will be used to measure biodiversity, analyze the
Frasnian/Famennian extinction, develop a sequence stratigraphic model
for the Central-Southern Appalachian basin, and to develop a more regional
biostratigraphic reference section.
ENVIRONMENTAL MICROPALEONTOLOGY REVISED: CHEMICO-ECOLOGICAL
APPROACH
BRESLER, Vladimir, Institute for Nature Conservation Research, Dept.
of Zoology, Tel Aviv University, Israel; and Valentina Yanko-Hombach,
Avalon Institute of Applied Science, Winnipeg, MB, Canada
Micropaleontology discovers and describes micro- and
meioorganisms of different ages. To revive these microfossils, i.e., to
reconstruct the interaction between different species and their environment
(environmental micropaleontology), the chemical-ecological approach was
used. The experimental and field studies of eastern Mediterranean foraminifera
were focused on the interaction of foraminifera with xenobiotics and ability
of foraminifera to protect themselves against xenobiotics using various
defense mechanisms (Bresler and Yanko, 1995; Bresler and Yanko-Hombach,
2000). This approach was based on the assumption that if anti-xenobiotic
defense mechanisms fail to protect the organisms, populations, or ecosystems,
the effect of xenobiotics would be shown by damage to various levels of
biological structures of organisms, from molecular to ecosystems. Thus,
the investigation of anti-xenobiotic defense mechanisms of foraminifera
reflects the adaptation of studied species to their environment. Special
devices together with molecular, biophysical, cytophysiological, biochemical
and morphological vital microfluorometrical methods were used. This enabled
us to evaluate the health of foraminifera and to perform early warning
monitoring, environmental risk assessment and a prognostication of the
studied area.
Numerous foraminiferal defense systems are similar to
those of multicellular organisms. This reflects the ancient origin and
evolutionary importance of foraminiferal defense mechanisms, which integrated
specimens and species in ecosystems and determines their structure and
stability. At least one of these defense mechanisms (xenobiotic deposition
into foraminiferal test) can be examined in fossils. Thus, a further comparative
study of anti-xenobiotic defense mechanisms in modern living microorganisms
against the main xenobiotics in these environments may be used as reliable
tool for the chemical-ecological analysis of fossils and further development
of environmental micropaleontology.
APPLICATION OF MOLLUSCAN PALEOECOLOGY TO THE
EVERGLADES RESTORATION PROJECT: DECADAL TO CENTENNIAL SCALE CHANGE IN
FLORIDA BAY
BREWSTER-WINGARD, G. Lynn, U.S. Geological Survey, Reston, VA, USA
Molluscan assemblages from shallow sediment cores taken
in Florida Bay, Everglades National Park, have provided historical data
on salinity, sub-aquatic vegetation, water quality, and other environmental
parameters. The historical perspective provided by traditional paleoecologic
techniques is essential to restoration efforts in endangered ecosystems.
The south Florida ecosystem has been profoundly affected during the last
century by construction that disrupted natural water flow patterns, by
increased demands on water from a booming population, and by an economy
strongly dependent on agriculture and tourism. Paleoecologic data are
used to delineate the natural range of variation that occurred within
the system prior to significant human alteration. These data can be contrasted
with changes that have occurred since the system has been altered to provide
land managers with realistic success criteria for restoration.
Molluscan data indicate that significant changes occurred
in the latter half of the 20th century in Florida Bay. Brachidontes
exustus, a euryhaline mussel tolerant of low water quality and increased
salinity fluctuations, constitutes greater than 80% of the molluscan assemblage
in the upper portions of six cores. Corresponding decreases in molluscan
abundance and faunal richness also have occurred during the last forty
years. These findings indicate a system under stress. Furthermore, the
molluscan assemblages indicate increasing salinities throughout the 20th
century in the northern transition zone of Florida Bay near the freshwater
outflow. The molluscan epiphytal species indicate that subaquatic vegetation
has varied over the last two centuries. Patterns of change leading up
to the 1987 seagrass die-off are repeated downcore, implying that die-offs
have occurred prior to any significant human influence. In addition, the
molluscan epiphytes in cores from isolated basins show similar patterns
of change, which indicates common factors are affecting the faunas and,
presumably, the vegetation they live on.
