NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Sa - Sk
(5/22/01)
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BEST-FIT INTERVALS: MEASURES OF THE RESOLVING
POWER OF PALEONTOLOGICAL FIRST- AND LAST-APPEARANCE EVENTS
SADLER, Peter M., Dept. of Earth Sciences, University of California,
Riverside, CA, USA
The locally preserved range of a fossil taxon includes gaps that result
from the patchy distribution of organisms and the incomplete preservation
or recovery of fossils. The same factors cause stratigraphic sections
to underestimate the length of taxon ranges. Because the effects vary
with taxon and location, stratigraphic sections contradict one another
concerning the sequence of first- and last-appearance events. Like the
gaps within a range, the contradictions between sections may be used to
gauge the reliability of range ends and test the significance of preserved
patterns of extinction and origination. Probabilistic confidence intervals
built from gap sizes tend to treat short-lived taxa like long-lived taxa
with poorly preserved ranges. Short ranges provide too few gaps for useful
analysis, but their position in sequence is not compromised.
Computer algorithms resolve the contradictions between sections by finding
a sequence of range-end events that minimizes the net misfit with all
the local range charts. Operationally, the task is analogous to finding
the most parsimonious cladogram. Usually the solution is not unique; more
than one sequence of events may share the best fit. For each event, resolving
power can be quantified as a "best-fit interval"the range of
positions in sequence that the event occupies in the full set of equally
best-fit sequences. Overlapping best-fit intervals indicate events whose
timing cannot be separated by the fossil record. Culling the available
events down to those whose best-fit intervals do not overlap produces
a maximum consensus sequence that typically exceeds the temporal resolution
of traditional biostratigraphic zonation by a factor of five to ten. Considering
all the best fit intervals leads to standing diversity curves that are
free of the artifacts of zonal subdivisions.
TRACING THE FATE OF AVALONIA: MICROPALEONTOLOGICAL
ANSWERS TO A GEOLOGICAL CONUNDRUM
SAMUELSSON, Joakim, Sédimentologie et Paléontologie, UPR
du CNRS Géosciences, Université de Rennes 1, Rennes Cedex,
France; and Marco Vecoli, Institut für Geologische Wissenschaften,
MLU Halle/Wittenberg, Halle (Saale), Germany
Most early Paleozoic palynomorphs, especially the acritarchs and the
chitinozoans, were probably planktonic. Consequently, the spatial distribution
of those palynomorphs was essentially controlled by climatic factors,
i.e., indirectly by paleolatitude and paleocurrents. Thus, at least during
late Arenig and Llanvirn times (late Ibexian and middle Whiterockian in
North American terms), acritarchs and chitinozoans can be effectively
used as paleogeographic indicators. Although of enigmatic biological affinities,
the distribution patterns of chitinozoans are relatively well understood,
and consequently, they are especially useful in a paleogeographic context.
The microcontinent Avalonia was part of the high-latitude Gondwana paleocontinent
until it drifted off in Middle Ordovician times. Subsequently, Avalonia
started to collide with Baltica probably in the Ashgill (late Cincinnatian),
and with Laurentia in the Early Silurian. Thus, as an a priori
hypothesis, chitinozoan faunas preserved in the oldest rocks of Avalonia
ought to be similar to the contemporary cold-water Gondwana faunas. In
younger rocks a successive incorporation of chitinozoans typical of middle
latitudes as on Baltica and of the low latitudes as on Laurentia ought
to take place. This pattern is already established for the benthic macrofauna,
where in Caradoc (late Whiterockian to early Cincinnatian) times the Avalonian
faunas started to mix with those of Baltica. A number of Avalonian successions
analyzed for their chitinozoan faunas clearly reflect the a priori
suggestion above: the oldest strata yielded a typical north Gondwana chitinozoan
fauna. In the early Late Ordovican, an influx of chitinozoans also common
in Baltoscandia is evident. Chitinozoans recovered from the inferred northern
end of Avalonia support the idea of a narrowing Iapetus Ocean in latest
Ordovician times. Furthermore, besides mirroring the drift history of
Avalonia, the chitinozoan faunas can also be used together with coeval
acritarchs to chronostratigraphically constrain the Avalonia-Baltica collision.
