NAPC 2001
June 26 - July 1 2001 Berkeley, California
Abstracts, Ha - Has
(5/17/01)
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POINTED ENDS IN SPACE AND TIME: THE PHYLOGENETIC
AND GEOGRAPHIC DISTRIBUTION OF LABRAL AND COLUMELLAR "TEETH"
AMONG NASSARIINE GASTROPODS
HAASL, David M., Dept. of Geosciences, California State University, Chico,
CA, USA
The neogastropod subfamily Nassariinae (Muricoidea: Nassariidae)
exhibit a striking geographic and phylogenetic pattern in the distribution
of apertural and columellar characters. Labral spines or teeth, columellar
spurs, and strongly developed columellar calluses occur more frequently
among tropical Indo-West Pacific (IWP) nassariines than in nassariine
species from other regions. A higher frequency of spines, teeth, and strongly
developed shell armor also has been reported from IWP species in many
other gastropod families (e.g., Muricidae, Thaididae, Fasciolariidae,
Strombidae). This is often attributed to higher levels of predation pressure
in the tropical IWP relative to the Atlantic. Phylogenetic analyses of
nassariine gastropods suggest these characters are largely confined within
a single, extremely diverse IWP clade that includes nearly 70% of extant
nassariine species. Despite the complex distribution of labral and columellar
characters and the current coarse resolution of phylogenetic relationships
among IWP clade members, a few general observations can be made. The appearance
of strong columellar or labral sculpture within the IWP clade seems to
be a relatively recent event in the clade's history. The IWP nassariine
pre-Pliocene record is poorly known, but Miocene clade members lack strongly
developed labral or columellar sculpture; they more closely resemble modern
and fossil East Pacific and Atlantic species. Strong columellar calluses
first appear in the IWP during the Late Miocene. Labral or columellar
teeth and spines appear later, during the Pliocene. The number of IWP
nassariine species increases dramatically after the Late Miocene suggesting
a possible link between the acquisition of these characters and the clade's
diversification. Future research will focus on more detailed phylogenetic
analyses of the nassariine IWP clade, but additional information on the
structure and general occurrence of labral and columellar characters among
the Nassariinae is also needed.
HAGADORN, James W., and Kenneth H. Nealson, Div. of Geological and Planetary
Sciences, California Institute of Technology, Pasadena, CA, USA
X-radiographic computed tomography (CT) is a nondestructive
technique for examining the 3-D distribution of x-ray attenuation within
objects. CT data consists of a series of cross-sectional attenuation plots,
or slices, through a sample. By isolating areas of uniform attenuation
within each slice and stacking slices together, an isopycnal volume is
created. Where attenuation corresponds to paleobiologically-related heterogeneities,
isopycnal volumes of matrix-encased fossils can be created without physically
removing fossils from samples.
Although widely used in vertebrate paleontology, CT has not been used to
study invertebrate fossils which are soft-bodied, encased in matrix, or
preserved as 3-D casts/moldslike many Precambrian fossils. Our work suggests
that CT can yield reasonable 3-D models of such fossils. For example, analyses
of the Neoproterozoic disc-shaped fossil Aspidella reveals stalk-like
structures buried within the rock, immediately overlying bed sole impressions
of putative discoidal holdfasts. In larger samples (>10 cm3)
analyzed at 250 mm slice thicknesses, sufficient attenuation contrast exists
between the fossil molds and surrounding matrix to allow construction of
isopycnal volumes of these stalk-like structures. Similarly, isopycnal volumes
of silicified cloudiniids from Mexico and Nevada (analyzed at 8 mm slice
thicknesses) are comparable to morphologic features identified in previous
studies. Although volume-based morphology can be discerned in a variety
of other phosphatized, pyritized, clay-replaced, calcified, agglutinated,
and silicified Phanerozoic microfossils, we have not yet resolved attenuation
differences sufficient for visualizing clay-replaced fossils within shales
or aragonitic/calcitic/dolomitic fossils within carbonates. As a first step
toward imaging Proterozoic acritarchs and filaments, analyses of silicified
Phanerozoic microbiotas >25 mm in diameter have yielded isopycnal volumes
comparable to morphologic features identified through conventional petrographic
techniques.
