NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Fe - Fre
(5/17/01)
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PRELIMINARY RESULTS OF FORAMINIFERAL STUDIES FROM
THE LATE PLEISTOCENE AND HOLOCENE SEDIMENTS FROM THE CHUKCHI BORDERLAND,
ARCTIC OCEAN
FEBO, Lawrence A., and Leonid Polyak, Byrd Polar Research Center, The
Ohio State University, Columbus, OH, USA
Several piston and box cores from a shelf-to-basin transect
are being investigated for paleoceanographic reconstructions as part of
the Shelf-Basin Interaction Program. Reported here are results of foraminiferal
studies from two sites on the Chukchi slope and adjacent Northwind basin.
Foraminifera were sampled every centimeter and counted
in the 63-125 µm, 125-250 µm, and >250 µm size fractions.
Piston core P-6 and box cores B4-B5 were taken on the Chukchi slope (400600
mwd) and show a limited foraminiferal record. Foraminifera are low in
numbers in the Holocene sediments of P-6, presumably due to strong CaCO3
dissolution. However, sediments from the penultimate interglacial, tentatively
correlated to Oxygen Isotope Stage 3, contain significant numbers of foraminifers.
Planktic foraminifers are represented by Neogloboquadrina pachyderma
(left coiling). Prevailing benthic species are Cassidulina teretis
and Eponides tener. High contents of C. teretis in the Arctic
Ocean are shown to be associated with the Intermediate Waters of Atlantic
origin.
Box core B15 from the Northwind basin (2100 mwd) contains
abundant foraminifers in Holocene sediments, which, in combination with
dinocysts, allow us to better characterize the recent environments in
the Chukchi Borderland. Three 14C ages were used to construct
an age model. According to these ages and the lithostratigraphy, the core
spans most of the Holocene and the last deglaciation. Holocene sedimentation
rates are ~1.6 cm/kahigher than most previously studied cores in the deep
western Arctic Ocean. Foraminifers are nearly absent in the deglacial
sediments and increase in abundance starting at ~11 ka. Two abundance
peaks in planktic and benthic foraminifers occur between 67 ka and
~4 ka. Dominant benthic species include Stetsonia horvathi, E.
tener, Epistominella tumidulus horvathi, and Cibicidoides
wuellerstorfi. The combined changes in foraminiferal and dinocyst
abundances and compositions provide a first record of biological productivity
and sea-ice extent over the Chukchi Borderland during the Holocene.
FAUNAL SUCCESSION IN THE VENDIAN (TERMINAL PROTEROZOIC)
DEPOSITS OF THE WHITE SEA REGION, NORTH OF THE RUSSIAN PLATFORM
FEDONKIN, Mikhail A., and Andrei Yu. Ivantsov, Paleontological Institute,
Russian Academy of Sciences, Moscow, Russia
Siliciclastic deposits of the Vendian (Terminal Proterozoic
System) exposed in the White Sea region seem to contain one of the most
complete fossil record of the oldest metazoans. Faunal elements known
separately from the Terminal Proterozoic of the Newfoundland, Great Britain,
Namibia, South Australia, Urals, Arctic Siberia and other regions are
discovered here in a succession. In addition, endemic invertebrates of
complex morphology are discovered as well. Observations of fundamental
importance concerning the time-space distribution of the Vendian fauna
in the White Sea region are made: (a) growth of the taxonomic diversity
of the body fossils and trace fossils upward the succession, (b) stage
pattern in the biodiversity growth, (c) variety of the species' time ranges,
(d) historical change in the paleofaunistic connection of the paleobasin,
and (e) disappearance of the metazoan body fossils and bioturbations in
the sediments of the brackish paleobasins. These facts may reflect the
oldest known metazoan diversification in the marine habitats. At least
six faunal assemblages named after the dominating fossil are identified
in a sequence: Calyptrina-Beltanelloides, Ventogyrus, Inaria, Pteridinium,
Charnia, Yorgia, Dickinsonia lissa. Wide geographic distribution of
these fossil taxa opens the way to the globally correlatable biostratigraphic
units (biozones and stages) to be established. A uranium-led zircon age
555.3 Ma for a volcanic ash by the top of the Charnia fossil assemblage
in the sea cliffs of Zymnie Gory indicates a minimum age of the triploblastic
metazoans because the bilaterian body fossils and trace fossils occur
stratigraphically below. Biodiversity dynamics seem to have not any direct
connection to the carbon isotope excursions in the Vendian ocean.