MORPHOLOGIC EVOLUTION OF CONGERINE BIVALVES
IN THE LATE MIOCENE LAKE PANNON OF CENTRAL EUROPE
SANDERS, Hilary, and Dana H. Geary, Dept. of Geology and Geophysics,
University of Wisconsin, Madison, WI, USA; and Imre Magyar, MOL Hungarian
Oil and Gas Company, Budapest, Hungary
Covering parts of Central and Eastern Europe from approximately 12.5
to 4.0 million years ago, Lake Pannon serves as an exemplary "evolutionary
laboratory." The stratigraphy, paleogeography, and paleoenvironments
of Lake Pannon are well documented, and its deposits contain a diverse
fauna recording an unparalleled endemic radiation of brackish and freshwater
molluscs. The unique dreissenid bivalve, Congeria, is abundant
in Pannonian deposits. This study examines patterns of Congeria's
morphologic change through time and space. Museum specimens were supplemented
with new field collections and investigated via outline analysis (eigenshape
method), traditional morphometric techniques, and multivariate statistical
analysis.
The morphologic evolution of the C. rhomboidea lineage is characterized
by a shift from thin-shelled, ovoid forms, through intermediate morphologies,
to robust, angular forms. Two species-level transformations occur in this
lineage: C. praerhomboidea -> C. rhomboidea -> C. alata.
Early representatives of the C. balatonica lineage are limited
to thin-shelled, triangular forms with diminutive byssal openings. Over
time, morphospace occupation by C. balatonica expanded to include
more irregular, thickened forms displaying prominent byssal openings,
with intermediate morphologies present. Both the morphologic diversification
of C. balatonica and the turnover from C. praerhomboidea
to C. rhomboidea are constrained stratigraphically within the Limnocardium
decorum biozone (ca. 8.59.0 Ma), an interval of continued northwest-to-southeast
deltaic progradation during which the lake shrank to half its former size.
Coincidence of these events suggests that environmental changes influenced
evolutionary change within Congeria.
HOLOCENE PALEOPRODUCTIVITY IN THE NORTHWESTERN
PACIFIC DETERMINED BY FORAMINIFERAL ASSEMBLAGES IN A FJORD OF WESTERN
VANCOUVER ISLAND, BRITISH COLUMBIA
SCHELL, Trecia M., Centre for Marine Geology, Dept. of Earth Sciences,
Dalhousie University, Halifax, NS, Canada; and Audrey Dallimore, Dept.
of Earth Sciences, Carleton University, Ottawa, ON, Canada
Scientific interest in the evidence linking oceanographic processes and
fish population dynamics has increased since the highly publicized Pacific
salmon collapse off the west coast of British Columbia and the collapse
of the Atlantic cod fishery. To study this problem in a prehistorical
context, Effingham Inlet was used as a study site; it is a 17-km long
by 1-km wide fjord located at the apparent northern extreme of the California
Current with a connection with the open ocean. Historical fish catch data
suggest a large-scale expansion and contraction of this favorable habitat
due to the large-scale changes in oceanic climate, i.e., upwelling and
ENSO (El Niño Southern Oscillation).
Foraminiferal assemblages may be used as proxies for paleoclimatic and
paleoceanographic conditions such as temperature, oxygen, salinity, and
organic material production. Various combinations of those factors may
indicate periods of enhanced and suppressed upwelling events, and the
associated productivity. Once the paleoceanography of a region is understood,
it may serve as a proxy for the suitability of a paleohabitat for a particular
pelagic fish species. The restricted nature of Effingham Inlet, a fjord
on western Vancouver Island, British Columbia is an ideal primary study
site with its deep basins, shallow sills, laminated sediments and low
sediment oxygen content, to provide an excellent sedimentological and
paleobiological preservation record of these upwelling and other ocean-climate
events.