HALLOCK, Pamela, Dana E. Williams, and Heidi Crevison, College of Marine
Science, University of South Florida, St. Petersburg, FL, USA
Coral-reef communities are threatened worldwide by stresses
ranging from localized impacts to global change. Resource managers urgently
need indicators of the biological condition of reef environments that
can relate data acquired through remote-sensing, water quality and benthic-community
monitoring to stress responses in reef organisms? Reef-dwelling foraminifera,
especially taxa that host algal symbionts, show great potential for use
as indicators of reef vitality: (a) Foraminifera are widely used as environmental
and paleoenvironmental indicators. (b) Zooxanthellate corals and foraminifera
with algal symbionts have similar environmental requirements. (c) A readily
identifiable and abundant genus, Amphistegina, exhibits similar
stress responses to those found in corals. (d) The relatively short life
spans of foraminifera as compared with colonial corals facilitates differentiation
between long-term decline and episodic stress events. (e) Foraminifers
are relatively small and abundant, permitting statistically-significant
sample sizes to be collected quickly and relatively inexpensively. (f)
Collection of foraminifera has minimal impact on reef resources.
The "FoRAM" (Foraminifers in Reef Assessment
Monitoring) protocol is the synthesis of 30 years of research on reef
sediments and reef-dwelling larger foraminifera. The three-tiered procedure
includes sediment-constituent analysis, which can address questions of
historical change and reference-site suitability; analysis of live foraminiferal
assemblages to indicate the suitability of sites of concern for organisms
with algal symbionts; and analysis of Amphistegina populations
for evidence of specific stressors to which these foraminifera respond
similarly to corals. Future research to identify and quantify physiological
and molecular responses to specific stressors will further facilitate
use of larger foraminifers as bioassay organisms in reef research.
HANCOX, P. John, Dept. of Geology, University of the Witwatersrand, Johannesburg,
South Africa; and Bruce S. Rubidge, Sean P. Modesto, and Alain J. Renaut,
Bernard Price Institute for Palaeontological Research, University of the
Witwatersrand, Johannesburg, South Africa
Dicynodonts are a clade of herbivorous non-mammalian
synapsids that are important components of Late Paleozoic and Early Mesozoic
terrestrial faunas. The systematics and phylogenetics of the Permian forms
is now well established, however that of their Triassic counterparts is
still poorly understood, with cladograms to date being only of the hand
crafted type. Here we present the first computer generated (PAUP) phylogenetic
study of the Triassic dicynodonts, based mainly on first hand observation
of the type material from several countries. The scope for long distance
correlation of nonmarine, dicynodont bearing strata, has long been recognized,
and dicynodonts have previously been used to define various land vertebrate
ages (LVAs), chronofaunas, land-vertebrate faunas, empires, intervals,
biochrons, faunal epochs and land-vertebrate faunachrons (LVFs). This
study is therefore vital, not only to our understanding of the systematics
of the Triassic dicynodonts, but also for studies on the biogeography
and biochronology of these forms.
HANGER, Rex A., Dept. of Geography and Geology, University of Wisconsin-Whitewater,
Whitewater, WI, USA
During the Late Paleozoic, faunas of the west coast of
Pangea plus the offshore island arc terranes, were dominated by brachiopods,
corals, fusulinids, bryozoans and mollusks. Outcropping today in western
North America, the presence of both Asiatic and endemic taxa among the
terrane faunas led to far-travelled, "exotic" interpretations
for the arcs themselves, in accord with tectonic models incorporating
west-directed subduction throughout the Late Paleozoic. Such models allowed
arc terranes to exist at extreme (1000s of km) distances outboard within
Panthalassa. Recent dating and provenance analysis of detrital zircons
(Soreghan and Gehrels, 2000) reveal many patterns, most of which link
western North American arc terranes to sources on the Pangean continental
margin. These data constrain original arc paleogeographic positions as
proximal to the margin, favoring tectonic models that incorporate east-directed
subduction, irreconcilable to the original interpretations of paleobiogeographic
data.
Previous "exotic" interpretations were based
largely on the presence of a single, or very few, "key" taxa.
Using databases of whole faunas of brachiopods and bryozoans, plus supplemental
data from corals and fusulinids, probabilistic similarity analyses, testing
against a null model of random distribution in space, reveal new paleobiogeographic
patterns. Although some significant relationships exist with Asiatic faunas,
the preponderance of statistically significant arc terrane affinities
lie with the western Pangean continental margin. Rather than being antagonists,
paleobiogeography and detrital zircon provenance are reciprocal illuminators,
both indicating a proximal location for most western North American island
arc terranes during the Late Paleozoic.
