NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Cl - De
(5/17/01)
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EARLY OCCURRENCE OF C4 GRASSES IN
MIDDLE MIOCENE NORTH AMERICA BASED ON STABLE ISOTOPES IN TOOTH ENAMEL
CLEMENTZ, Mark T., and Paul L. Koch, Dept. of Earth Sciences, University
of California, Santa Cruz, CA, USA
The timing of the appearance of C4 grasses within terrestrial
ecosystems has been reported to have occurred between 8 and 5 Ma in North
America, Asia, Africa, and South America. This conclusion is based on
isotope analysis of soil carbonates and tooth enamel from a few taxa within
each study area. The enamel carbon isotope value reflects the diet of
an organism, and can serve as a measure of consumption of C4
plants, which have significantly higher carbon isotope values than C3
plants. Because herbivores are selective foragers, analysis of only a
few taxa, instead of whole faunas, may reduce the possibility of accurately
gauging when C4 plants became a significant component of terrestrial
vegetation. Sampling of entire large-bodied terrestrial faunas, including
both browsers and grazers, provides a more accurate estimation of C4
presence in terrestrial ecosystems. We analyzed the carbon isotope composition
of herbivore tooth enamel from proboscideans, equids, camelids, antilocaprids,
and rhinoceratids from sites in Oregon, California, and Nebraska ranging
in age from 12 to 10 Ma. Carbon isotope values for grazers and browsers
in California and Oregon were within the range of expected values for
consumers of C3 vegetation. However, in Nebraska, carbon isotope
values were well outside the range of values expected for C3
consumers, with maximum values at -4 per mil. Also, we observed a distinct
separation in carbon isotope values between grazing and browsing taxa,
with grazing taxa yielding significantly higher carbon isotope values.
Decoupling of browser and grazer carbon isotope values in Nebraska and
low carbon isotope values for whole faunas in California and Oregon suggest
that change in the carbon isotope composition of atmospheric CO2
was not responsible for the isotope differences we have detected. Therefore,
we conclude that by 12 Ma, C4 plants were already a significant
component of terrestrial vegetative biomass within the mid-continent of
North America.
GRAPHIC CORRELATION OF THE UPPER DEVONIAN (FRASNIAN
AND FAMENNIAN)
COATES, John, Wright State University, Fairborn, OH, USA
The upper Devonian (Frasnian and Famennian) has been extensively studied
with respect to macrofossil data, but there is a lag in systematic high-resolution
biostratigraphic stuides. A detailed biostratigraphic study of eight outcrops,
in addition to the Standard Reference Section (SRS), was done in the central
southern Appalachian basin in southwest Virginia. The stratigraphic units
from the oldest to youngest are the Millsboro (Givetian), Brallier, Mallory,
Briery Gap, Blizzard, Pound, and Red Lick. The Mallory, Briery Gap, and
blizzard are Frasnian, while the Pound and Red Lick are Famennian. Data
from Brame 2001 was used in this study. The SRS contains a wide range
of comparable taxa that were compared to the seven other outcrops. A quantitative
analysis was performed on these comparisons to determine the Line of Correlation
(LOC). An accurate correlation was determined by extrapolating a section
from the Composite Standard and then compared to the mature Composite
Standard. Once the LOC is constrained, an accurate LOC is achieved. A
mature Composite Standard is analyzed for sediment accumulation rates,
Frasnian and Famennian extinction events and sequence stratigraphy of
the Upper Devonian. After a mature Composite Standard is formed it will
be tested against data from another section from the Appalachian Basin.
THE EVOLUTIONARY AFFINITIES OF CNIDARIAN-GRADE
EDIACARAN FOSSILS: TESTS USING MOLECULAR DIVERGENCE DATES
COLLINS, A.G., Museum of Paleontology and Dept. of Integrative Biology,
University of California, Berkeley, CA, USA; and B.M. Waggoner, Dept.
of Biology, University of Central Arkansas, Conway, AR, USA
Most of the latest Neoproterozoic "Ediacaran fossils"
have been referred to the phylum Cnidaria in the past. Justification for
these assertions has been on morphological grounds that range from vaguely
defined similarities to detailed comparisons. In particular, representatives
of the living Chondrophorina (Hydrozoa), Pennatulacea (Anthozoa), and
Scyphozoa have all been putatively identified in the Ediacaran biota.