The presence low oxygen tolerant foraminiferal faunas in the inner basin
indicate that anoxic conditions predominate, but are not permanent. In
addition, there are several discrete pulses of Buccella frigida
followed by an increase in Fursenkoinia fusiformis abundance, indicating
that there have been several incidents of inputs of freshly marine waters
into the inlet (possibly upwelling events) followed by decreases in oxygen
levels, presumably caused by high productivity events triggered by upwellings.
HEAPS OF ECHINOIDS IN A PENNSYLVANIAN ECHINODERM
LAGERSTÄTTEN: IMPLICATIONS FOR FOSSILIZED BEHAVIOR
SCHNEIDER, Chris L., Dept. of Geological Sciences, University of Texas
at Austin, Austin, TX, USA
An exceptionally preserved echinoderm community from the Winchell Formation
at Brownwood, north-central Texas contains several thousand individuals
of a large species of Archaeocidaris. Other fossils are less abundant
and include crinoids, other echinoids, brachiopods, encrusting bryozoans,
fenestellid bryozoans, edrioasteroids, and asterozoans. Pteridosperm and
lycopsid leaf debris is abundant.
This recurring community is preserved along several horizons in a, sulfur-rich,
channel-shaped, near-shore black shale. Fossils are complete and only
slightly disarticulated with elements remaining in close association,
indicating that decay occurred before final burial. Though some echinoids
are overturned, there is little evidence of disturbance by scavengers
or transport mechanisms.
Hundreds to thousands of Archaeocidaris echinoids occur within
lagerstätten horizons. Within these aggregations, archaeocidarids
cluster into smaller, dense groups, sometimes with overlapping spines.
Extant echinoids have also been observed aggregating, often clustering
similarly to these Pennsylvanian archaeocidarids. These modern echinoid
aggregations have been interpreted as feeding, defensive, or spawning
behavior. Because the echinoids and other fossils seem undamaged by predation,
it is unlikely that the archaeocidarids represent a defensive aggregation.
The Archaeocidaris echinoids at this locality were probably aggregating
to spawn or to feast on the abundant plant debris. The rarer echinoid
species were most likely present to scavenge leaf matter, as their distribution
is much more scattered.
Unusual black material full of crinoid fragments is found within the
tests of some archaeocidarids or oozed out between their interambulacral
plates. This is interpreted as evidence of final meals. Crinoids are rare
at this locality, so these remains may represent crinoids that were consumed
elsewhere by the echinoids. Because of the abundance of plant debris,
leaf matter may have also been a significant part of echinoid diet before
death.
PHYLOGENETIC REVISION OF THE CARDIINAE (BIVALVIA,
CARDIIDAE): INDIAN OCEANTROPICAL AMERICAN DISJUNCT DISTRIBUTIONS AND NEW
ZEALANDSOUTH AMERICAN BIOGEOGRAPHIC
CONNECTIONS
SCHNEIDER, Jay A., Dept. of Geology & Geophysics, University of Wisconsin,
Madison, WI, USA
A phylogenetic analysis of Cardiinae finds it to be paraphyletic. Cardiinae
is therefore restricted to Cardium, Bucardium, Vepricardium, Dinocardium,
Planicardium, Chesacardium, Acanthocardia s.s., A. (Rudicardium) and
Schedocardia. The closest relatives of Cardiinae are the Eocene
Sawkinsia and the "CFTL" clade containing Plagiocardium,
Maoricardium, Clinocardiinae, Fraginae, Lymnocardiinae and Tridacninae
(giant clams). The remaining taxa that had been placed in Cardiinae form
a monophyletic group, sister taxon to Sawkinsia + Cardiinae + CFTL;
a new subfamily is erected for this group. This new taxon contains Orthocardium,
Loxocardium, Europicardium, Hedecardium s.s., H. (Titanocardium) and
H. subgen. n., Agnocardia and Afrocardium. Many species
in this new taxon had simply been (and continue to be) placed in Trachycardium
(subfamily Trachycardiinae) based on superficial examination of shells.