HANKINS, Karina G., and David J. Bottjer, Dept. of Earth Sciences, University
of Southern California, Los Angeles, CA, USA
The mass extinction in the marine realm at the end of
the Triassic is considered one of the five biggest extinction events of
the Phanerozoic, but is not well studied due to a lack of good sections
spanning the boundary. Even less is known about the dynamics of the recovery
interval that followed. One of the most complete and fossiliferous marine
sequences of Triassic-Jurassic strata is located at New York Canyon in
the Gabbs Valley Range of west-central Nevada, which houses the proposed
global stratotype section for this boundary. This area has been the focus
of extensive biostratigraphic studies and facies change analyses (Taylor
et al., 1983; Hallam and Wignall 2000), and the paleoecology of Upper
Triassic strata has been assessed by Laws (1982). However, the ecological
changes that took place across the boundary have not received detailed
analyses.
This study represents a first attempt at analyzing the
nature of paleoecological changes across the boundary and into the recovery
interval in the New York Canyon area, with changes in paleocommunity composition
and structure as the primary focus. Preliminary observations of the Lower
Jurassic Sunrise Formation reveal that a low-diversity epifauna of relatively
small bivalves and gastropods exists in the shallower-water facies, while
brachiopods and ammonites become increasingly abundant in the offshore
facies. Intervals of intense bioturbation occur within Lower Jurassic
strata and large, resistant, primarily horizontal burrows appear in the
Sinemurian New York Canyon Member. However, the diversity of trace fossils
throughout these beds remains low. These observations indicate that facies
changes play an important role in the record of the recovery from the
end-Triassic extinction at New York Canyon, and are consistent with a
prolonged recovery from this crisis as described in Hallam (1996). Further
investigation may shed light on the possible causes of the extinction
itself, and the reasons for a slow recovery.
HANNIBAL, Joseph T., The Cleveland Museum of Natural History, Cleveland,
OH, USA; and H. Gregory McDonald, Geologic Resources Division, National
Park Service, Denver, CO, USA
Crayfish from the Pliocene of the Idaho/Oregon region
were first described by Cope and later reevaluated by carcinologist Mary
Rathbun. Examination and preparation of new three-dimensionally preserved
material and museum specimens of Pacifastacus chenoderma (Cope)
reveal a number of undescribed characters confirming Hobb's placement
of the species in the genus Pacifastacus as well as Rathbun's observation
that the species is morphologically similar to extant crayfish of the
region, including P. connectens.
Preservation of material, with the exception of the carapace
posterior, can be very good, although there is no single complete specimen.
The epistome, mandible, renal aperture, and other parts seldom if ever
seen in fossil crayfish are preserved. Well-preserved cuticle exhibits
layering. Some cuticle is crazed, some is broken into bits, and some is
crushed to various degrees.
The species is robust, and has a spiny, acute rostrum
and pointed pleurites. This armament may be a protective adaptation to
Pliocene predators such as the large extinct species of pike-minnow Ptychocheilus
found in Lake Idaho sediments. An extant species of Ptychocheilus
present in the Snake River feeds on crayfish. At least one fossil crayfish
has a mark that may be attributable to a vertebrate bite.
Large crayfish gastroliths (up to 13 mm in diameter)
have been collected from the Pliocene of this region since the time of
Cope and Marsh. The size of the gastroliths is what would be expected
for the size of the body fossils. Thin sections show that these gastroliths
are layered much like those of modern crayfish, confirming their identification.
Thus, these gastroliths do document the existence of crayfish at localities
where body fossils are lacking. Gastroliths are occasionally found in
pairs, which may indicate that they came from a single crayfish.