We test these hypotheses using analyses of divergence dates implied by
an extensive phylogeny of extant cnidarians using 18S rRNA. Since 18S
rRNA can easily be shown to not evolve in a clock-like manner, we infer
molecular divergence dates by employing recently developed Bayesian methods
that do not require clock-like evolution. We investigate the effect of
using several calibrations of the molecular divergence dates, each depending
on various assumptions about the taxonomic affinities of various Ediacaran
fossils. If a calibration based on one interpretation of a controversial
fossil yields a glaringly improbable age for a better-known clade, that
interpretation is likely to be incorrect.
GLOBAL ORDOVICIAN FAUNAL TRANSITIONS IN THE
MARINE BENTHOS: PROXIMATE CAUSES
CONNOLLY, Sean R., Dept. of Marine Biology, James Cook University, Townsville,
QLD, Australia; and Arnold I. Miller, Dept. of Geology, University of
Cincinnati, Cincinnati, OH, USA
During the Ordovician Radiation, domination of benthic
marine communities shifted away from trilobites, towards articulate brachiopods,
and, to a lesser degree, towards bivalves and gastropods. In this paper,
we identify the patterns in origination and extinction probabilities that
gave rise to these transitions. Using methods adapted from capture-mark-recapture
(CMR) population studies, we estimate origination, extinction, and sampling
probabilities jointly in order to avoid confounding patterns in turnover
rates with temporal variation in the quality of the fossil record. Not
surprisingly, higher extinction probabilities in trilobites relative to
articulate brachiopods, bivalves, and gastropods were partly responsible
for relative decreases in trilobite diversity. However, articulate brachiopods
also had higher origination probabilities than trilobites, indicating
that relative increases in articulate brachiopod diversity would have
occurred even in the absence of between-class differences in extinction
probabilities. This contrasts with inferences based on earlier Phanerozoic-scale,
long-term averages of turnover probabilities, and it indicates that a
major cause of this faunal transition has been overlooked. Temporal patterns
in turnover rates suggest that the relative importance of origination
differences and extinction differences as determinants of these faunal
transitions shifted over the course of the Ordovician.
A NON-INVASIVE FLOATING GRID MAPPING SYSTEM
COOLEY, Joseph B., Christopher L. Organ, and Tobin L. Hieronymus, Museum
of the Rockies, Bozeman, MT, USA
In quarries where the concentration of bone is very high
or the fossil layer is very thick, mapping on a grid system can be quite
difficult. The inability to place and maintain accurate grid corner markers
throughout a quarry can cause inaccurate mapping of a quarry. During the
summer of 1999 the Museum of the Rockies excavated a hadrosaur quarry
that had very high concentrations of bone. To solve the problem of placing
grid corner markers throughout the quarry we created a floating grid system.
Along the back wall of the quarry wires were anchored and spaced at one
meter. On each wire the corners of each grid was marked by tape. When
a grid needed to be mapped the wires were extended to mobile posts where
they were attached and leveled. A one meter by one meter into 10 centimeter
by 10 centimeter squares was suspended from the grid wires by equal lengths
of wire attached to each corner. Longer wires allowed for mapping of the
specimens found lower in the quarry while shorter wires were used to map
specimens higher in the quarry. After the grid was mapped the grid wires
were rolled up and stored along the wall where they did not interfere
with the excavation. Preservation of the fossils was maintained while
the mapping was very accurate.
COLOR PATTERN STABILITY IN SEAGRASS NERITID GASTROPODS
FROM THE NEOGENE OF THE DOMINICAN REPUBLIC
COSTA, Fábio A.H., Exelixis, San Francisco, CA; and Ross H. Nehm,
Columbia University, Teachers College, New York, NY, USA
Morphological studies of species-level stasis and change
have been conducted on a wide-variety of taxa throughout the geological
timescale. These studies have focused almost exclusively on aspects of
skeletal size and shape; no studies appear to have investigated the macroevolutionary
dynamics of color pattern polymorphism. Here we report on our detailed
analyses of intraspecific and interspecific patterns of color polymorphism
in two neritid gastropods from the Neogene of the Dominican Republic.