THE IMPACT OF FOSSIL CALIBRATION CHOICE IN
MOLECULAR DIVERGENCE ESTIMATION
BROCHU, Christopher A., Dept. of Geoscience, University of Iowa, Iowa
City, IA, USA
Recent comparisons of crocodylian fossil appearances
and sequence data confirm recent suspicions that using a single divergence
to calibrate a groupwide clock can be dangerous. Rate estimates for mitochondrial
genes vary within an order of magnitude depending on the species-pair
comparison used, with comparisons from more recently diverged species
uniformly suggesting significantly higher rates of evolution and, when
used to calibrate a clock, more ancient divergence time estimates throughout
the group. Multiple hits per site will increase with time, causing an
apparent rate slowdown when older divergences are used, and for the same
species pair, the divergence time estimate can vary over 150 million years
depending on whether fast or slow rates are used. Likelihood corrections
to the data reduce the differences between comparisons, but do not remove
them, and some unlikely divergence time estimatessometimes predating first
occurrences in the fossil recordcan still result from some calibrations.
There are problems when alligatorid comparisons are used as calibrations,
regardless of how old the divergence is, because relative rate tests suggest
higher evolutionary rates for alligatorids; moreover, some alligatorid
clades are known to have significant ghost lineages, inflating molecular
rate estimates. Alligatorids also demonstrate the importance of taxonomic
revision when applying fossil calibrations, as phylogenetic reinterpretations
more than quadruple the first appearance age for some alligatorid lineages.
This highlights the importance of group-wide taxonomic sampling (including
fossils) and careful consideration of known geographic or facies biases
for the group's record.
PHYLOGENETIC REVISION AND FOSSIL DIVERGENCE
ESTIMATES: WHEN IS A CONFLICT NOT A CONFLICT?
BROCHU, Christopher A., and Colin D. Sumrall, Dept. of Geoscience, University
of Iowa, Iowa City, IA, USA; and Jessica M. Theodor, Dept. of Organismic
Biology, Ecology, and Evolution, University of California, Los Angeles,
CA, USA
Different sources of temporal informationthe stratigraphic
distribution of fossils and molecular distances between extant speciescan
yield very different estimates of divergence timing. But these do not
represent real "conflict" between data sets, as our temporal
estimates are limited by known incompleteness (the fossil record) and
labile assumptions (a priori estimates of molecular evolutionary
rate). Researchers are sometimes misled by imprecise language, leading
to a failure to address the same phylogenetic question with different
data sets. And although all aspects of divergence timing estimation, including
molecular clock calibration, ultimately rely on first appearance data
from the fossil record, the standard compendia used to obtain fossil first
appearance data have not always kept abreast of new discoveries or taxonomic
revisions accompanying applications of new phylogenetic methods to extinct
clades. Worse, rigorous phylogenetic methods have not been applied to
many prominent fossil groups, forcing comparisons between molecular estimates
(which are inherently phylogenetic) and nonmolecular patterns that may
reflect stratigraphic distributions or a priori process expectations
of evolution rather than phylogeny. This can lead to miscalibrations of
molecular clocks, but it can also cause researchers to find "conflict"
where none really exists, as the patterns being compared are nonanalogous
reflections of very different underlying processes. Many famous cases
of divergence timing "conflict" actually represent cases of
miscommunication because the fossil divergence estimates were not based
on hypothesis of phylogeny; real incongruence between molecules and fossils
can only occur if the fossils are considered in an explicitly phylogenetic
framework.
ZOOPHYCOS: STRUCTURAL AND ETHOLOGIC OVERVIEW
BROMLEY, Richard G., Geological Institute, University of Copenhagen,
Denmark
Truly a complex trace fossil, the venerable ichnogenus
Zoophycos is, as they say, "in need of revision." But
how? We need to understand the trace fossil better, before we undertake
a taxonomic revision.