HANSON, Dale A., Dept. of Geological Sciences, University of Oregon,
Eugene, OR, USA; and Theodore J. Fremd, John Day Fossil Beds National
Monument, Kimberly, OR, USA
Two major vertebrate fossil assemblages occur in the
Camp Creek area (near Logan Butte, Oregon), separated by the "Picture
Gorge Ignimbrite" of the John Day Formation. Long characterized as
faunally identical to the well-known eastern basin assemblages, recent
stratigraphically analyzed collections have revealed a similar, but significantly
different fauna. The lower assemblage is characterized by agriochoerids
(32% of identified specimens), tragulids (24%), oreodonts (8%), equids
(6%), and numerous species of canids (4%) and nimravids (2%). It also
produced the only known examples of the marsupial Herpetotherium merriami,
the ursoid Parictis primaevus, the enigmatic Allocyon loganensis,
and small nimravids. The Turtle Cove fauna, in contrast, consists of 35%
tragulids, 25% oreodonts, and 6% rhinocerotids, with agriochoeres representing
less than 2% of the faunas. Notable by their absence are the diminutive
nimravids and Allocyon. The upper assemblage at Camp Creek is characterized
by several families of rodents, making up 59% of identified specimens,
the exclusive occurrence of the large oreodont Merycochoerus, and
a near absence of other artiodactyls. The observed disparities between
the lower assemblage and the Turtle Cove fauna, previously thought to
be temporal, are probably due to local paleoenvironmental factors including
proximity to flowing water and elevational effects. Sedimentological evidence
supports this conjecture. The southern basin is characterized by numerous
channel deposits, almost absent from the eastern basin. These channel
deposits range from clayey to sandy lithologies, and are typically incised
one to three meters into the underlying sediments. Newly sampled tuffs
from the southern basin, correlated with those from Turtle Cove, allow
us to confirm that these are, in fact, isochronous assemblages, providing
an unusual opportunity to compare temporally equivalent but ecologically
different associations.
HARRIES, Peter J., Dept. of Geology, University of South Florida, Tampa,
FL, USA
During the past two centuries, mass extinction events
have played an important role in the development of paleontologic thought
and theory surrounding a spectrum of issues. Although these earlier studies
identified numerous extinction horizons in the geologic record, most of
the data collected were not highly resolved from a stratigraphic standpoint
and, therefore, many of these data sets were of insufficient resolution
to answer important questions related to mass extinction dynamics. However,
primarily during the past two decades, there has been a large effort devoted
to discerning the details of mass extinction events#&151;both in terms of extinction
and repopulationwith the ultimate goal of better understanding causation
as well as ecologic and evolutionary changes associated with these events.
This research, which has spanned numerous biotic crises of wide ranging
magnitudes and geography, has created a record of faunal ranges that is
considerably more resolved than those that previously were available.
In virtually all cases, these better-resolved data have revealed that
mass extinction events are far more complex than previously thought. Most
mass extinction events appear to be have occurred in a step-wise fashion,
and the presence of this pattern suggests that these events represent
complex biotic responses to environmental and ecologic perturbations.
Although some of these patterns may reflect sampling and preservational
biases, in the cases where statistical tests have been applied to test
the robustness of the range data, they have shown that the patterns are
not artifacts. Despite the increased resolution and insight that has been
gained, there are, however, limits to the resolution that can be obtained
and hence the questions that can be answered. These limits ultimately
reflect the depositional, stratigraphic, and preservational fidelity of
the record and act as the final control on whether data of sufficient
detail can ever be collected to answer certain questions.
HARWOOD, David M., Dept. of Geosciences, University of Nebraska-Lincoln,
Lincoln, NE, USA; and Vladimir A. Nikolaev, Komarov Botanical Institute,
St. Petersburg, Russia
Silicified scales tentatively attributed to the Chrysophyceae
occur in Upper Proterozoic chert from Alaska. The oldest Xanthophyceae
are Carboniferous in age. Diatom assemblages appeared by the Late-Early
Cretaceous and began radiating toward diverse Late Cretaceous floras,
although a significant turnover occurred in the mid-Cretaceous. Early
diatoms had a long history of silicified resting stages and non-silicified
to weakly-silicified vegetative cells, parallel to some modern Chrysophyceae
and Xanthophyceae. One theory of diatom origin suggested a link between
the diatom valves and siliceous scales of chrysophytes, yet these do not
have a resting stage with paired valves, and they are haploid, not diploid
as in the diatoms. The problem of ploidy was addressed by the suggestion
that a diploid silicified cyst stage, like that of Parmales became the
dominant phase in the diatom life cycle. We suggest a similar life-cycle
shift, but features shared by Lower Cretaceous diatoms and some Xanthophyte
orders focus our attention here. Features in common including diploidy,
oil production, silica impregnation of the cell wall, silicified resting
stages with paired valves, similar pigments, benthic habitat, cylindrical
colonies, long pervalvar axes, overlapping valves and similar size. Lower
Cretaceous diatoms from Antarctica and Australia offer a new framework
to compare the morphology, ecology and life history of the Chromophyte
algae. These oldest records of diatoms involved benthic filamentous colonies
of long, cylindrical cells and heavily silicified resting spores, which
radiated during the mid-Cretaceous into the planktic realm and a diversity
of benthic substrates. This may have been stimulated by mid-Cretaceous
transgression/regression cycles, which opened new niches and introduced
taxa to changing environmental gradients of salinity, nutrients, etc.