FOSSIL DECAPOD CRUSTACEANS IN THE HIGH LATITUDES:
PIONEERS AND SURVIVORS
FELDMANN, Rodney M., Dept. of Geology, Kent State University, Kent, OH,
USA; and Carrie E. Schweitzer, Stark Regional Campus, Kent State University,
Canton, OH, USA
Recent studies of paleobiogeographic patterns of decapod
crustaceans in high latitudes strengthens earlier observations, based
upon a limited number of taxa, that the high latitudes were important
sites of origin of families and genera. Ongoing collection of decapods
from both hemispheres reveals that the pattern is much more robust than
previously thought. As many as 42 genera of lobsters, mud shrimp, and
crabs have their earliest geologic occurrence in the high latitudes in
the time interval from the Cretaceous to the Eocene. Several of these
taxa are among the longest-ranging decapods and are represented by extant
species. Geographic and ecologic patterns of most genera reflect diverse
dispersal and adaptive patterns. High latitude, bipolar, amphitropical,
and global distribution patterns are documented, suggesting that decapods
are plastic with regard to latitudinal conditions; photoperiod and water
temperature per se do not appear to limit their geographic distribution.
However, general absence of decapods in post-Eocene Antarctic settings
and their low diversity in high northern latitudes suggests that shallow
water taxa may be excluded from areas characterized by low water temperature
coupled with low seasonal temperature fluctuation. Among taxa known to
have high latitude origins, water depth and substrate preference of many
taxa have changed from shallow water, coarse to medium grained substrates
to deeper water, fine grained substrates; the reverse pattern has not
been observed. Nearly all are confined to normal marine salinities and
none has given rise to fresh water or non-marine descendants. The geologic
record of high-latitude fossil decapod crustaceans is now sufficiently
robust to serve as a test against distributional patterns of more frequently
studied megainvertebrates. Distributional patterns corroborate those illustrated
by other groups but the ecological patterns suggest that decapod genera
may be more versatile than those in groups such as the mollusks, echinoderms,
and bryozoans.
HEMIAUCHENIA, A HIGH-CROWNED BROWSER FROM
FLORIDA
FERANEC, Robert S., Dept. of Integrative Biology, University of California,
Berkeley, CA, USA
Previous studies analyzing the hypsodonty of the genus
Hemiauchenia suggest, due to its high-crowned teeth, that it was
a grazera feeder of monocots, while other studies based on muzzle width
suggest that it was a browser or mixed-feedera feeder of dicotyledons
or both dicotyledons and monocotyledons. The analysis of stable carbon
isotope values from the tooth enamel of Hemiauchenia provides another
method to determine feeding strategy. Florida provides an ideal location
to conduct a study on herbivore feeding strategy because unlike other
regions of the country almost all the present-day dicotyledons use the
C3 photosynthetic pathway, while most of the monocots use the
C4 photosynthetic pathway. The modern flora would
therefore suggest that if Hemiauchenia were a grazer the stable
carbon isotope values of tooth enamel should reflect C4 monocot
feeding (>-2.0). If Hemiauchenia were a browser, the isotopic
value should reflect ingestion of C3 dicots (<-8.0). During
glacial periods, climate and vegetation models suggest further dominance
of C4 monocots, which would result in similar stable isotope
values as expected for the modern flora. The d13C values for
Hemiauchenia from the Blancan through the Rancholabrean in Florida
average more negative than -8.0 , a C3 dicotyledon diet. This
study, which extends from the late Tertiary through the Quaternary, suggests
that Hemiauchenia was predominantly a high-crowned browser over
the past four million years. Because Hemiauchenia is high-crowned
and not a grazer, hypsodonty may not be an appropriate measure of feeding
strategy or habitat type in all circumstances.