The morphology of the trace fossil is highly variable,
both through time and within individuals. Several names, usually considered
synonyms of Zoophycos, are available for these variants, but their
occurrence within single individuals is not suggestive of synonymy. Perhaps
these heterogeneous individuals should be regarded as compound trace fossils.
Zoophycos also has been considered ethologically
diverse, and some authors have suggested more than one behavioral style
within some individual specimens. Suggestions for functions for the structures
include deposit feeding, surface-detritus feeding, constructional ballast,
waste disposal, cache-building, gardeningthe scope is large. Some
spectacular
individuals will be singled out for scrutiny. Can such wide diversity,
if genuine, be crowded into a single ichnogenus?
THE EVOLUTIONARY HISTORY OF THE NIMRAVIDAE (CARNIVORA)
IN THE JOHN DAY BASIN OF OREGON
BRYANT, Harold N., Royal Saskatchewan Museum, Regina, SK, Canada; and
Theodore J. Fremd, John Day Fossil Beds National Monument, Kimberly, OR,
USA
The Nimravidae is an extinct clade of cat-like carnivorans
of late Eocene to late Miocene age. The John Day Basin plays a pivotal
role in our understanding of nimravid evolution because the latter stages
of the initial North American radiation of this clade are best preserved
in its early Arikareean depositional sequence. Six of eleven North American
nimravinae species recognized in a recent systematic review are known
from the John Day (Hoplophoneus primaevus, Eusmilus cerebralis, Pogonodon
platycopis, Nimravus brachyops, Dinictis cyclops, Dinaelurus crassus);
the latter two species are known only from this area. Although the sources
of early collections from the John Day, including the type specimens of
five of the above species, are poorly documented, stratigraphically controlled
collecting since the mid 1980s, together with the dating of tuffs, has
provided a much improved biostratigraphic and temporal framework for interpreting
nimravid evolution.
The John Day sequence documents the last five million
years of nimravine history (3025 Mya), and provides an opportunity
to follow evolutionary trends and extinction events in this clade within
a limited geographic area. Nimravid diversity is high in the earliest
portion of the early Arikareean (below the Picture Gorge Ignimbrite; >28.7
Mya); at least the first four species in the above list are present. Later
in the early Arikareean, species diversity drops considerably (leaving
only the Pogonodon lineage, for which there is good stratigraphic
control, and possibly Dinictis cyclops and Dinaelurus crassus).
With the improved temporal resolution in the John Day sequence, the involvement
of possible causal factors, such as climatic and environmental change
and competitive exclusion, in the extinction of the nimravine clade can
begin to be assessed. Continued collecting will lead to further refinement
in the timing of evolutionary events, and an increasing ability to address
these issues in a rigorous fashion.
FOSSIL FUTURES: PRESERVING FOSSILS FROM PUBLIC
LANDSPANEL DISCUSSION WITH REPRESENTATIVES OF FEDERAL LAND MANAGEMENT
AGENCIES
BRYANT, Laurie, and Mike O'Neill, Bureau of Land Management, USA; Lucia
Kuizon, USDA Forest Service, USA; H. Gregory McDonald, National Park Service,
USA; Sally Shelton, National Museum of Natural History, Smithsonian Institution,
USA; and Theodore J. Fremd, John Day National Monument, Kimberly, OR,
USA
Fossils from federal lands have contributed significantly
to scientific research and public education for investigating and understanding
the history of life on earth. Most paleontological collections originating
from federal lands are housed in non-federal facilities throughout the
country, and held in trust for the benefit of the public. These institutions
provide expertise for the study, care and preservation of federal fossil
specimens; provide access to other researchers and scientists; and make
collections accessible to all segments of the public not otherwise able
to view such specimens. The relationship of federal agencies with non-federal
curatorial facilities, both public and private, is crucial to the continued
study, availability, management, protection, and interpretation of this
shared natural heritage.