The only extant subtaxa in the new subfamily are Afrocardium and
Europicardium. Hedecardium s.l. was not restricted to New Zealand
as usually argued but was present in Myanmar and Australia, as well as
being represented in South America by H. subgen. n. Renewed studies
of the long-ignored marine invertebrate Cenozoic faunas of South America
will yield additional examples of taxa long thought to be New Zealand
endemics. The only other member of the new taxon with representatives
in the western hemisphere is the extinct Agnocardia. Agnocardia's
closest relative, Afrocardium, long misconstrued as a fragine,
has been recorded only in Recent faunas, usually from the Indian Ocean.
This disjunct biogeographic distribution is found to be a function of
a century of misidentification of fossil and Recent species, for species
attributable to Agnocardia occur in the Paleogene of Europe and
Africa; likewise, species attributable to Afrocardium occur from
the Eocene to Pliocene of Europe and Africa. A greater awareness of modern
taxonomy of both fossil and Recent forms is necessary to avoid constructing
erroneous biogeographic distributions and phylogenetic hypotheses.
CLAM-RING TIME-SERIES: A NEW METHOD FOR HIGH-RESOLUTION
ENVIRONMENTAL RECONSTRUCTION
SCHÖNE, Bernd R., Dept. of Geosciences, University of Arizona, Tucson,
AZ, USA
Modified dendrochronological methods can improve the temporal resolution
of environmental reconstruction from bivalve mollusk shells. Mollusks
grow by periodic accretion of skeletal material leaving daily, fortnightly
and annual growth increments bordered by distinctive growth lines in their
shells. Cross-dating individual growth increment time-series can help
to find and verify overlapping life spans among different specimens from
a given region. "Clam-ring" chronologies from individuals with
overlapping life spans can be strung together to form master chronologies,
which comprise much longer time periods than individual life spans. Master
chronologies provide a source for the analysis of longer-term environmental
periodicities and fluctuations. We measured annual growth increment widths
in 67 Chione cortezi, C. fluctifraga and C. californiensis
specimens collected alive at different times in the 1990s in the intertidal
zone of the northern Gulf of California, Mexico. The specimens average
seven to eight years in ontogenetic age. Standardized growth index time-series
calculated from each specimen were cross-dated and strung together. Inter-annual
growth patterns in specimens with overlapping life spans are strikingly
similar. The Chione master chronology covers the period from 1982
to 1999. 75% of the variability in growth rates during the past ten years
can be explained by water temperature and salinity. This study demonstrates
that even relatively short-lived bivalve mollusks can be used to establish
master chronologies, which reveal high-resolution environmental information
over periods that are longer than the individual mollusk's life span.
THE TERTIARY HISTORY OF NORTH AMERICAN MEGAFOSSIL
CONIFERS: THE FEW, THE PROUD, AND OFT TIMES NEGLECTED
SCHORN, Howard E., and Diane M. Erwin, Museum of Palentology, University
of California, Berkeley, CA, USA
The modern coniferous (s.l.) flora of the Northern Hemisphere
consists of 38 genera (~350425 species), 36 exclusively Northern
Hemisphere, and two podocarp genera more typical of the Southern Hemisphere.
The greatest concentration of extant genera in the Northern Hemisphere
is in Asia, s.l. (34 genera, 89%), North America (NA) has three
(8%) restricted genera, and Europe-North Africa has one (3%). Some 30
(79%) of the extant genera were present in NA during some part of the
Tertiary. Two extinct entities, not including form genera, are also recognized.
As in all walks of paleobotanical life, difficulties in identification
of similar sterile and/or poorly preserved material, plus unwarranted
misidentifications, plague our historical analyses.
