NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Hu - Iv
(5/17/01)
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TAGMATA, SEGMENT SPECIFICATION, AND THE DYNAMICS
OF POST-CEPHALIC SEGMENT ACCRETION IN TRILOBITES
HUGHES, Nigel C., Dept. of Earth Sciences, University of California,
Riverside, CA, USA.; Giuseppe Fusco and Alessandro Minelli, Dept. of Biology,
University of Padova, Padova, Italy; and Mark Webster, University of California,
Riverside, CA, USA
While variation in the number of trilobite cephalic segments
remains debatable, it is clear that the postcephalic region exhibited
wide variation in segment numbers among different clades. Intraspecific
variability in the number of thoracic segments is known for at least 25
species, mainly Cambrian, so the boundary between thorax and pygidium
was placed at a different segment in different adults of the same species.
The thorax to transitory pygidium boundary also shifted during ontogeny.
Among Recent arthropods, intraspecific variability in segment number is
known in several clades, but in all cases tagmata have definitive boundaries
as soon as they become expressed as distinct morphological entities. Equating
trilobite body regions with expression domains of Hox genes is
not straightforward because although the dorsal exoskeleton is divided
into two posterior units, the thorax and the pygidium, the ventral appendages
associated with these units share a similar basic structure. A similar
mismatch between dorsal and ventral structures is also known among Recent
arthropods, but trilobites are apparently unique in that the regional
identity of individual postcephalic segments changed during their ontogeny,
as segments formed in the pygidium were later released into the thorax.
The pattern of growth in the postcephalic region of trilobites is hemianamorphic,
i.e., only the early molts were accompnied by an addition of new thoracic
segments (meraspid period = anamorphic phase), then the animal continued
to molt without further addition of thoracic segments (holaspid period
= epimorphic phase). As in some Recent arthropods, the shape of the adult
appears more tightly constrained through ontogeny than the number of segments:
in adult Aulacopleura konincki, specimens with 18 to 22 thoracic
segments shared almost identical sagittal proportions. These results suggest
that there was some developmental flexibility in trilobite body architecture,
thus raising the question of whether trilobite postcephalic tagmata are
strictly comparable to those of the remaining arthropods.
EVENT BED DEPOSITION IN THE CINCINNATIAN SERIES:
IMPLICATIONS FOR TAPHONOMIC PROCESSES AND ASSESSING MICROEVOLUTIONARY
CHANGES WITHIN FLEXICALYMENE
HUNDA, Brenda R., and Nigel C. Hughes, Dept. of Earth Sciences, University
of California, Riverside, CA, USA
Despite intense scientific interest there is currently
little high resolution data available to understand how organisms respond
to multiple episodes of environmental change at time-scales ranging from
1,000 to 1,000,000 years. The prerequisites for such a study include exceptional
preservation of multiple fossiliferous horizons and a high-resolution
stratigraphic framework. Recent stratigraphic analyses of the Cincinnatian
Series now provide an exceptionally precise spatial and temporal framework
for assessing micro-evolutionary changes within individual species and
species lineages.
Initial studies in the area have shown that storm-related
episodes of rapid mud deposition smothered populations of live Flexicalymene,
preserving unique and substantial samples of contemporary individuals
alive some 450 million years ago. Thin section analysis has revealed a
similar depositional regime at Mt. Orab, within the Arnheim Formation,
with at least seven gradational beds within a 0.46 m mudstone unit. Differences
in size distribution, density, and attitude of the trilobites suggests
that Mt. Orab beds differ from the specific behavioral aggregations seen
within the "granulosa" bed of the Kope Formation, although both
are thought to represent contemporaneous populations. Similar "event
bed" preservation occurs throughout the Cincinnatian Series, offering
the possibility of repeated sampling of contemporary populations sequentially
throughout the Series. Morphometric analysis of these contemporary populations
of Flexicalymene will constrain patterns of morphological variability
at the population level, providing a firm basis for understanding the
morphological variation evident within Cincinnatian Flexicalymene,
and its relationship to multiple episodes of environmental change within
a sequence stratigraphic framework.