THE RELATIONSHIP BETWEEN DIVERSITY AND ABUNDANCE:
AN EXAMPLE FROM THE LOWER-MIDDLE ORDOVICIAN BOUNDARY OF THE GREAT BASIN
FINNEGAN, Seth, and Mary L. Droser, Dept. of Earth Sciences, University
of California, Riverside, CA, USA
The traditional focus of paleobiological and paleoecological
research has been on issues of diversity. The study of diversity trends
provides essential insights into patterns and processes of ecological
and evolutionary change. However, diversity is only one aspect of ecological
systems. An in-depth understanding of paleoecological change also requires
data on depositional environments, biogeography, and abundance. Diversity
and abundance may be decoupled at a variety of temporal, taxonomic, and
geographic scales. Communities with low diversity but high abundance are
well documented as characteristic colonizers of disturbed environments,
and underline the importance of considering abundance and diversity separately.
Analyses of abundance data may lead to recognition of patterns of ecosystem
transformation not apparent from taxonomic diversity data alone. As the
previous example illustrates, this may be particularly true during so-called
"critical intervals." One such interval is the Lower-Middle
Ordovician boundary. A growing body of evidence suggests that the sweeping
evolutionary and ecological changes of the Ordovician radiations are disproportionately
concentrated around this interval. Preliminary data from the boundary
interval of the Great Basin indicate that there is a significant disconnect
between diversity and abundance of brachiopods at this time. A dramatic
increase in the abundance of brachiopods is seen at the Lower-Middle Ordovician
boundary in a variety of environments. This increase in abundance does
not correspond with Ordovician patterns of brachiopod diversification,
and represents an important step towards the establishment of Paleozoic
ecosystem types. There is also evidence, though controversial, of a converse
pattern of decoupled diversity and abundance among trilobites. While they
undergo a major radiation at the base of the Middle Ordovician, the abundance
of trilobite material declines significantly in studied sections. More
study is needed to confirm the geographic and temporal extent of this
trend.
DINOSAURIA AND ASSOCIATED VERTEBRATE FAUNA OF THE
LATE CRETACEOUS CHRONISTER SITE OF
MISSOURI
FIX, Michael F., Dept. of Geology, St. Louis Community College at Florissant
Valley, and Dept. of Physics, University of Missouri St. Louis, St. Louis,
MO, USA; and Guy Darrough, Missouri Ozark Dinosaur Project Inc., Arnold,
MO, USA
The late Cretaceous (Campanian) Chronister site of Southeastern
Missouri stands unique as the only known locality in the state containing
Mesozoic terrestrial vertebrate remains. Fossils occur within a clay that
shows considerable soft sediment deformation due to the close proximity
of a normal fault, on whose downthrown block it has been preserved.
The environment of deposition as indicated by faunal
and stratigraphic evidence, is a body of fresh to brackish water that
was at least occasionally connected to the Gulf of Mexico, which was probably
no more than 20 kilometers away. Allocthonous boulders of Paleozoic rocks
in the clay are probably associated with faulting, but evidence suggests
that parts of the deposit may also represent debris flows.
Abundance of bone is highly variable, but in some parts
of the deposit is high enough to constitute a "bone bed." Many
bones have been damaged by stresses that accompanied deposition, tectonic
sediment deformation, and some are crushed, which could be due to compaction
or to bioturbation. Some bones show evidence of predation or scavenging.
The fauna includes three types of dinosaur that have
been positively identified: Hypsibema missouriensis, which is considered
to be a hadrosaur of uncertain affinities; an undetermined genus of tyrannosaurid;
and an undetermined genus of dromaeosaurid. More problematic is the assignment
of a single phalanx to an undetermined genus of ornithomimid. The deposit
also contains aquatic vertebrates: crocodilians, Leidyosuchus sp.;
turtles (the most common faunal element), Adocus punctatus and
Naomichelys speciosa; a sirenid amphibian, Habrosaurus sp.;
and several fish, including Lepisosteus sp. (gar), an amiid, (bowfin),
and a sparid (sheepshead/porgies). Current excavation by the Missouri
Ozark Dinosaur Project Inc., is being conducted under an enclosure to
keep out water, and utilizes a 60 square meter hanging grid to facilitate
detailed mapping and taphonomic record keeping.