Major events in the Tertiary history of North American conifers closely
track the changing physiographic/climatic histories of the area. At a
first level approximation we recognize four intervals of development,
viz., the first three that document increasing diversity by "step-wise"
addition of genera, and the fourth, leading to our modern forests, is
one of loss of generic diversity by extirpation. Period I, ~6550
Ma, low generic diversity of "archaic" conifers presently mono-
or oligotypic, largely deciduous, individual taxa widespread, inhabited
low elevation sites. Period II, ~5032 Ma, with the exception
of the loss of the deciduous Mesocyparis, the archaic genera continue.
More elevated sites of deposition became available and document the spread
and diversification of additional pinaceous and cupressaceous genera into
North American forests. Period III, ~3212 Ma, all previous
genera continue and additional extant, and one extinct, genera are added.
This interval, with its great physiographic diversity, and diverse yet
equable moist climate, saw the largest number of extant conifer genera
in North America, rivaling that of present Asia. Period IV, <12
Ma. Following the previous "additive" periods, the later Tertiary
in North America is a time of loss of generic diversity, decreasing from
the previous high, to the present 16 genera, in a period of ~23
Ma.
PRECURSOR EVENTS OF MEGATHRUST EARTHQUAKES AS DETERMINED
FROM COASTAL MARSH DEPOSITS ON THE WEST COAST OF THE UNITED STATES USING
FORAMINIFERA AS INDICATORS
SCOTT, David B., and Andrea Hawkes, Centre for Marine Geology, Dalhousie
University, Halifax, NS, Canada; and Jere Lipps, Museum of Paleontology,
University of California, Berkeley, CA, USA
We present results from two areas on the West Coast of the United States
where large megathrust earthquakes are known to occur. They have been
shown to occur in several places with frequencies of 200- to 500-year
repeat times. However, we have determined, using a combination of benthic
foraminifera and thecamoebians, that there are detectable precursor events
that appear to happen 25 years before a major fault break. This
is indicated by assemblages of both thecamoebians and foraminifera that
suggest small (30 cm or less) subsidence events just prior to a major
earthquake. The first indication was from an historical event, the great
1964 Alaska earthquake, where the exact sequence of events was known and
there were coastal deposits with the subsidence event preserved. Secondly,
we examined sequences from Netarts Bay, Oregon where previous workers
had suspected that they had seen precursors using diatoms as indicators.
In Netarts Bay the event occurred in a salt marsh deposit and showed a
definite 30 cm subsidence just prior to major quakes and tsunamis. In
Alaska, a forest fauna of thecamoebians changed to a slightly brackish
fauna; this sequence was Pb210 dated by British colleagues to show that
the 1 cm interval before the quake was not more than 5 years. If this
phenomenon can be proven in other areas, it will give planners and managers
a new tool for dealing with catastrophic earthquakes by providing a long
lead-time to react before the event occurs.
A NEW FOSSIL MAMMAL ASSEMBLAGE FROM THE SOUTHERN
CHILEAN ANDES: IMPLICATIONS FOR GEOLOGY, GEOCHRONOLOGY AND TECTONICS
SEARS, Karen E., Committee on Evolutionary Biology, University of Chicago,
and Dept. of Geology, Field Museum of Natural History, Chicago, IL, USA;
John J. Flynn, Dept. of Geology, Field Museum of Natural History, Chicago,
IL, USA; Michael J. Novacek, Div. of Vertebrate Paleontology, American
Museum of Natural History, New York, NY, USA; and Daniel Frassinetti,
Depto. de Geología, Museo Nacional de Historia Natural, Santiago,
Chile
Paleontological reconnaissance beginning in 1986 led to the discovery
of a new and diverse fossil terrestrial mammal assemblage of Santacrucian
SALMA (latest early Miocene) age in the southern Andes of Chile. This
is the westernmost high latitude mammal fauna in South America and was
the first discovery of a diverse (36 taxa) fossil mammal assemblage from
Chile in nearly a century. The mammal fauna includes several marsupial
species, most notably a very diverse assemblage of Paleothentes
that includes a new species. The appearance of Paleothentes in
the southern Chilean Andes extends their geographic range. In addition,
the rich Paleothentes fauna shows some interesting morphological
patterns that bear on species recognition. The discovery of a new Santacrucian
fauna also allows refinement of the early to middle Miocene SALMAs, bearing
on the controversial Friasian as typified within Chile.