TIME-AVERAGING AND MORPHOMETRIC DATA: DO FOSSIL
SAMPLES ACCURATELY REFLECT POPULATION-LEVEL VARIABILITY?
HUNT, Gene, Committee on Evolutionary Biology, University of Chicago,
Chicago, IL, USA
While the importance of time-averaging is widely appreciated
in paleoecological studies, its effects on morphological data have been
less explored. Morphological change during the interval in which a sample
accumulates will inflate the phenotypic variance of that sample. In this
study, I consider two related questions: (1) By how much are time-averaged
samples expected to overestimate population variance under different models
of evolution? (2) Does analysis of published data suggest that the variance
inflation in fossil samples is intolerable large? If fossil samples tend
to grossly overestimate variability, paleontologists must be cautious
when attempting to infer biological variation in fossil taxa.
To address the first question, I derive the expected
degree to which fossil samples should overestimate population variances
under three models of evolution: (i) constant (linear) evolution, (ii)
unbiased random walk and (iii) biased random walk. For these models, the
expected variance inflation can be expressed as simple functions of time
and rate parameters, but more empirical work is necessary to establish
realistic ranges for these rates. In order to address the second question,
I first compiled morphologic data on fossil and recent samples of the
same species from the literature, and compared their variability. As a
complementary approach, I also used published data from examples of within-lineage
morphological evolution to examine the effects on variability of artificially
time-averaging adjacent samples.
Results indicate that (1) fossil and modern samples of
the same species usually show comparable levels of variability, and (2)
often, one can lump samples spanning thousands to even millions of years
without doing great violence to estimates of within-sample variance. There
are, of course, instances where variances estimated from fossil samples
will be gross overestimates. However, it appears that for most paleontological
purposes, fossil variability is an adequate proxy for population-level
variability.
REVISING PALEOGENE WEST ANTARCTIC CLIMATE AND VEGETATION
HISTORY: NEW GEOCHRONOLOGY AND PALAEOENVIRONMENTAL DATA
HUNT, Richard J., School of Earth Sciences, University of Leeds, Leeds,
UK
Paleocene-Oligocene volcanics with plant-bearing sediment
intercalations crop out extensively on King George Island, Antarctica.
These plants are the most complete Paleogene terrestrial foliar record
in Antarctica and variations in the composition of the flora are the basis
of climate change models for this period (e.g., Birkenmajer, 1997).
The flora is preserved in lacustrine deposits and grew
in the fore-arc region of the Antarctic Peninsula, where it was prone
to inundation by arc volcanics. It comprises impressions and carbonised
compressions of leaves, fertile material and silicified wood. Gymnosperms,
angiosperms and ferns are represented.
The Wawel flora from Point Hennequin is currently regarded
as an impoverished Oligocene post-glacial flora. However, 40Ar/39Ar
dating of the encapsulating lavas indicates that the sequence is early
Eocene in age (4449 Ma) and recent field collections have yielded
a diverse range of plant fossils from the locality. Thirty-two angiosperm
leaf morphotypes have been described and are referred to families including
the Nothofagaceae, Proteaceae, Sterculiaceae, and Lauraceae. This increases
the recognised diversity of Eocene vegetation in West Antarctica and is
important because the composition of the flora is demonstrably different
from other Eocene localities on King George Island. Leaf margin analysis
of the Wawel flora, based on simple linear regression, yields a mean annual
temperature of ~9° C.
In overall composition, the closest modern analogue for
the King George Island flora is the Valdivian rainforests of Chile. These
forests are controlled disturbance, largely of volcanic origin. Local
variations in vegetational composition previously attributed to climatic
change during the Paleogene could be explained in terms of disturbance
and related succession dynamics.
Birkenmajer, K. 1997. Bulletin of the Polish Academy
of Sciences, Earth Sciences 44(3):157181.