Federal lands are administered by a variety of agencies
created for a specific purpose, each with its own legislative mandate
as to how these lands will be managed. Despite these unique mandates,
Department of the Interior agencies, U.S. Forest Service and the Smithsonian
Institution have made a commitment to develop a unified Federal policy
for storing and preserving fossils collected from federal lands. The goals
are to develop consistent standards for the professional long-term care
of fossil collections that maximize the availability of fossils for research
and scientific study, and to provide access to information resulting from
this research to the general public in the form of exhibits and educational
programs. Recommendations include new and continuing partnerships with
curatorial facilities; enhanced use of online databases, images and other
information technology; and an increased emphasis on stewardship opportunities.
The panel discussion will provide an open dialog that
will cover differences in philosophy of the various land management agencies,
their historical relationships with non-federal repositories, current
legal requirements of accountability for fossils from public lands, and
how these affect non-federal repositories.
EARLY EVOLUTION OF A DOMINANT CARIBBEAN REEF CORAL:
MORPHOMETRICS AND PHYLOGENETIC ANALYSIS OF EARLY PLIOCENE MONTASTRAEA
FROM THE DOMINICAN REPUBLIC
BUDD, Ann F., Dept. of Geoscience, University of Iowa, Iowa City, IA,
USA
The early evolution of a dominant Caribbean reef coral,
the Montastraea "annularis" species complex, is traced
using morphometric and phylogenetic approaches on specimens collected
in the early Pliocene of the Dominican Republic and the Plio-Pleistocene
of Costa Rica and Panama. To distinguish species, new landmark methods
are developed by comparisons with genetically characterized modern colonies
from Panama. The landmarks comprise 27 spatially homologous points, which
define the thickness and structure of the corallite wall and associated
costosepta. Bookstein size and shape coordinates are analyzed using cluster
analysis and canonical discriminant analysis, and three morphotypes are
distinguished in the Pliocene and ten in the Plio-Pleistocene. Cladistic
analyses are performed using characters derived partially from morphometric
data. Homology is assessed using microstructure. The results reveal two
or more distinct evolutionary groups. One group contains one modern species,
and the other contains a second; the relationships of the third are poorly
resolved.
High numbers of plesiomorphic taxa, long range extensions,
and lack of agreement with genetic data indicate that the new characters
alone are inadequate for interpreting evolutionary relationships. Longitudinal
characters involving the dissepiments and columella offer promise for
increasing resolution. Preliminary results suggest that the three modern
species of the M. "annularis" complex arose prior to
accelerated extinction at the end of Plio-Pleistocene faunal turnover
of Caribbean reef corals, and two may have originated younger than 4 Ma.
Three static and possibly ancestral species occur in the Pliocene of the
Dominican Republic; whereas six or more sister species are represented
in Plio-Pleistocene sequences in Costa Rica and Panama. Coexistence of
predominantly pre- and post-turnover clades may have been responsible
for the high diversity observed within the complex during turnover.
A NEW STEM-ARACHNATE FROM THE SIRIUS PASSET (LOWER
CAMBRIAN OF NORTH GREENLAND) AND THE BASAL EUARTHROPOD PROBLEM
BUDD, Graham E., Dept. of Earth Sciences (Historical Geology and Palaeontology),
University of Uppsala, Uppsala, Sweden
A new crown-group euarthropod is presented from the Lower
Cambrian Sirius Passet fauna of North Greenland. It is one of the most
common taxa in the present collections from the Sirius Passet fauna, being
represented by some 1700 specimens out of an estimated total of 8500 fossils
(19%). Much internal anatomy of the fossil has been preserved, although
interpretation of the preserved structures has been hampered by their
remarkably variable appearance in different specimens. A model for the
internal architecture of the animal is nevertheless proposed, which recognizes
the preservation of apodemes, musculature and the gut, and a complex internal
skeleton, providing the most complete picture of the internal anatomy
of any Cambrian arthropod. This morphology complements that preserved
in the Chengjiang and Burgess Shale faunas and offers a secure basis for
reconstruction of basal arthropod phylogeny, in particular in elucidating
the split between crown-group euarthropods (especially stem-group arachnates)
and taxa at the top of the stem group. However, the vexed question of
basal head segmentation patterns in euarthropods remains open to several
interpretations.