We demonstrate that color pattern polymorphism is more stable than shell
morphology over macroevolutionary timescales. Neritina figulopicta
preserves intricate color patterns classifiable into seven categories
at the following frequencies: Interrupted 4%; Zigzag 20%; Textile 36%;
Banded 9%; Diagonal 4%; Network 26%; and Spotted 1%; Neritina virginea
of the Recent western Atlantic is hypothesized to be a close relative
of N. figulopicta. Shell color patterns alone do not distinguish
these two species, although slight differences in color pattern frequencies
do occur. In contrast, these species differ in submicroscopic aspects
of their teeth and plicae. The range and frequency of color pattern polymorphism
has remained stable in this lineage for a minimum of 13 MY, whereas shell
morphology has changed. Smaragida viridis preserves intricate color
patterns classifiable into seven categories at the following frequencies:
Absent 12%; Restricted 40%; Interrupted 25%; Straight 6%; Zigzag 12%;Textile
4%; and Banded 1%. An additional pattern, classified as D, has only been
observed in a few populations of extant Mediterranean specimens. Patterns
R, S, and Z are found in DR and Recent specimens of S. viridis
but are absent from other living species of Smaragdia. The range
and frequency of color pattern polymorphism in S. viridis has remained
stable for a minimum of 13 MY, whereas slight geographic and temporal
differences in shell morphology have occurred.
EVOLUTION OF HIGH-LATITUDE MARINE INVERTEBRATE
FAUNAS: A REVIEW
CRAME, J. Alistair, British Antarctic Survey, High Cross, Cambridge,
UK
Distinct high-latitude and polar marine invertebrate
faunas can be traced back in time to at least the Late Paleozoic era.
A number of them contain strong bipolar elements and it would seem likely
that these were formed by some type of global climatic differentiation.
Although comprehensive data sets are still at a premium, it is becoming
apparent that these high-latitude and polar faunas are also of consistently
lower taxonomic diversity than their lower-latitude counterparts. Latitudinal
diversity gradients are a persistent feature of the fossil record, although
on nothing like the scale of those seen at the present day. They may be
taken as an indication that, when averaged over time, there is a significant
difference in the rates of evolution between tropical and polar regions.
The dramatic steepening of gradients through the Cenozoic
era may be attributable to a pulse of tropical speciation. This in turn
could have been driven by purely intrinsic factors, such as evolutionary
escalation and intense competition between certain shallow-water clades.
However, there is also evidence to suggest that extrinsic factors, such
as climate change, promoted Cenozoic diversification on a variety of temporal
and spatial scales. In particular the Neogene radiation of many taxa has
been linked to the onset of pronounced glacioeustatic climate cycles.
These same cycles undoubtedly had a global effect but were more pronounced
in the tropics due to the greater amount of available habitat space there.
We cannot yet say that rates of extinction were significantly
higher for marine invertebrate taxa in the polar regions. Even the most
dramatic Cenozoic temperature declines average out to no more than a fraction
of a 1°C per thousand years. Levels of productivity may be more important
than temperature per se in controlling the composition of polar faunas.
INTERTIDAL MOUNDS OF TROPICAL CALLIANASSIDS PROVIDE
SUBSTRATES FOR COMPLEX UPOGEBIID SHRIMP BURROWS: MODERN AND PLEISTOCENE
EXAMPLES FROM THE BAHAMAS
CURRAN, H. Allen, Dept. of Geology, Smith College, Northampton, MA, USA;
and Anthony J. Martin, Dept. of Environmental Studies, Emory University,
Atlanta, GA, USA
Burrowing by thalassinidean shrimp in modern tropical,
shallow subtidal to intertidal carbonate environments is widespread and
a powerful bioturbation agent of sandy substrates. Deep and intense burrowing
by callianassid shrimp commonly occurs on the margins of hypersaline lagoons
throughout the Bahamas, such as Pigeon Creek on San Salvador Island. Extensive
sand flats along Pigeon Creek are deeply and thoroughly bioturbated by
the callianassid Glypturus acanthochirus. In addition to dominating
the deep tier, burrowing activity of the callianassids results in a highly
mounded intertidal surface. Individual burrow cones commonly coalesce
with time to form composite mound surfaces that become stabilized with
development of microbial mats. These stabilized surfaces set the stage
for colonization by shallow-tier burrowers, particularly the upogebiid
shrimp, Upogebia vasquezi, and several species of fiddler crabs.
Burrow systems of Upogebia vasquezi are distinctive
and complex. They typically consist of a pair of U-shaped burrows in close
proximity or crisscrossing, with knobs or short tunnels at their bases.