GEOLOGY AND PALEONTOLOGY OF THE UPPER JOHN DAY
BEDS, JOHN DAY RIVER VALLEY, OREGON: LITHOSTRATIGRAPHIC AND BIOCHRONOLOGIC
REVISION IN THE HAYSTACK VALLEY AND KIMBERLY AREAS
HUNT, Robert M., and Ellen Stepleton, Div. of Vertebrate Paleontology,
University of Nebraska, Lincoln, NE, USA
Fine-grained pyroclastic sediments of the John Day Formation
in central Oregon preserve superposed mammalian faunas of Oligocene through
early Miocene age. Youngest faunas from the upper part of the formation
date the final phase of continental deposition prior to outpouring of
the Columbia River Group basalts. Upper John Day rocks, first described
by J.C.Merriam (19001901) in the Kimberly and Haystack Valley areas,
were subsequently divided by Fisher and Rensberger (1972) into two members.
We focused our study on this geographic area and these units. Upper John
Day sedimentation in the Kimberly-Haystack Valley area was punctuated
by at least two major erosional episodes prior to basalt flooding. South
of Kimberly, the Kimberly Member is disconformably incised and overlain
by tuffaceous late Arikareean siltstones (~22.6 Ma) with fluvial coarse
gravels. This sequence was later tilted, faulted, and eroded, and on the
eroded surface coarse gravels and tuffs, containing a Hemingfordian fauna
was deposited in angular unconformity. After a final erosive interval,
the entire sequence was capped by basalts. In Haystack Valley, Balm Creek
dissects the southern limb of a syncline, which preserves the most complete
local section of upper John Day rocks. Four sedimentary units are identified,
the lowest two bearing Arikareean faunas, and the latter two without fossil
mammals. The uppermost of these units, comprising coarse gravels and tuffaceous
sandstones, cuts deeply into the underlying rocks, and is believed to
correlate to the fossiliferous Hemingfordian unit south of Kimberly. Because
the Hemingfordian unit is of regional extent, and lies with angular unconformity
on older John Day rocks, it probably deserves separate formation rank.
The complexity of upper John Day rocks suggests greater variety in early
Miocene depositional settings relative to more uniform lower John Day
Oligocene environments.
SPATIAL PATTERNING AMONG LATE CRETACEOUS (LANCIAN)
MAMMALS IN NORTH AMERICA
HUNTER, John P., Dept. of Anatomy, New York College of Osteopathic Medicine,
Old Westbury, NY, USA
I tested the previously proposed hypothesis that Late
Cretaceous (Maastrichtian) mammalian faunas in North America differ in
composition and dominance along a north-south gradient. For this purpose,
I compiled a dataset of occurrences and abundances of Lancian mammalian
faunas from the northern North American Western Interior. Initial ordination
using correspondence analysis revealed variation among these faunas in
both composition and dominance associated with latitude. To further test
whether these patterns were due to simple spatial autocorrelation (i.e.,
resemblance solely due to geographic proximity) rather than a large-scale
north-south gradient, I examined the partial matrix correspondence (Mantel)
structure among faunal dissimilarity, spatial separation (surface distance),
and latitude. There was no association between composition or dominance
and latitude when surface distance was held analytically constant. Significant
association between composition and dominance remained with surface distance,
however, when latitude was held constant. Spatial patterning among faunas
is more likely explained by spatial separation than by a north-south gradient.
Further examination of the correspondence between individual species distributions
and surface distance, however, revealed interpretable patterns, such as
instances of congeneric species, presumed to be ecologically similar to
one another, replacing one another along the landscape. Thus, lower-level
ecological processes, such as competition, may underlie the observed larger-scale
spatial pattern.
COMPARATIVE PALEOBIOLOGY OF TWO DIFFERENT MIDDLE
TRIASSIC MARINE ENVIRONMENTS FROM WESTERN PANGEA (USA)
HUYNH, Tran T., and David J. Bottjer, Dept. of Earth Sciences, University
of Southern California, Los Angeles, CA, USA
Following the end-Permian mass extinction, it wasn't
until Middle Triassic times that normal benthic conditions returned and
various groups were re-established worldwide. This period marks the initiation
of the Mesozoic marine radiation, as measured by global diversity trends.
Recent work on the Early Triassic recovery interval has allowed for better
assessment of the paleobiological changes that occurred in the benthic
realm at the transition from the Early to Middle Triassic.