The fossil mammals occur in a terrestrial sequence that conformably overlies
a marine section of late Oligocene to early Miocene age. The marine-terrestrial
sequence, and the fossils therein, bear significantly on theories concerning
the extent of the late Tertiary Patagonian epicontinental seaway, and
the onset of later Cenozoic phases of uplift in the southern Andes. Uplift
in this region likely was initiated by the Santacrucian SALMA (1617.5
Ma), although it remains uncertain whether the major uplift occurred in
two phases or one. These discoveries support and expand upon previous
suggestions that there are sharp paleogeographic, geologic and tectonic
contrasts north and south of the Lago General Carrera/Lago Buenos Aires
Area. Minimum estimates of uplift rate are 0.050.07 mm/yr (to as
high as 0.22 mm/yr). These rates are comparable to those from other parts
of the Andes. The timing and location of uplift may be correlated with
major plate tectonic events nearby (impingement of the CMTJ and subduction
of the East Pacific Rise).
INTERPRETING THE RECORD OF DINOSAUR EXTINCTION
IN THE HELL CREEK FORMATION: AVOIDING SIGNOR-LIPPS AND OTHER BIOSTRATIGRAPHICAL
PROBLEMS
SHEEHAN, Peter M., Milwaukee Public Museum, Milwaukee, WI, USA; and David
E. Fastovsky, University of Rhode Island, Kingston, RI, USA; and Claudia
Barreto, University of Wisconsin-Milwaukee, Milwaukee, WI, USA
The Hell Creek Formation is renowned for abundant dinosaur fossils, but
only a few thousand individuals have detailed stratigraphic documentation.
Analysis of this record is problematic because the Signor-Lipps Effect
(SLE) increases with decreasing sample size. The SLE can be addressed
statistically, but other approaches avoid the SLE effect entirely.
The extinction debate centers on two hypotheses: (1) Dinosaurs became
extinct gradually, over either ~10 MY, ~2 MY or many thousands of years.
Dinosaurs may have been extinct before the Chicxulub impact, suffered
a final blow at the impact, or survived the impact. (2) Dinosaurs became
extinct over a brief interval after the impact event.
One way to avoid SLE is to determine if communities were changing through
the Hell Creek Formation. If dinosaurs were becoming extinct over 2 to
10 MY, communities should show evidence of changes analogous to changes
in modern communities when they are disrupted. Two surveys of Hell Creek
Formation dinosaur fossils indicate that the dinosaurian components of
communities were stable through the ~ 2 MY of HCF time. Another way to
avoid SLE is to compare dinosaur abundance at various intervals through
the Hell Creek Formation. No trend of decreasing abundance has been found,
although the record is highly variable from level to level. Additionally,
although a precise record of the position of fossils in the Hell Creek
Formation has been made, range charts constructed as though they present
standard biostratigraphic data do not maintain superpositional relationships.
Dinosaurs are so rare that individual fossils at a given level may be
a kilometer or more apart. Deposition was sporadic with occasional floods,
long intervals of soil formation, and occasional steams meandering over
the landscape eroding older beds. As a result, over these distances, individual
beds precisely the same distance below a marker level (such as the palynological
K/T boundary) may be of very different ages, thus removing superpositional
control.