New diatom genera appear during the Late Cretaceous and Paleogene at a
rate of ~1.6 genera/m.y. and disappear at a rate of ~1.3 genera/m.y.
HASIOTIS, Stephen T., Dept. of Earth Sciences, Indiana State University,
Terre Haute, IN, USA
Alluvial, lacustrine, aeolian, and transitional-marine
deposits of the Upper Jurassic Morrison Formation in the Rocky Mountain
region contain varying degrees of hidden biodiversity representing terrestrial
and freshwater ecosystems. The morphology, distribution, and lateral and
vertical tiering of ichnofossils provide information on trophic interactions
preserved by organism behavior, and ecological and climatic changes experienced
during the deposition of the Morrison. The trace fossils in soil ecosystems
represent ecological innovations in (1) food hoarding, (2) adaptations
to disturbance from flooding and precipitation, (3) unpredictable hypercarbic
and hypoxic conditions, and (4) subterranean reproductive strategies employing
a holometabolous life cycle. The traces representing these ecological
behaviors vary in abundance in paleosols, from isolated occurrences associated
with pedogenic features to thousands of crosscutting traces that obliterate
all bedding and pedogenic structures.
The Morrison ichnofossil record in immature to mature
paleosols reveals that the major components of detritivore-based food
webs and essential innovations for fossorial life in soil ecosystems were
present. Ichnofossils represent community members of energy pathways and
niches for detritivores (saprophagous, coprophagous, and necrophagous
roles), herbivores, omnivores, and carnivores in the terrestrial ecosystems.
Traces of permanent to transient soil-dwelling life styles illustrate
adaptations to varying degrees of environmental disturbance, osmoregulation
crises, and hypercarbic and hypoxic conditions. Food hoarding was incorporated
into the subterranean reproductive strategies of several different groups
of temporary and periodic soil-dwelling invertebrates. Co-evolved morphological,
physiological, and behavioral adaptations to hypoxia and hypercarbia resulted
from food stored with larvae and adults in belowground settings. Social
behavior in insects and mammals was a solution to competition for resources
and space in the soil ecosystem.
HASIOTIS, Stephen T., Dept. of Earth Sciences, Indiana State University,
Terre Haute, IN, USA
The recognition and interpretation of complex ichnofossils,
particularly in the Mesozoic, is a relatively recent phenomenon. Complex
ichnofossils represent unique solutions through degrees of social cooperation
to the perils of terrestrialism and fossorial life. The evolution of social
cooperation and eusocial behavior (only in insects) is an innovation that
has been evolved multiple times by different insects and mammals for performing
chores and dealing with hazards associated with foraging for food, rearing
the young, nest defense, burrow maintenance, and more, in terrestrial
environments. These ichnofossils also preserve major innovations in soil
ecosystems that include (1) food hoarding, (2) adaptations to disturbance
from flooding and precipitation, (3) enduring unpredictable hypercarbic
and hypoxic conditions, and (4) reproductive strategies by employing a
subterranean life cycle.
Complex ichnofossils are highly variable in architecture
and reflect the type of organism, the number of individuals per nest,
the length of time the structure is used, and the degree of sociality.
A pattern of interconnected galleries and chambers of varying length,
width, height, and number usually distinguish complex traces. Insect societies,
such as termites (Isoptera), ants (Hymenoptera), and the higher bees and
wasps (Hymenoptera: Aculeata), show the greatest variability in trace
fossil complexity-simple to extremely elaborate structures. Individuals
cooperate to construct and maintain the nest, collect and grow food supplies,
feed nest members, protect the nest from invaders, and care for the young.
To a lesser extent, reptiles, therapsids, and mammals also exhibit these
behaviors, which is also reflected in the complexity of the trace fossil.
These organisms also maintain the nest temperature and humidity, as well
as to avoid hypercarbic and hypoxic gas levels. Situations are resolved
by individuals working together to maintain and alter the nest architecture
to bring appropriate atmospheric and climatic conditions to the subterranean
community.
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