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Contrasting Deep-water Records from the Upper Permian and Lower Triassic of South Tibet and British Columbia: Evidence for a Diachronous Mass Extinction

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Figure

FIGURE 1—Global paleogeography during the Permian-Triassic boundary interval (based from data in Stampfli et al., 1991, Scotese andLongford, 1995, and Kobayashi, 1999).
FIGURE 3—Stratigraphic section for section 1, Permian and Early Tri-stone; Wassic boundary strata in the center of the Xishan outrop at Selong,southern Tibet (see Fig
FIGURE 4—Comparison of P–Tr boundary strata in the middle (section 1) and eastern end (section 2) of the Xishan outcrops, Selong, showingWlocal development of stromatolitic limestone at contact between the Selong and Kangshare formations
FIGURE 6—Photomicrograph showing the intimate intergrowth of gyp-sum laths with the stromatolitic laminae
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