The entirety of the burrow pair is surrounded by a thick, externally pelleted
wall. Inside burrow diameters range from 210 mm, and burrow depths
are 1015 cm, in contrast to the much deeper callianassid burrows.
These complex upogebiid burrows also occur as trace fossils in late Pleistocene
lagoonal facies on San Salvador. Initially reported as fragmentary burrow
fills, whole burrow systems virtually identical to the modern upogebiid
burrows more recently have been found at several localities. The fossil
burrows are most abundant immediately below a terra rossa paleosol marking
late Pleistocene stillstand and regression of seas associated with onset
of Wisconsinan glaciation. This stratigraphic occurrence makes these complex
upogebiid trace fossils potentially useful as both paleoenvironmental
and sea-level position indicators for Quaternary carbonate sequences throughout
the Bahamas and other geologically similar regions.
DIGITAL BIOTA: OVERVIEW OF BIOLOGICALLY INSPIRED
SOFTWARE SYSTEMS FOR MODELING BEHAVIOR AND EVOLUTION
DAMER, Bruce, Contact Consortium, Scotts Valley, CA, USA
In 1997, a special conference involving paleontologists,
computer scientists and artists, was held in Banff, Canada and featured
a trek to the Burgess Shale. The event was meant to create cross-disciplinary
connections linking the study of evolution and biology with the developing
practice of software systems exhibiting biological and evolutionary properties.
Using computer-based demonstrations the speaker will review two classes
of software systems presented at the Digital Burgess Conference and consider
their relevance to the paleontological community.
One set of systems model aspects of the environment in
which biological systems exist, simulating 3D space, gravity, terrains,
safe and hazardous areas. Simplistic "digital biological entities"
(biots) are placed in these virtual worlds and "learning" behaviors
through adaptive forms of signaling produce behaviors akin to organisms
in nature. Adapting such a system to paleontology might result in a system
able to derive the construction of fauna responsible for fossil traces
in some of the oldest Cambrian sediments.
A second class of software systems attempts to create
the preconditions and carrying capacity to allow a large number of "digital
biots" to evolve a simple "genome" data structure and express
morphological changes through competition and reproduction. The dynamics
of large, rapid population shifts and travel over networked computer systems
creates an evolutionary environment not found in biology. Observing these
systems causes one to speculate on the basic algorithmic nature of living
systems divorced from physical representation (i.e., carbon-based biology).
One might consider how life could be "elsewhere" (as in Astrobiology)
or how novel forms of life might emerge in the future (say, from human
technology). While not often engaged in by scientists, this kind of thought
experiment is useful in that it can broaden both professional and personal
intellectual horizons and cast new light on the nature of living systems.
A PHYLOGENETIC EXAMINATON OF THE NEAREST-LIVING-RELATIVE
METHOD FOR RECONSTRUCTING PALEOCLIMATE AT MAMMALIAN FOSSIL LOCALITIES
DAVIS, Edward B., Dept. of Integrative Biology and Museum of Paleontology,
University of California, Berkeley, CA, USA
Overlapping climatic tolerances of extant taxa are commonly
used in paleoclimate reconstruction. This method is limited by the stratigraphic
ranges of living taxa. Paleoclimate hypotheses have been extended deeper
in time through assuming that the nearest living relatives of extinct
taxa provide appropriate climatic analogs. These methodologies implicitly
assume that the climatic tolerances of taxa do not change through time,
and the nearest-living-relative method assumes that there is a phylogenetic
control on the climatic tolerances of evolving lineages.
The assumptions of the nearest-living-relative methodology
can be tested for mammal lineages through a phylogenetic analysis that
examines the association of various important climatic parameters with
various taxa. Accordingly, this study applied a phylogenetic approach
to understand the relationship between climatic features (such as maximum
and minimum January and July temperatures, annual precipitation, and seasonality)
and evolution of extant species within Marmota and Microtus.
Species within these genera have been considered important paleoclimate
indicators due to their abundances, distinctive dental characters, and
present restriction to certain microhabitats. The association between
phylogenetic hypotheses based on molecular data and climatic parameters,
both derived from published records, was tested using Felsenstein's independent
contrast method. The technique involved mapping the climatic tolerances
of various species onto the hypothesized phylogenetic relationships and
thereby determining if groups of species were delineated by identifiable
climatic boundaries.
