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Terrestrial Palaeoecology and Global Change

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288 Valentin A. Krassilov. <strong>Terrestrial</strong> <strong>Palaeoecology</strong><br />

Fig. 114. Mid-Cretaceous biomes: (1) Xeromorphic scale-leaved, (2) Xeromorphic serrato-scale leaved, (3) Mixed evergreen (lauro-coniferous of<br />

Mediterranean type), (4) Mixed deciduous with evergreen elements (sequoio–platanoid with laurophylls), (5) Coniferous of temperate rainforest type<br />

with Sequoia <strong>and</strong> Cupressinocladus, (6) Mixed deciduous (parataxodio-platanoid).<br />

Typical localities: 1 – Anadyr, 2 – Sikhote Alin, 3 – Vilyuy, 4 – Kem, Yenisey basin, 5 – Nemegt, Gobi, 6 – Western Kazakhstan, 7 – Voronezh, 8 –<br />

Crimea, 9 – Bohemia, 10 – South Scania, 11 – Portugal, 12 – Bali (Guangze), 13 – Xigaze, Tibet, 14 – Jabalpur, 15 – Katch, 16 – Lebanon, 17 – Sudan,<br />

18 – Southern Mali, 19 – Tanzania, 20 – Koonwarra, southeastern Australia, 21 – Eromang, Quiensl<strong>and</strong>, 22 – New Zeal<strong>and</strong>, 23 – West Greenl<strong>and</strong>, 24 –<br />

North Slope, Alaska, 25 – Vancouver, 26 – Alberta, 27 – Potomac, Maryl<strong>and</strong>, 28 – Baqueró, Santa Cruz, 29 – Fossil Bluff, Alex<strong>and</strong>er Isl<strong>and</strong>.

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