FAUNAL SHIFT ACROSS THE PERMIAN-TRIASSIC BOUNDARY
IN SOUTHERN TIBET
SHEN, Shuzhong, and Changqun Cao, Nanjing Institute of Palaeontology
and Geology, Chinese Academy of Sciences, Nanjing, China
Little knowledge is available on whether the end-Permian mass extinction
is paleogeographically varied or not in terms of timing and magnitude.
An investigation into two Permian-Triassic boundary sections suggests
a closely comparable pattern between Southern Tibet, South China and other
areas. The base of the Triassic in both sections is indicated by the first
appearance of Otoceras and Hindeodus parvus. At the Selong
Xishan section, the Permian-Triassic transitional sequence consists of
the Coral Bed, the Caliche Bed, the Waagenites Bed and the Otoceras
Bed. The Coral and Waagenites Beds are characterized by containing
abundant brachiopods, corals and bryozoans. These Permian-type benthic
faunas were replaced by numerous ammonoids in the overlying Otoceras
Bed. This biotic shift at the Selong Xishan section appears to have
been accompanied by a major and rapid transgression event within a decimeter
interval beneath the Permian-Triassic boundary, as evidenced by the occurrence
of framboidal pyrites, a lithologic shift from grainstone to packstone
and a shift from brachiopod-dominated to ammonoid/bivalve-dominated community.
Associated with this transgression event and biotic changeover, a dramatic
drop in d13C value from +3.2 in the Caliche Bed to -2.89 per
mil in the Waagenites Bed is detected. In the Qubu section near Mt. Everest,
there is about 50-meter shale and siltstone between the Otoceras
Bed and the Qubuerga Formation with numerous Permian brachiopods. No fossils
were found from the lower pale gray siltstone but some plant fragments;
and ammonoids appear in the upper dark or varicolored shale. This part
represents a rapid regression-transgression event of the latest-Changhsingian
and is comparable to the Caliche Bed and the Waagenites Bed at the Selong
Xishan section. This event and the carbon isotopic drop are widely known
in carbonate Permian-Triassic sections in South China and other areas.
ANALYZING EVOLUTIONARY TRENDS IN NON-MAMMALIAN
SYNAPSIDS: SCALE DEPENDENCE AND STRATIGRAPHIC VS. PHYLOGENETIC PERSPECTIVES
SIDOR, C.A., Dept. of Paleobiology, National Museum of Natural History,
Smithsonian Institution, Washington, DC, USA
Evolutionary trends are commonly discussed with regard to the fossil
record of non-mammalian synapsids (e.g., reduction of the post-dentary
bones), but despite its widespread use, the term is used in different
and sometimes conflicting ways. Stratigraphic and phylogenetic trends
should be kept distinct conceptually, although congruent patterns can
increase our confidence that they reflect a real underlying phenomenon.
Simulation studies have demonstrated that unbiased, lineage-level evolution
can produce clade-level trends under certain boundary conditions. Distinguishing
among different types of trends, and postulating different mechanisms,
is therefore critically tied to the hierarchical scale at which persistent
directionality can be resolved.
Here, I quantify some of the morphological changes that occurred in the
evolution of the synapsid lower jaw during the late Paleozoic and early
Mesozoic, and address several previously proposed hypotheses concerning
the nature and magnitude of morphological trends. I gathered measurements
and discrete character data from the mandibles of 108 fossil synapsid
taxa, including four linear measurements, two areas, and 82 qualitative
characters. The stratigraphic range of each taxon was binned into one
or more of 18 age ranks spanning Pennsylvanian though Jurassic time. Phylogenetic
data included each taxon's clade rank and the number of branch points
passed from the root of the synapsid cladogram used. Analyses were performed
at multiple scales (e.g., Synapsida, its subclades that include mammals,
and its subclade side-branches that do not include mammals). The results
of these analyses show a complex pattern of both passive and active trends.
For example, theriodonts as a whole show a persistent trend for increasing
the size of the dentary, but analyses focusing on its subgroups (gorgonopsians,
therocephalians, or different cynodont families) fail to show a corresponding
pattern. Assessing the prevalence of trends in the synapsid fossil record
will require reinvestigating long-held views with new techniques.