Preliminary results indicate a correlation between phylogeny
and climate tolerances for Microtus species endemic to North America.
If additional analysis substantiates these results, the nearest-living-relative
method could prove to be an important tool in reconstructing the paleoclimates
of some fossil mammal localities.
AZOOXANTHELLATE CORAL IN SPACE AND TIME:
BIOGEOGRAPHY AND DIVERSITY PATTERNS FROM THE NEOGENE TO THE RECENT IN
THE CARIBBEAN AND SURROUNDING AREAS
DAWSON, John P., Dept. of Geoscience, University of Iowa, Iowa City,
IA, USA
In order to understand spatial and temporal patterns
of azooxanthellate corals in the Caribbean, a database of Neogene to Recent
azooxanthellate corals in the Caribbean and surrounding areas has been
compiled. The Recent record consists of 129 species of azooxanthellate
corals from the 19 geographical/political regions in the Caribbean and
surrounding areas. The total species-by-region data matrix was divided
into two sub-matrices representing the shallow water taxa (less than 200
meters) and the deep-water taxa (greater than 200 meters). These two sub-matrices
were used to analyze how geographic distributions change with depth. The
total matrix and the two sub-matrices were analyzed using r-mode and q-mode
cluster analyses using Bray-Curtis' similarity coefficient and UPGMA clustering
algorithm. In addition, detrended correspondence analysis of the regions
was performed.
Results for the total data matrix revealed three major
groups of regions and one ungrouped region. One of these groups has a
primarily insular, tropical faunal component and includes the center of
diversity for the Caribbean. A second grouping lacks the primarily insular,
tropical faunal component but has a subtropical Carolinian faunal component.
The shallow water sub-matrix displays the same groups as the total matrix.
However, the deep-water sub-matrix has some changes in its groupings and
indicates a more uniform, deep-water fauna throughout the Caribbean.
The Neogene record consists of 49 species of azooxanthellate corals from
nine regions in the Caribbean. Initial cluster analysis results of the
Neogene data indicate that the center of the Caribbean appears to have
been the center of diversity for the azooxanthellate corals since the
Neogene. However, there has been large turnover of the fauna at the Pliocene-Pleistocene
boundary with only eight Neogene species present in the Recent.
THE ORIGIN, EVOLUTION, AND BIOGEOGRAPHY OF WALRUSES
(CARNIVORA: ODOBENIDAE)
DEMÉRÉ, Thomas A., Dept. of Paleontology, San Diego Natural
History Museum, San Diego, CA, USA
The monophyletic Odobenidae or walrus clade includes
a single extant species, Odobenus rosmarus, as well as at least
20 fossil species arranged in 14 genera. Phylogenetic and stratigraphic
data indicate that odobenids first evolved in the North Pacific region
sometime before 18 Ma (late early Miocene) with basal taxa being confined
to the eastern (Proneotherium) and western (Prototaria)
parts of this region during the early middle Miocene. The later diverging
odobenid Neotherium is found in the eastern North Pacific in the
late middle Miocene. In the North Pacific during the early late Miocene
species of the generalized odobenid Imagotaria are found in both
the western and eastern North Pacific. A major radiation in the late Miocene
produced two odobenid crown clades, the Dusignathinae (includes the extinct
genera Dusignathus, Gomphotaria, and Pontolis) and
the Odobeninae (includes, in addition to the modern walrus Odobenus,
the extinct genera Aivikus, Protodobenus, Pliopedia,
Alachtherium, Prorosmarus, and Valenictus). The fossil
record indicates that dusignathine walruses remained endemic to the eastern
North Pacific throughout their evolutionary history. In contrast, odobenine
walruses, although evolving in the North Pacific during the late Miocene,
dispersed into the eastern and western North Atlantic via the Arctic Ocean
by early Pliocene time. The last of the dusignathine walruses is known
from the late Pliocene of the eastern North Pacific. Odobenus evolved
in the North Pacific and dispersed into the Arctic Ocean and eventually
the North Atlantic probably during one of the early interglacial events
of the latest Pliocene and Pleistocene. During the Pleistocene there was
possibly a single circum-arctic species of Odobenus that extended
its range into near temperate latitudes in both the Pacific and Atlantic
during interglacial periods. The two extant subspecies of Odobenus
rosmarus may represent the product of range fragmentation and allopatric
speciation during a glacial period of maximum Arctic sea ice volume.
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