ESTIMATING BIODIVERSITY IN LIGHT OF HETEROGENEOUS
SAMPLING INTENSITIES: THE RELATIONSHIP
BETWEEN TAXON-OCCURRENCE SUBSAMPLING
METHODS AND ALPHA AND BETA DIVERSITY
BUSH, Andrew M., Molly J. Markey, and Charles R. Marshall, Dept. of Earth
and Planetary Sciences, Harvard University, Cambridge, MA, USA
Estimates of biologic diversity depend on sampling intensity.
If within-locality abundance data are available, a two-step standardization
method (an equal number of specimens per list and an equal number of lists)
will best normalize for heterogeneous sampling. Several proposed subsampling
methods require only presence-absence data, but it is unclear to what
extent they provide reasonable standardization. We explore the relationships
between the subsampling curves generated by these methods and alpha and
beta diversity. Alpha diversity is here equated with the mean number of
taxa over a set of lists, and beta is the total number of taxa divided
by alpha (a common definition well-suited to this type of data). The relationships
between the various subsampling curves and alpha and beta diversity may
be demonstrated using the curve that relates beta diversity to the number
of lists in a data set. Multiplying values of beta on this curve by alpha
produces the by-list (unweighted) subsampling curve. Multiplying beta
and the number of samples by alpha produces the by-list (weighted by occurrence)
curve, which is nearly identical to the rarefaction-by-occurrence curve.
Multiplying beta by alpha and the number of samples by alpha squared produces
the by-list (weighted by occurrences squared) method. These relationships
are exact if all lists contain an equal number of taxa. Heterogeneity
in list length only substantially affects the occurrences-squared curve.
We use these relationships to show how each method will respond to changes
in alpha and beta diversity. If within-locality sampling intensity is
constant, all methods will accurately reflect diversity changes driven
by beta, but the weighted subsampling methods will damp changes driven
by alpha. The unweighted method is most sensitive to changes in sampling
intensity. Thus, all methods will fail under some circumstances, and these
circumstances depend on the ways in which diversity structure and sampling
intensity vary in time and space.
PALEONTOLOGY AND PALEOECOLOGY OF THE ARCO HILLS
FORMATION (CHESTERIAN), EAST-CENTRAL IDAHO
BUTTS-MATHESON, Susan, and Peter E. Isaacson, University of Idaho, Moscow,
ID, USA
Within the thick Carboniferous carbonate and siliciclastic
rocks of the northern Rockies is a succession with exquisitely preserved
faunas of Chesterian (Late Mississippian) age. The Arco Hills Formation
yields abundant silicified brachiopods. Brachiopod assemblages show both
in situ communities and biostratinomic accumulations in storm-generated
packstones and grainstones. Beds with sufficient silicification and minimal
dolomitization were sampled at regular intervals. Extraction with muriatic
acid yielded abundant fossils, including some with all growth stages represented.
These were cleaned, photographed, and cataloged. Among the abundant brachiopods
are echinoderms, bryozoans, rare gastropods, bivalves, vertebrates, and
trilobites.
Inasmuch as Chesterian brachiopod faunas remain poorly
described, a complete taxonomic description is underway. Additionally,
detailed assemblage and community analysis within the Late Mississippian
Arco Hills Formation will be analyzed for the following parameters; generic
and species diversity, richness, and dominance. Preliminary community
analysis reveals low specific diversity Orbiculoidea, Spiriferidina/Athyrididae,
and Productoidea/Davidsonioidea communities.
Associations within brachiopod communities and facies
affinities will be used in biotopic analysis. With biocoenoses and taphocoenoses
found, the presence of communities can result in clarity of depositional
setting far exceeding that gained from lithologic analysis alone. Four
factors are of paramount interest to the regional geologist: depth (storm
and fair weather wave base), siliciclastic input, including the sediment
source, substrate availability, and lowered oxygen levels imposed by geographic
barriers or bathymetric changes. This paleoecologic work will help us
to answer these questions and improve what little is known about Antler
history.
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