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Pander Society Newsletter - University of Leicester

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asal conglomerate (in relation with the Triassic sealing <strong>of</strong> the post-accretionary Kurosegawa Terrane,<br />

Outer Zone <strong>of</strong> SW Japan) has been published (Ishida et al., 2005). Provenance <strong>of</strong> the Triassic conodontbearing<br />

gravels in the Lower Jurassic cover formation <strong>of</strong> the Mae Sariang Zone was discussed with special<br />

respect to the sealing and erosional event <strong>of</strong> the Shan Thai Terrane (Ishida et al., 2005). The Triassic<br />

(Carnian-Norian) conodont biostratigraphy <strong>of</strong> the meta-chert succession in the Mino-Tamba Jurassic<br />

accretion terrane (Inner Zone <strong>of</strong> SW Japan) will now be studied (Mikami et al., 2006).<br />

Yukio Isozaki. Currently working on detailed stratigraphy <strong>of</strong> the Guadalupian-Lopingian (=Middle-Upper<br />

Permian) boundary interval and the Lopingian/Induan (=Permian-Triassic) boundary interval in South<br />

China and in Japan.<br />

Nadezhda G. Izokh. Study <strong>of</strong> conodonts from Ordovician, Silurian and Devonian <strong>of</strong> the Altai-Sayan<br />

folded area, West Siberia, Russia and South Tien Shan.<br />

Lennart Jeppsson. Collecting and processing work on the Linde and Klev events, and on the recently<br />

discovered early Wenlock Ansarve event has yielded much new data. This is critical for achieving a highresolution<br />

stratigraphy for these intervals, to identify localities for future work (on other major clades,<br />

isotopic and sedimentological changes), to judge the strength <strong>of</strong> these events, and, not least, to reveal how<br />

badly conodonts fared during these events. Manuscripts include papers now in the list <strong>of</strong> publications (see<br />

also Calner et al.), the submitted one and the subzones <strong>of</strong> the O. s. rhenana Zone. These can be followed<br />

across different facies belts in the Silurian sequence <strong>of</strong> Gotland. Application <strong>of</strong> them result in unexpected<br />

large revisions in the local stratigraphy, but also makes the range <strong>of</strong> other clades conform with those found<br />

elsewhere.<br />

David Ian Johnston. A paper on disrupted conodont bedding plane assemblages from the Mississippian <strong>of</strong><br />

western Canada by Charles Henderson and myself has been published. We also presented a poster on this<br />

topic at the AAPG meeting in Calgary this past June. I have also been doing some biostratigraphic service<br />

work involving conodonts this year as well. Working on another manuscript (with C. Henderson)<br />

concerning the conodont biostratigraphy and the implications for sequence stratigraphy for the upper<br />

Wabamun Group to lower Banff Formation interval in the surface and subsurface <strong>of</strong> southern Alberta. The<br />

work is based on the MSc thesis <strong>of</strong> C. Henderson’s recent graduate student Michael Schmidt. I am now<br />

involved in non-conodont work by providing services in petroleum geology.<br />

David Jones. Working on morphometric analysis <strong>of</strong> Ozarkodina excavata and Pterospathodus to examine<br />

taxonomy, population variation and evolutionary rates, patterns and processes.<br />

Gareth Ll. Jones. Mineral exploration activities in Ireland only just begun to lift again, lagging behind the<br />

recovery in zinc prices. I look forward to working with conodonts (and foraminifers, algae, etc.) in 2006.<br />

Meanwhile geothermal exploration is keeping me warm!<br />

Jun Chen. In order to know more about Late Permian-Early Triassic conodonts from Meishan Section<br />

(GSSP), South China, especially the evolutionary status <strong>of</strong> genera Clarkina, many samples have been<br />

collected and processed. Abundant specimens have been picked from these residues. Now working on my<br />

thesis (under Pr<strong>of</strong>. Charles M. Henderson, Calgary, Canada) and hopefully will be completed by mid-2006.<br />

Tea Kolar-Jurkov�ek. Most <strong>of</strong> my projects on Triassic biostratigraphic studies in Slovenia and Croatia<br />

continue collaboratively with my colleagues. An intensive study <strong>of</strong> the P-T interval and Lower Triassic is<br />

in progress in many sections <strong>of</strong> the Dinarides in order to define the systemic boundary biostratigraphically.<br />

Micropaleontological study <strong>of</strong> two sections in the Raibl Beds (Carnian) <strong>of</strong> Slovenia have been published; 1)<br />

a conodont apparatus <strong>of</strong> Nicoraella ? budaensis is demonstrated from the Belca section; and 2) some new<br />

gastropod taxa are recognized from the two assemblages <strong>of</strong> the Mezica area.<br />

Erik Cowing Katvala. Most <strong>of</strong> my work to date has focused on using biostratigraphic, paleoecologic, and<br />

paleogeographic data from Mississippian through Triassic conodonts to help constrain paleontologic,<br />

stratigraphic and tectonic interpretations in the accreted terranes <strong>of</strong> western North America. I have also<br />

been working on element distributions in conodont elements on the electron microprobe.<br />

Ali Murat Kilic. Working on the Triassic conodonts from the Kocaeli & Karaburun peninsulas, Taurids,<br />

Bulgaria and Japan with Pr<strong>of</strong>s. K. Budurov & F. Hirsch.<br />

William Kirchgasser. Work continues on conodont and microvertebrate fossils <strong>of</strong> the ‘Conodont Bed’<br />

(North Evans Limestone) around the Givetian/Frasnian boundary in western New York. A manuscript with<br />

G. Klapper on the Frasnian conodont sequence in New York is in prep. Work continues on the conodontgoniatite<br />

associations in the lower Frasnian <strong>of</strong> Pennsylvania, a project being conducted in collaboration<br />

with Gordon Bair (SUNY Fredonia) and Carl Brett (Univ. <strong>of</strong> Cincinnati).<br />

Elena M. Kirilishina. Research on the conodonts from Frasnian-Famenian boundary interval <strong>of</strong> central<br />

regions <strong>of</strong> the Russian Platform.<br />

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