Preliminary examination of different paleoenvironments
represented by Middle Triassic Star Peak Group strata (west ern US) suggests
that the ecological and evolutionary character of the initial Mesozoic
marine radiation varied between depositional settings. Compared to Early
Triassic assemblages of nearshore environments, less cosmopolitan members
and increased levels of tiering complexity characterize the Middle Triassic
fauna. Lazarus taxa continued to return to level-bottom nearshore settings
at this time, filling in more Bambachian megaguilds. In contrast, deep-water
assemblages of the Middle Triassic are significantly different from those
found in the Early Triassic from similar depositional settings. The fossil
associations of deeper-water environments are comprised of cephalopod
and bivalve taxa that are more typical of later Mesozoic assemblages.
Thus, while nearshore environments exhibited community-level patterns
of re-assembly by Lazarus taxa, evolutionarily distinct offshore assemblages
emerged at the initiation of the Mesozoic radiation in the western US.
PLUME WINTER SCENARIO FOR THE PERMO-TRIASSIC
BOUNDARY MASS EXTINCTION
ISOZAKI, Yukio, Dept. of Earth Sciences and Astronomy, University of
Tokyo, Komaba, Tokyo, Japan
The end-Permian mass extinction, the greatest in the
Phanerozoic, occurred through two distinct steps, i.e., the first big
decline in biodiversity across the Guadalupian/Wuchapingian boundary and
the well-known main one across the Chanhsingian/Griesbachian boundary.
The deep-sea cherts in Japan also recorded changes across the two horizons
in fauna, lithofacies and redox. The intercalation of tuff at the two
horizons, in stratotypes in South China strongly suggests an intimate
cause-effect relation between volcanism and extinction. In particular,
the ryholitic nature of tuff beds indicates explosive volcanic eruption
derived from highly viscous acidic magma rather than contribution from
the nearly coeval Siberian flood basalt. The "Plume Winter"
scenario is proposed to explain a possible link among the following three
unusual geologic phenomena occurred across the Permo-Triassic boundary
(PTB); the existence of Pangea, long-term oxygen depletion in deep-sea
(superanoxia), and mass dying. These three are all global in context and
unusual in the Phanerozoic but unique to PTB. The coincidence in timing
of the initial breakup of Pangea, superanoxia, and biosphere crisis probably
indicates a sequence of events triggered by a superplume activity in Earth's
mantle. When a plume head penetrated into the bottom of preexisting continent
to break up, partial melting of crust may have occurred to generate rhyolitic
magma. Unusually violent volcanism associated with continental breakup
may have caused (1) formation of dust/aerosol screen, (2) stop of photosynthesis,
(3) collapse of food web, (4) mass extinction, and (5) superanoxia. The
noble gas evidence for extraterrestrial impact (Becker et al., 2001) from
an erroneously assigned PTB horizon in Japan is not accepted straightforward.
CLIMATIC AND TECTONIC SIGNIFICANCE OF UPPER
MIOCENE AND LOWER PLIOCENE DIATOMITES IN CENTRAL MEXICO
ISRADE, Isabel, and Victor Hugo Garduño, Instituto de Investigaciones
Metalurgicas, Depto. de Geología, Edif. U. Universidad Michoacana
de San Nicolás de Hidalgo, México; and John A. Barron, USGS,
Menlo Park, CA, USA
An initial Miocene (117 Ma) phase of lacustrine
sedimentation in west central Mexico occurred during a period of widespread
tectonic extension. Lacustrine diatomaceous rocks of this period contain
the genus Mesodictyon,which also characterizes upper Miocene deposits
in the western US, Peru, France and North Africa. Although climatic conditions
in west central Mexico during this interval were relatively warm and humid,
the lakes were shallow and limited in extent.
Following a latest Miocene (85.2 Ma) stage of reduced
precipitation and very limited lacustrine sediments, a period of extensive,
relatively deep, perennial lakes extending for more than 250 km in an
east-west direction marked the early Pliocene period between 5.2 and 4.0
Ma. Pliocene diatomites contain Stephanodiscus carconensis and
Cyclotella "Tertiarius" spp., taxa found in rocks
of this age in the western US. Pliocene vertebrate faunas from Rancho
El Ocote and Coecillo (Guanajuato) reflect a savanna setting with moist
and warm conditions. This interval of the early Pliocene is marked by
relatively high global sea level and increased high latitude temperatures.