THE FATE AND FUTURE OF THE COLORADO DELTA CLAM:
PALEOECOLOGICAL EVIDENCE FOR ENDANGERMENT, PALEOECOLOGICAL GUIDELINES
FOR RECOVERY
FLESSA, Karl W., Carlie R. Rodriguez, and David L. Dettman, Dept. of
Geosciences, University of Arizona, Tucson, AZ, USA; Miguel A. Tellez-Duarte
and Guillermo A. Avila-Serrano, Facultad de Ciencias Marinas, Universidad
Autonoma de Baja California, Ensenada, BC, México; and Sarah Noggle,
Dept. of Geosciences, University of Arizona, Tucson, AZ, USA
Paleoecological evidence can be used to identify the
cause of species endangerment. Before dams and diversions on the Colorado
River, the mactrid bivalve Mulinia coloradoensis was the most abundant
mollusk inhabiting the tidal flats of the Colorado Delta. More than 90%
of the ~2 trillion shells that make up the islands of the delta are from
this species. Recent surveys of the delta's living fauna encountered only
twelve specimens of M. coloradoensisless than 1% of the shelly
individuals found.
The d18O values in shells of pre-dam M.
coloradoensisare significantly more negative than d18O
values in live-collected shells of Chione cortezi, the most common
bivalve living on the delta today. This indicates that M. coloradoensis lived
in waters much less saline than found today and strongly implicates the
diversion of Colorado River flow as the cause of the population crash
of the species.
Paleoecological evidence can also be used to prescribe
restoration efforts. Although complete resumption of the Colorado River's
flow to its delta would likely restore the population of this species,
this simple prescription is politically unrealistic: all of the Colorado
River's water is now diverted for agricultural or domestic uses in the
US and Mexico. Partial restoration might be feasible if upstream water
users could agree on an "allocation for nature." What percentage
of the river's flow would be needed to restore only a part of the population
of Mulinia coloradoensis? We examined d18O values in
shells from Las Isletas, 50 km south of the river's mouth, where a viable
population existed despite near-complete mixing of river water and normal
Gulf water. Assuming that this population was a source rather than a sink,
the d18O values can be used to calculate the necessary proportion
of river water and the required flow in acre-feet per year.
TESTING CLOCKS: ASSESSING MORPHOLOGICAL, MOLECULAR,
AND PALEONTOLOGICAL DATA ON THE TIMING AND RATE OF EVOLUTION IN MAMMALS
FLYNN, John J., and Sarah M. Zehr, Dept. of Geology, The Field Museum,
Chicago, IL, USA
Dramatic differences of opinion exist regarding the effects
of rates of character evolution on both phylogeny reconstruction and estimating
clade ages/divergence times, and there remain significant conflicts between
molecular and morphological/fossil record inferences. Several lines of
evidence contradict recent molecular clock suggestions of 50100%
greater ages (than derived from the fossil record) for the mammalian orders,
although it is clear that much remains to be done in assessing the cause
of the conflict between these data.
Within Mammalia, the Carnivora are an excellent group
for establishing pattern, tempo and mode of evolution. Our analyses indicate
that multiple lines of evidence (nucleotide sequences, morphology, fossil
record) generally yield congruent phylogenetic results, and combining
them can greatly increase robustness and resolution. But phylogeny-based
analyses of change in molecules indicate wide variance within genes and
across taxa. To test for rate heterogeneity we applied several "relative"
and "absolute" (calibrated by multiple fossil-constrained divergence
ages within the Carnivora) rate tests. Likelihood ratio tests on individual
molecular data sets (mitochondrial cyt b, ND2, ND3; nuclear c-myc,TBG
and transthyretin intron) showed significant rate heterogeneity (p <0.001)
in every one. To focus on which taxa may be responsible for the rate heterogeneity,
Tajima's (1993) 1D relative rate test was performed for all pairwise comparisons
of carnivoran taxa using several outgroupsthese preliminary tests, and
those of Flynn (1996), suggest there is rate heterogeneity among many
carnivoran lineages for all of these molecular data sets. Fossil-constrained
"absolute" rate calculations indicate up to 1.5 orders of magnitude
differences in nucleotide changes/time across the carnivoran radiation.
This may be a general pattern in many groups, but it has been documented
for only a few, and may be of significance for interpreting molecular
clock "inverse calculations" of divergence ages from nucleotide
differences among taxa.
