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Evolution of metabolic scaling among the tetrapod:effect of phylogeny,the geologic time of class formation,and uniformity of species within a class

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Integrative Zoology 2022年第5期17卷 904-917页

作者： Valery M.GAVRILOV Tatiana B.GOLUBEVA Andrey V.BUSHUEV Department of Vertebrate Zoology M.V.Lomonosov Moscow State UniversityMoscowRussia Zvenigorod Biological Station M.V.Lomonosov Moscow State UniversityMoscowRussia

The metabolic scaling in the animal has been discussed for over 90 years,but no consensus has been *** analysis of 2126 species of vertebrates reveals a signiﬁcant allometric exponent *** show that classes of terrestrial vertebrates exhibit the evolution of metabolic *** the allometric coefﬁcient“a”and the allometric exponent“b”change naturally,but differently depending on the geological time of group *** allometric coefﬁcient“a”shows the measure of the evolutionary development of systems that forms resting metabolism in *** classes,such as birds and mammals,have a metabolic rate that is in an order of magnitude higher than that in ectothermic classes,including amphibians and *** the terrestrial vertebrate phylogeny,weﬁnd that the metabolic scaling is characterized by 3 main allometric exponent values:b=3/4(mammals),b>3/4(ectotherms,such as amphibians and reptiles),and bgeological start date of for-mation of the class approaches the present *** higher the mass-speciﬁc standard metabolic rate in the class,the slower metabolic rate grows with increasing body size in this *** results lay the groundwork for further exploration of the evolutionary and ecological aspects of the development of metabolic scaling in animals.

关键词： geological time metabolic rate scaling

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Multistage Metamorphic Evolution and P-T-t Path of High-T Eclogite from the North Dabie Complex Zone during Continental Subduction and Exhumation

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Acta Geologica Sinica(English Edition) 2016年第2期90卷 759-760页

作者： LIU Yican DENG Liangpeng GU Xiaofeng GROPPO Chiara ROLFO Franco CAS Key Laboratory of Crust-Mantle Materials and Environments School of Earth and Space Sciences University of Science and Technology of China Department of Earth Sciences University of Torino C.N.R.-I.G.G. Section of Torino

Objective High-T eclogites from the North Dabie complex zone （NDZ）, central China underwent a complex metamorphic evolution involved in ultrahigh-pressure （UHP） and high- pressure eclogite-facies metamorphism, and subsequent granulite-facies overprinting and amphibolite-facies retrogression during the Mesozoic continental deep subduction and exhumation. As a consequence, the eclogites were strongly affected by multiple decompression and re-crystallization processes during exhumation. Some eclogites have even been wholly transformed to garnet granulite, or garnet amphibolite, or even garnet-absent amphibolite.

关键词： ECLOGITE SUBDUCTION (Geology) ULTRAHIGH pressure metamorphism FACIES (Geology) geological time

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Geochronology and Geochemistry of Zengga Mesozoic Grantoids from East Gangdese Batholith, Implications for the Remelting Mechanism of Granite Formation

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Acta Geologica Sinica(English Edition) 2015年第A02期89卷 113-114页

作者： ZHANG Lan YANG Jingsui ZHANG Jian School of the Earth Sciences and Resources China University of Geosciences Beijing 100083 CARMA State Key Laboratory for Continental Tectonics and Dynamics Institute of Geology Chinese Academy ofGeological Sciences Beo'ing 10003 7 Tianjin Institute of Geology and Mineral Resources CGS Tianjin 300170

This paper reports geochemistry （major and trace elements）, zircon U-Pb and Lu-Hf isotope studies of leucogranite, granodiorite and clinopyroxene-bearing diorite from the Zengga intrusive body, eastern Gangdese bath... 详细信息

关键词： RESEARCH Mesozoic Era Granodiorite Plagioclase geological time Geochemistry

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Geochronology and Geochemistry of the Triassic Mafic Complexes from the Western Garzê-Litang Ophiolitic Mélange and Implications for the Melt Evolution of a Continental Margin

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Acta Geologica Sinica(English Edition) 2015年第A02期89卷 50-51页

作者： LIU Bin MA Changqian ZHANG Xin GUO Pan ZHANG Hang XIONG Fuhao State Key Laboratory of geological Processes and Mineral Resources China University ofGeosciences Wuhan430074 China Faculty of Earth Sciences China University of Geosciences Wuhan 430074 China

There is a general consensus that most ophiolites on the earth formed above a subduction zone and they often display a characteristic, sequential evolution of MORB to island arc tholeiities （IAT） to bonnites （Dilek et al., 2010, 2009; Pearce et al., 2003）. However, ophiolites occurred in a continental margin are very rare and usually have more complicated, irregular components, such as N-MORB,

关键词： RESEARCH Mafic rocks Ophiolites Mid-ocean ridges geological time Geochemistry

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