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that, prior to thatdiscovery, palaeobiological
ideas were essentially unconstrained. The
study of bedding plane assemblages, growth
and wear of elements, and modelling of
multielement architecture gives a framework
on which to develop palaeobiological
concepts; he noted that the issue of
zoological affinity is a subject that interests a
large number of people. He presented
evidence for paired sensory organs, ray-
supported caudal fin, extrinsic eye
musculature, and his lines of argument
supporting chordate affinities.
Papers then covered evolution,
palaeobiology and geochemistry. Hubert
Szaniawski (Polska Akademia Nauk)
discussed evolutionary relationships between
the earliest protoconodonts, paraconodonts
and euconodonts based on interpretations of
element morphology of some unusual forms
such as Coelocerodontus. Karen Cochrane
(Univ. Leicester) pursued the issue from a
histological perspective challenging the
traditional view of euconodont evolution from
protoconodonts via paraconodonts. She
used an unusual presentation graphic
representing 'white matter' in black. Petrovna
Kasatkina (Russian Academy of Sciences,
Vladivostok) argued from soft tissue
homology and analogy that euconodonts are
more appropriately considered as close to
chaetognaths and proposed a new
superphylum the Chaetodonta consisting of
euconodonts and chaetognaths. Stephanie
Barrett (Univ. Leicester) outlined her work on
functional morphology of the feeding
apparatus via the study of occlusion patterns
in prioniodontid Pa elements and speculated
on the impact of this on evolutionary patterns
during the Ordovician.
Two geochemical papers were
cautionary in tone. Studies of rare earth
elements in Triassic conodonts by Yasmin
Haunold (Inst. Paleo., Vienna) concluded that
variations reflect only very local conditions. A
study by Julie Trotter (CSIRO Division of
Petroleum Resources, Australia) of strontium
isotopes from conodonts from the Early
Ordovician Emanual Formation of the Canning
Basin show remarkable heterogeneity within
single elements; this has serious implications
for the development of a global strontium
curve. This paper generated the most intense
and varied discussion of the session, if not
the conference.
The next session ran concurrently
with the first IGCP 421 meeting, wherein the
general state of the project was assessed.
Focus then went on the early Palaeozoic and
dealt with more traditional conodont topics of
biostratigraphy and taxonomy: three
biostratigraphic papers spanning the
Cambrian and Ordovician; conodonts from the
central Appalachians (John Repetski,
U.S.G.S.), conodonts from the subsurface
western Canada and Williston Basins
(Godfrey Nowlan, Geol. Surv. Canada), and
Cambrian-Ordovician of the Argentine
Precordillera (Guillermo Albanesi, Museo de
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PaleontologÌa, Univ. Nacional Cordoba). Two
papers focussed on Upper Ordovician
conodont faunas from opposite sides of the
Atlantic; from Wales (Annalisa Ferretti, Univ.
Modena), and central Nevada (Walter Sweet,
Ohio State Uni.). The final two papers
focussed on palaeoecology and taxonomy:
Zhang Jianhua (Univ. Stockholm) presented
analysis indicating the Ordovician conodont
Spinodus spinatusis a deep-water indicator
and Anita Löfgren (Lund Uni.) presented a
septimembrate reconstruction of Cornuodus.
Day 2 dealt with Silurian conodonts
and biostratigraphy. Peep Männik (Inst.
Geol., Tallinn) carved up the late Llandovery
and early Wenlock celloniand
amorphognathoideszones into 10 new zones
based on the Pterospathoduslineage. Carlo
Corradini (Univ. Modena, our energetic
Sardinian guide) presented a Silurian zonal
scheme for Sardinia similar to the classic
approach of Walliser (1964). Viive Vira (Inst.
Geol., Tallinn) subdivided the Baltic Ludlow to
Pridoli using the 'remscheidensis' group.
Andrew Simpson (then Univ. Queensland)
presented Silurian conodont faunas from the
Jack Formation of northern Australia.
The Early Devonian followed: Jose
Ignacio Valenzuela-Rios (Univ. Valencia)
reinterpreted the A. eleanorelineage; Pierre
Bultynck (Inst. Roy. Sci. Naturelles de
Belgique) showed the facies relationships of
Morroccan Emsian to Eifelian conodonts
(dehiscensto partituszones). Other
Devonian studies by Bill Kirchgasser (State
Uni. New York) reported on biostratigraphic
implications of the widespread discovery of
"North Evans" conodont faunas. Willi Ziegler
(Forsch. Senckenberg) reviewed recent
developments in high-resolution conodont
biochronology in the Devonian noting that it
was more useful than sequence stratigraphy,
graphic correlation or alternate zonal
schemes, and tying their phylogenetic-zone
concept to recent radiometric data. Charles
Sandberg (U.S.G.S.) focussed on the use of
conodonts in establishing the timing of the
Late Devonian Alamo Impact Meggabreccia.
Gilbert Klapper (Dept Geol., Univ. Iowa)
compared the original 13-fold Frasnian
conodont zonation based on the Montagne
Noire sequence with 9-fold "standard"
zonation of the German and Great Basin
sequences, highlighting taxonomic and
methodological differences. This offering
generated the most biostratigraphic "heat" of
the meeting. Willi Ziegler (Forsch.
Senckenberg) presented conodont data
through the Frasnian-Famennian boundary of
the Rheinisches Schiefergebirge. Immo
Schülke (Univ. Hannover) reviewed early
Famennian conodonts of the Montagne Noire.
Norman Savage (Univ. Oregon) completed
with a report on Late Devonian conodont
faunas from Timan.
A break in the conodont flow followed
with a session dedicated entirely to IGCP421:
Alison Basden (MUCEP) covered Early
Devonian fish of the Tyers-Boola area of
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