USING TAPHONOMY TO DETERMINE PALEOLOGICAL PARAMETERS
OF THE CHRONISTER LOCAL FAUNA, BOLLINGER COUNTY, MISSOURI
FORIR, Matthew, Dept. of Geology, St. Louis Community College, St. Louis,
MO, USA
The Chronister site yields a localized concentration
of Late Mesozoic (continental Upper Cretaceous) vertebrate fossils in
the southeastern Ozarks of Missouri. The site is isolated from marine
Upper Cretaceous strata of the Gulf Embayment 20 km to the south. It is
considered to be a localized pocket of continental Late Cretaceous clay
preserved in a down dropped block associated with a structurally complex
area near Glen Allen, Missouri. Believed to be Campanian in age from the
similarity of its hadrosaurian material with that of New Jersey, the locality
is the original site of Missouri's first dinosaur, Neosaurus missourensis
Gilmore and Stewart, 1945. Taphonomic observations on the site, interpret
fracturing of concentrated dinosaur bone as green bone fracturing taking
place at a Cretaceous watering hole. Dinosaur bone and chelonian shell
showing evidence of predation in the form of puncture marks also reinforces
the watering hole model. Extensive cherty layers associated with the bone
bearing clays, also exhibit what is interpreted as compression fracturing
of many of the chert cobbles, possibly as a consequence of the migration
of a large number of herbivores. The Chronister site has been difficult
to work not only because of the presence of extensive overburden but also
because associated bone material is highly disarticulated and fragmented,
again suggestive of activity associated with the watering hole model.
Incorporated in with the bone bearing clays are anomalous boulders and
residual chert derived from mid Paleozoic formations that are otherwise
absent from the area. Such boulders, some of which are over one meter
in diameter, are believed to have fallen or slid from cliffs which flanked
the watering hole during the Cretaceous but which today have been removed
by erosion.
BIOSTRATIGRAPHY OF THE ENTELODONTIDAE (MAMMALIA:
ARTIODACTYLA) FROM THE JOHN DAY BASIN, OREGON
FOSS, Scott E., and Theodore J. Fremd, John Day Fossil Beds National
Monument, Kimberly, OR, USA
The temporally continuous units of the John Day Formation
form an ideal basis for biostratigraphic investigations. Entelodont fossils
have been discovered in all four currently recognized members of the John
Day Formation (Big Basin, Turtle Cove, Kimberly, and Haystack Valley).
Datable tuffs are present in all four members. The Turtle Cove and Kimberly
members are further subdivided into thirteen recognizable subunits (units
AM), each of which contain at least one, but usually numerous, datable
primary ash-fall tuff layers.
At least three valid species of entelodonts (Archaeotherium
caninus, A. calkinsi, Daeodon shoshonensis) have been recovered from
the John Day Formation that can be correlated to these subunits, and which,
therefore, may be dated with accuracy. Unlike other depositional regions
of North America, the temporal record of entelodonts is relatively complete
in the John Day. It is possible that there were multiple faunal exchange
events between Asia and North America, and that the John Day species represent
a continuous record of entelodont habitation in North America from at
least the early Oligocene until the earliest Hemingfordian. The biostratigraphic
framework established in the John Day allows the direct correlation of
entelodont taxa across North America and allows a more complete calibration
of entelodont evolution and biogeography world-wide.
CARBON ISOTOPES AND HIGH C4 BIOMASS DURING
THE MIOCENE IN THE GREAT PLAINS, USA
FOX, David L., and Paul L. Koch, Dept. of Earth Sciences, University
of California, Santa Cruz, CA, USA
Changes in mammalian faunas and stable isotope records
during the Miocene suggest global reorganization of terrestrial ecosystems,
with increased abundance of C4 plants (tropical grasses) relative
to C3 plants (trees, shrubs, cool climate grasses) after 8
Ma. In North America, middle Miocene faunas dominated by browsing herbivores
were replaced by late Miocene faunas dominated by grazers, and species
diversity decreased. Because C3 and C4 plants have
distinct carbon isotope signatures, the isotopic composition of tooth
enamel carbonate of mammalian herbivores indicates the proportion of these
plants in the diet. The oldest unequivocal isotopic evidence from enamel
for C4 consumption in North America is at about 7 Ma; older
mammalian herbivores had C3-dominated diets and no species
appear to have had specialized C3 or C4 diets. To
investigate further the changes in North America during the Miocene, we
measured the carbon isotope composition of pedogenic carbonate from the
Great Plains. The carbon isotope composition of pedogenic carbonate reflects
the mix of C3 and C4 plants that grew in the soil,
providing an integrated signature of the entire local flora. To date we
have analyzed 179 samples from seven formations in Nebraska, northwestern
New Mexico, and western Texas that range in age from about 25 to 6 Ma.
