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A baseline model for the co-evolution of hosts and pathogens by Bennett R., Bowers R. G.

By Bennett R., Bowers R. G.

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Most abundant are the following fossil remains: Siphonifera algae Calciofolium okense Schw. ), G. ; and crinoids Stukalinocrinus magnus sp. nov. and Inclarocrinus inclarus sp. nov. Typical are large forms. The thickness is 6-11 m.

36 Suppl. ru/ EARLY CARBONIFEROUS ECHINODERMS OF THE MOSCOW REGION Plate 10 PALEONTOLOGICAL JOURNAL Vol. 36 Suppl. ru/ Vol. 36 Suppl. 2 2002 EARLY CARBONIFEROUS ECHINODERMS OF THE MOSCOW REGION Plate 12 PALEONTOLOGICAL JOURNAL Vol. 36 Suppl. ru/ 6b Vol. 36 Suppl. 2 2002 EARLY CARBONIFEROUS ECHINODERMS OF THE MOSCOW REGION P l a t e 14 PALEONTOLOGICAL JOURNAL Vol. 36 Suppl. ru/ Vol. 36 Suppl. 2 2002 EARLY CARBONIFEROUS ECHINODERMS OF THE MOSCOW REGION Plate 16 PALEONTOLOGICAL JOURNAL Vol. 36 Suppl.

5 and 6. Unilineatocrinus tenuicarinatus Arendt, sp. ; (5) no. 1557/99,'columnal: (5a) articular facet view, (5b) side view; x4; the same locality; (6) holotype, no. 1557/98, column fragment consisting of three colum­ nals and broken transversally in two halves: (6a) articular facet view, (6b) internal side view; x4; the same locality. P l a t e 15 Figs. 1-3 and 6-9. ) excentricus Arendt, sp. ; (1) no. 5; (lb) lateral surface; x3; quarry near the village of Mitino, Exposure 11, Bed 38, marl; Serpukhovian Stage, Lower Serpukhovian Substage, Steshev Horizon (lower part); (2) holotype, no.

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