A NEW PALEOBOTANICAL DATABASE INITIATIVE
SIMS, Hallie J., and Scott L. Wing, Dept. of Paleobiology, National Museum
of Natural History, Smithsonian Institution, Washington, DC, USA
Beginning in 1979, Niklas, Tiffney, and Knoll published a series of key
papers documenting Phanerozoic land plant diversity based on a compilation
of stratigraphic ranges from the paleobotanical literature. Although these
authors identified omissions and sampling biases underlying their results,
the work provided a first assessment of temporal patterns in diversity.
Several subsequent studies have focused on narrower temporal intervals
and produced significantly different patterns. More recent work has highlighted
the value of locality-based occurrence data in identifying geographic
and environmental gradients in macroevolutionary patterns. In addition,
such occurrence data make it possible to identify and minimize effects
of a range of sampling biases, including variation in sampling effort,
preservation rate, and amount of available rock record. The Paleobotany
Working Group (part of the Paleobiology Database; see http://flatpebble.nceas.ucsb.edu/public/)
has begun a project to enter lists of taxonomic occurrences (and abundances
where available) for Phanerozoic land plant localities. Data are drawn
from the primary literature, museum collections, and unpublished fieldwork.
As a group of specialists (currently fifteen members), we hope to update
stratigraphic information and build a table of valid species, genera,
and their synonyms. By making the data publicly available as a web-searchable
database, the paleobotanical community will be invited (and perhaps incited?)
to identify omissions and errors. The group is exploring several scientific
goals, including producing a sampling standardized plant diversity curve,
assessing changes in within-community diversity over time, and exploring
trends in morphological evolution. However, the lists of valid taxa and
occurrence lists from well-defined localities, vetted by specialists,
can form building blocks for a wide range of research projects. We hope
that this initiative will gain momentum within the community to maintain
and contribute to a public repository of high-quality paleobotanical data.
ISOTOPIC ANALYSIS OF THE CHANDLER AND SAFFORD (CENTRAL
ARIZONA) PROBOSCIDEAN FOSSILS
SKAFF, Andria L., and Carol M. Tang, Dept. of Geological Sciences, Arizona
State University, Tempe, AZ, USA
Recently, two proboscidean fossils have been found in central Arizona
and will be analyzed for carbon and oxygen isotopes. Many proboscidean
fossils have been discovered in southern and northern Arizona, but few
have come from the central part of the state, making these finds significant.
The remains of a Pleistocene Mammuthus columbi fossil were discovered
in Chandler, Arizona in the Queen Creek floodplain deposits during the
construction of a housing development. Various postcranial elements, both
tusks and several molar fragments were recovered. The molars are so fragmented
that it is impossible to determine the age of the individual, but the
long bone epiphyses are fused implying that it was an adult at the time
of death.
The remains of a Pliocene Rhycothere (Proboscidea: Gomphotheridae) were
discovered in the badlands of the 111 Ranch locality near Safford, Arizona.
The fossils consisted of several postcranial fragments and most of the
right mandible containing two well preserved molars. The anterior molar
was completely worn and parts had probably already fallen out at the time
of death, and the posterior was partially worn with several unworn lophs.
Trefoil patterns in the posterior molar and the high angle of the jaw
symphysis allowed for identification. Molar fragments from another individual
were also found at the locality and will be analyzed as well.
Using standard sampling techniques employed in previous isotopic studies
of fossil proboscideans, samples of dentine and enamel were taken from
the molars and tusk using dental drill bits in a flexible shaft drill.
Five samples were taken from each molar or tusk in the least fragmented
areas. Since proboscideans employ accretionary growth on their teeth,
this should provide us with high-resolution information regarding the
paleoenvironmental conditions present in the areas they inhabited and
the life history of the individuals.
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