Mean composition of these nodules is -6.7 ± 0.70 permil. Assuming
modern atmospheric composition and a +15 permil fractionation between
plant biomass and pedogenic carbonate, C3 and C4
carbonate end members would be -11 and +3 permil, respectively. Thus,
our data imply the persistent presence of up to 40% C4 biomass
throughout the study interval. This pattern contrasts with paleosol records
from Pakistan and South America, ruling out secular changes in atmospheric
composition or C3 fractionation as explanations. Given that
no mammals had specialized diets until after 7 Ma despite the apparent
abundance of C4 plants, our results suggest the possibility
that ecological changes in North American faunas were not driven exclusively
by changes in habitat.
EARLY TRIASSIC PROLIFERATION OF MICROGASTROPODS:
AN UNUSUAL GLOBAL PHENOMENON
FRAISER, Margaret L., Richard J. Twitchett, and David J. Bottjer, Dept.
of Earth Sciences, University of Southern California, Los Angeles, CA,
USA
Estimated at nearly 510 million years long, the
Early Triassic (Scythian) represents the biotic recovery interval following
the most devastating biotic crisis in the history of life, the end-Permian
mass extinction. This biotic recovery interval is the longest following
any mass extinction and was a period of low-diversity, simply structured
communities. Early Triassic invertebrate marine faunas have been characterized
as morphologically simple, opportunistic, unspecialized, and cosmopolitan.
Previously, many primarily qualitative studies have indicated that Lower
Triassic strata are typically dominated by only a few species of bivalves
and tiny snails. In particular, Lower Triassic shallow-water carbonates
composed nearly entirely of microgastropods are a prominent component
of Tethyan strata. This research is the first quantitative study to disclose
how truly unique microgastropod-bearing rocks are to the Early Triassic.
Field work in the western US, Japan and Europe has revealed that microgastropods
are commonly the primary rock-forming allochems in tropical paleolatitude
Lower Triassic outcrops. Similarly, analysis of the literature reveals
references to Lower Triassic carbonates "rich in microgastropods"
or containing "abundant small snails" from every ocean and for
every stage of the Early Triassic. The rarity of microgastropod-bearing
limestones in pre-extinction Permian strata and Middle Triassic strata
demonstrates that the global occurrence of microgastropod-dominated carbonates
in the Early Triassic is indeed an unusual phenomenon. One possible explanation
for this phenomenon is that microgastropods behaved as "biotic recovery
opportunists" during the Early Triassic and thrived in high-stress,
low resource shallow-water carbonate environments during the aftermath
of the end-Permian mass extinction. The dwarfed size of Early Triassic
gastropods could largely be due to the effects of environmental stress
such as decreased primary productivity during the Early Triassic.
THE BEGINNING OF MESOZOIC BIVALVE REEFS: EARLY
JURASSIC "LITHIOTIS" FACIES BIOHERMS
FRASER, Nicole M., and David J. Bottjer, Dept. of Earth Sciences, University
of Southern California, Los Angeles, CA, USA
Prior to the Cretaceous reef-building rudists, the Early
Jurassic is notable for bioherms constructed by a unique group of large
aberrant bivalves that collectively form the "Lithiotis"
facies: Lithiotis, Gervelleioperna sp., Lithioperna
sp., Cochlearites and Mytiloperna. These bivalves dominated
nearshore tropical ecosystems of the Early Jurassic (Pliensbachian) and
abruptly went extinct at the end of the Early Jurassic (Toarcian). The
dearth of reefs constructed by colonial organisms and the preponderance
of filter-feeding bivalves in nearshore tropical environments is a common
feature of later Mesozoic environments, beginning in the Early Jurassic
and culminating in the large Late Cretaceous rudist reefs. "Lithiotis"
facies bioherms in Oregon, California, Italy and Morocco have been used
in this study. Line-intercept transects, bulk sample collection and species
identification have been completed for each site. Original aragonite was
preserved in some Italian specimens; d18O, d13C
and Mg/Ca analyses are currently being performed on these specimens to
quantitatively assess paleoenvironment. While most of the "Lithiotis"
bioherms in Oregon and California are relatively low-diversity with minor
constituents of nereinid gastropods and red algae, the Moroccan and some
Italian sites exhibit higher diversity with corals, sponges and brachiopods.