Restriction of the Central American Seaway during the latest Miocene may
have also acted to increase precipitation in central Mexico during the
early Pliocene.
Shallow lake and fluvial deposits dominate after 4.0
Ma, and vertebrate remains of La Goleta in Michoacan and Rancho Viejo
in Guanajuato document a period of dispersal from North and South America.
A combination of reduced volcanic tectonic processes and reduced precipitation
are presumed to have been the cause for this middle Pliocene reduction
in lake size.
XENOTURBELLA (PHYLUM UNCERTAIN): THE
APPEARANCE AND LOSS OF EVERYTHING DURING ITS DEVELOPMENT
ISRAELSSON, Olle, Dept. of Integrative Biology and Museum of Paleontology,
University of California, Berkeley, CA, USA
Xenoturbella Westblad, 1949 is a strange marine
animal (up to 4 cm long) with epithelial epidermis and gastrodermis, a
basiepidermal nerve plexus and a ventral mouth, but without an anus, concentrated
nervous system, or any other distinct organs except for a "statocyst"
containing flagellated "statoconia." It is marine and not parasitic.
Despite its peculiarities and possible relevance to the early phases of
the metazoan evolution, Xenoturbella has been neglected by most
textbooks. Since its discovery, it has been the subject of most diverse
interpretations: as one of the most primitive metazoans due to its simplicity
in organization, as a primitive relative of acoelomorph flatworm, or as
a paedomorphic holothurian or enteropneust.
However, the simple body plan of Xenoturbella is neither
due to paedomorphy nor to plesiomorphy but to metamorphosis from a complex
larva. No living embryos have been observed before. The larvae have alimentary
tract, mantle cavity, gills and concentrated nervous system while the
adults lack such structures. The embryology as well as molecular data
indicate that Xenoturbella actually is a lophotrochozoan, probably
within or close to molluscs. Solving its systematic position does not
make it less puzzling. Why would an animal that is neither parasitic,
microscopic nor short-lived lose all its organs and change its concentrated
nervous system with ganglia to a loose network of neurons, especially
when its larva has all the features the adults lacks?
Xenoturbella has a general importance for the
understanding of evolution. It shows that it is possible for an organism
with a specialized body plan (larvae with complex morphology) to develop
into a totally different type of organism (adults without organs). Xenoturbella
is not an ancient group, a Cambrian relict. Instead, the embryonic data
suggest that it is fairly recent.
PALEONTOLOGICAL EVIDENCES OF THE EARLY EVOLUTION
OF THE CARIBBEAN SEAWAY
ITURRALDE-VINENT, Manuel A., Museo Nacional de Historia Natural, La Habana,
Cuba; and Zulma Gasparini, Museo de Historia Natural, Depto. Paleontología
Vertebrados, La Plata, Argentina
Similarities among several groups of Jurassic marine
animals that occur both in the western Tethys and the southwestern Pacific
suggest that since the Sinemurian (nearly 195200 m.y. ago) there
was an aquatic connection between both regions. Although such a connection,
theoretically, may have been throughout some gateway located south of
Pangaea, there are several biogeographic reasons to suggest that the preferred
passway was placed within central Pangaea. According to recent paleogeographic
reconstructions, this passway was established before the break-up of Pangaea,
probably across a dominantly shallow siliciclastic epicontinental basin
in the interior of western Pangaea. This sea should not be thought of
as the Caribbean basin, but as a precursor. The opening of an oceanic
Caribbean Seaway, located between North and South America, is corroborated
by the occurrence of an important assemblage of Oxfordian marine animals
in the Guaniguanico terrain of western Cuba, an assemblage that is clearly
related with both the western Tethys and the southwestern Pacific faunas.
The opening of the Caribbean Seaway represent an important paleoceanographic
event, as only from that moment may had had started the Mesozoic deep
circumequatorial oceanic circulation that linked the Tethys, the Central
Atlantic and the Pacific oceans.
LOCOMOTION TRAILS OF THE VENDIAN INVERTEBRATES PRESERVED WITH THE PRODUCER'S
BODY FOSSILS, WHITE SEA, RUSSIA
IVANTSOV, Andrei Yu., and Mikhail A. Fedonkin,
Paleontological Institute, Russian Academy of Sciences, Moscow, Russia
Body fossils of two invertebrate species are found in
direct association with their locomotion trails in the Vendian siliciclastic
deposits about 555 Ma old (Zimnii Bereg, White Sea). Bilateral and segmented
Yorgia (up to 25 cm long) is preserved in negative relief by the
chains or clusters of its ventral surface imprints preserved in the positive
relief on the lower bedding plane. Positive and smooth relief, absence
of the sharp border line between the trail and the surrounding microrelief
of the bedding plane and uniform morphology make the fundamental difference
of the ichnofossil from the associating body imprint that normally shows
a wide spectrum of preservation forms. While crawling over the mud Yorgia
produced an abundant mucus like the recent flat worms or gastropods. The
mucus impregnated, glued and sealed the sediment, thus protecting the
trail from erosion during the sedimentation event. Short impulses of gliding
locomotion alternated with longer resting phases during which more mucus
was produced and exact imprint of the ventral side was fixed in the sediment.
In the light of this study we have to reconsider the nature of other segmented
fossils preserved in a positive reliefthey may well be locomotion or feeding
trails. Short trails are found behind a few small (1 cm long) specimens
of Kimberella. These trails preserved in negative relief on the
sole of the sandstone bed were produced by the dorsal shell of an animal
while it was trying to escape the sand after the sedimentation event.
Another kind of ichnofossil produced by Kimberella is a fan-shape
scratch mark that goes from one end of the body fossil. These feeding
tracks may reflect the work of the proboscis that bears the hook-like
organs on its end.
USING STABLE ISOTOPIC DATA TO RESOLVE VARIATION
IN RATE AND DURATION OF SEASONAL GROWTH THROUGHOUT ONTOGENY
IVANY, Linda C., Dept. of Earth Sciences, Syracuse University, Syracuse,
NY, USA; Douglas S. Jones, Florida Museum of Natural History, University
of Florida, Gainesville, FL, USA; and Bruce H. Wilkinson, Dept. of Geological
Sciences, University of Michigan, Ann Arbor, MI, USA
Understanding variation in the rate and timing of growth
with ontogeny is a fundamental component of many paleobiological and paleoecological
studies. Examining variation through ontogeny in the stable isotopic composition
of accretionary biogenic hard parts is becoming more commonplace as a
technique for providing estimates of age and for gaining insights into
change in growth rate through ontogeny, as well as for inferring the environmental
conditions under which organisms lived. The noise associated with such
records, however, can make interpretation and inter-sample comparison
difficult. We have developed a computational approach that quantitatively
resolves secular (seasonal) change in environmental parameters such as
temperature and salinity with spatial (hard part) variation in isotopic
composition. Output consists of determinations of mean annual isotopic
composition, seasonal range in isotopic composition and variations in
hard part growth rate for any interval of data in an accretionary transect.
The advantage of this method for paleontologists, beyond the obvious paleoenvironmental
applications, is that rate and duration of growth can be approximated
at seasonal to subseasonal levels of resolution for any living or fossil
organism. We have applied this technique to d18O data from
the surf clam, Spisula solidissima, collected from a range of latitudes
and water depths along the Atlantic coast. Quantitative estimates of absolute
growth rates, as well as the proportion of each season represented by
hard part accretion, are derived for each shell with error estimates for
every season of the clam's life. Such information from a suite of individuals
can reveal how growth within a species is affected by changes in latitude,
depth, productivity, and other environmental gradients. In addition, changes
in rate and timing of growth within a lineage are the mainstay of heterochrony
studies, and quantitative methods for assessing such variables through
time in fossil specimens will allow more rigorous testing of hypotheses.
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