The increased presence of bivalve-constructed reefs in the Early Jurassic
could have resulted from increased nutrient delivery to the shelves. The
consequent increased rates of bioerosion and algal growth allowed filter-feeding
bivalves to outcompete stenohaline groups such as scleractinians. An alternate
hypothesis for the occurrence of bivalve constructed bioherms is that
these organisms are adapted to euryhaline environments. While this explanation
may be appropriate for the Oregon and some of the Italian sites, it is
inadequate to explain the occurrence of "Lithiotis" facies
bivalves with stenohaline organisms such as corals and sponges in Morocco
and other Italian sites.
SPECIES-LEVEL EVOLUTIONARY PATTERNS IN NEOGENE
STROMBIDS FROM THE DOMINICAN REPUBLIC
FREIHEIT, Jim, and Dana H. Geary, Dept. of Geology and Geophysics, University
of Wisconsin, Madison, WI, USA
Due to their determinate growth patterns, gastropods
of the family Strombidae are particularly suitable for evolutionary and
ecological studies involving size-related trends of morphological change.
Geary (1991) made an intriguing observation regarding strombids of the
West Atlantic; starting in the Pliocene, they seem to have gotten bigger.
This observation applies both within species (larger average adult size)
and to the genus Strombus as a whole (smaller species go extinct;
new species are larger than the former average). This implies widespread
selective pressure against small size but the details of such size-related
selection remain elusive.
We have examined a cluster of morphologically intergrading
strombid species from the Mio-Pliocene of the Cibao Valley in the Dominican
Republic in order to establish both the nature of the relationships between
these species and what patterns of morphologic change they exhibit through
time. End members of this group are the species Strombus bifrons
and Strombus proximus. Morphometric analysis reveals a pattern
of increasing size and robustness through time for individuals corresponding
most closely to S. proximus. Preliminary results suggest a similar
trend for S. bifrons. Future research will focus on unambiguously
establishing this trend and on clarifying the evolutionary relationships
between these groups.
APPRAISING THE SIGNIFICANCE OF COMPLEX ASSEMBLAGES
AND DATA DEFRAGMENTATION: AN EXAMPLE FROM THE VOLCANICLASTICS OF EASTERN
OREGON
FREMD, Theodore J., John Day Fossil Beds National Monument, Kimberly,
OR, USA
Many stratigraphically complex basins are globally significant
in terms of local preservation of long-term processes and events. These
are qualitatively characterized by sequences of well-preserved biotas
found in association with isochronous index strata that can be correlated
with deposits elsewhere. Comparative assessment of the significant features
of data-rich basins demonstrates that among such classic Tertiary settings
as the Siwaliks and the Bighorn Basin is the lesser-known John Day Basin.
The remarkable temporal continuity of the Tertiary deposits
in eastern Oregon was first recognized one hundred years ago by J.C. Merriam
of the University of California, Berkeley. However, it was only after
Merriam's development of an interdisciplinary group known as, "The
John Day Associates," that it was realized that no region in the
world shows more complete sequences of Tertiary land populations, both
plant and animal, than the John Day Formations. We now realize that these
series of strata are exceptional not only in terms of temporal continuity,
but in that they also contain multiple, diverse localities formed in laterally
variable intrabasin depositional environments, which allows comparison
of time-equivalent paleobiomes.
Basins like the John Day are warehouses of stratigraphic
information, indispensable for accurate phylogenetic and ecologic studies.
Many of the data sets needed for complete analyses and comparative study
of such areas are fragmented, however, as a result of non-integration
of varied disciplines into a cohesive research framework, unsystematic
institutional data storage, and overlooked inter-basin relationships.
As a result, there are misconstructions of the quality of the fossil record
appearing in overall tabulations, or a failure to recognize correlative
units proximal to basin margins. Defragmentation can be achieved for long-term,
interdisciplinary analysis of these basins and their margins when paleontological
studies, data collection, and storage are performed with the big picture
in mind.
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