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Science China Earth Sciences 2008年第11期51卷 1581-1588页

作者： XU Ran GONG YiMing ZENG JianWei Key Laboratory of Biogeology and Environmental Geology of Ministry of Education State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesWuhan 430074China Institute of Resources and Environment Key Laboratory of Biogenic Traces&Sedimentary Minerals of Henan ProvinceHenan Polytechnic UniversityJiaozuo 454003China

The abundance curves derived from area proportions of brachiopods and Girvanella in the thin sections from the Yangdi section, South China, exhibits complex relationships during the Late Devonian Frasnian-Famennian transition. The living activity of brachiopods such as grazing and borrowing did great damage to the growth of Girvanella. However, there was more to just a mere a survival competing relationship between them, Girvanella actually improved marine environments by oxygenating the dysoxic ambient sea-water through photosynthesis in the lower Kellwasser Horizon. Profited from this improvement brachiopods' abundance increased subsequently and suppressed Girvanella again. Nonetheless, without Girvanella's photosynthesis, brachiopods were wiped out by the farther anoxic environments in the upper Kellwasser Horizon. The complex relationships between Girvanella and brachiopods may be a key to unlocking the relationships between geomicrobes and metazoans in the geological overturn periods.

关键词： brachiopods Girvanella anoxia Late Devonian F-F mass extinction South China

TRACE ELEMENT GEOCHEMISTRY OF INARTICULATE brachiopods AND SEDIMENTARY ROCK ON THE CAMBRIAN-ORDOVICIAN BOUNDARY

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Science China Chemistry 1990年第7期33卷 873-886页

作者：赵振华赵惠兰 Institute of Geochemistry Academia Sinica Guiyang 550002 PRC

That the contents and compositions of trace elements, especially REE in sedimentary rock and agustite originating from inarticulate brachiopods, conodont, etc. change in the vertical direction usually has a close relation with the stratigraphic boundary of important biologies. This paper systematically analyses REE and 16 trace elements such as U, Th, Sr, Ba, Co, Ni, Cr, V, Cu, Pb, Zn, Sc, Au, As in sedimentary rocks and the agustite on the standard stratified section of the Cambrian-Ordovician Boundary in Dayangcha, Huniiang, Jilin Province. Based on this, the authors investigate the REE distribution pattern and the law of the contents and compositions of trace elements changing, providing the geochemical evidence for building stratified sections of the Cambrian-Ordovician boundary and discussing sedimentary environments.

关键词： stratified section of Cambrian-Ordovician Boundary Hunjiang inarticulate brachiopods

Jurassic brachiopods and Paleogeography of North Qinghai-Tibetan Plateau

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Journal of Earth Science 1990年第1期9卷 17-37,135页

作者： Yang Zunyi Shi XiaoyingDepartment of Geology , China University of Geosciences , Beijing 100083

This paper deals with Jurassic brachiopods from North Tibet and South Qinghai and the stratigraphical subdivision there. Based on faunas and strata,a general outline of the palaeogeographical evolution has been traced out along the line of plate-tectonic movements . In this paper , 10 species of 8 genera are described , among which the species Lacunosella rhombica , Rntithyris vulgaris , Tanyothyris appositus , Apatecosia navicularis and Flabellothyris sp . nov . have been recognized as new .

关键词： Jurassic brachiopods stratigraphy palaeogeography .

Exceptionally preserved brachiopods from the Chengjiang Lagerst(a|¨)tte(Yunnan,China):Perspectives on the Cambrian explosion of metazoans

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Science Foundation in China 2013年第2期21卷 66-80页

作者： ZHANG ZhiFei HOLMER Lars Erik State Key Laboratory of Continental Dynamics Early Life InstituteNorthwest University LPS Nanjing Institute of Geology and PalaeontologyChinese Academy of Sciences Department of Earth Sciences PalaeobiologyUppsala UniversityVillavgen 16SE-752 36 UppsalaSweden

The Cambrian explosion was coined to describe the geologically sudden appearance of numerous bilaterian body plans(Phyla)around the Ediacaran-Cambrian transition,around 565-520million years *** explanations and conjectures have been postulated in order to explain the pattern and duration of this explosive radiation of many different phyla of early ***,we focus on the evolution of a phylum of marine suspension-feeding animals—the brachiopods,as exemplified by the exceptionally preserved taxa from the celebrated Chengjiang Konservat Lagerst(a|¨)tte(Yunnan,China).The abundant soft-bodied preservation at these fossil quarries gives us the only firm insights into what brachiopods looked like and how they functioned and lived when they first appeared on the *** of Chengjiang brachiopods demonstrate that the early animals developed a remarkably varied organization of tissues and organs shortly after the onset of Cambrian *** the marine suspension-feeding brachiopods,most importantly the tentaculate feeding structure of early brachiopods is already differentiated into two shapes of lophophore,anteriorly coiled(spiralled)and posteriorly arching tentacle crowns and the unique latter type was previously not documented from fossil and living *** unlike any known Recent brachiopod,all the known Cambrian brachiopods from Chengjiang have an open digestive tract that was disposed either as a Ushaped gut in linguliform and stem group brachiopods,or straight gut with a posterior anus in some calcareous-shelled ***,in contrast toliving lingulids,all the Cambrian brachiopods have an epibenthic lifestyle either cemented by a ventral valve or attached by variable pedicles to establish complex ecological community encompassing primary tierers and variable secondary *** is therefore assumed that brachiopods were the first benthic metazoan that achieved their success in ecological stratification and tiering complexity by lat

关键词： Cambrian explosion Chengjiang fauna Metazoans brachiopods Soft-tissue preservation

LOWER PERMIAN brachiopods AND PALYNOMORPHS OF THE ALBORZ MOUNTAINS (NORTH IRAN) AND THEIR PALAEOBIOGEOGRAPHIC AFFINITY

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LOWER PERMIAN BRACHIOPODS AND PALYNOMORPHS OF THE ALBORZ MOU...

Changhsingian sea level changes and brachiopod diversity in the upper Yangtze region

第二届国际古生物学大会

作者： Lucia ANGIOLINI Michael H.STEPHENSON Dipartimento di Scienze della Terra "A.Desio" Universita degli Studi di MilanoVia Mangiagalli 3420133 MilanoItaly British Geological Survey NottinghamUK

North Iran has always been considered of Gondwanan affinity for several reasons: its pre-Palaeozoic basement is thought to be related to the Baikalian orogenetic cycle, its Cambrian sedimentary rocks are similar to those occurring south of the Zagros suture. Similarly the region lacks Variscan deformation and is located south of the supposed position of the Palae-

关键词： North Iran palaebiogeography brachiopods palynomorphs Early Permian

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Science China Earth Sciences 2007年第3期50卷 343-349页

作者： ZENG Yong LIU Mei WANG ZhanLei CHEN Wei School of Resource Engineering and Earth Science of China University of Mining and TechnologyXuzhou 221008China

Sedimentary environment and distribution of brachiopods during the Changhsingian in Xingwen, Si-chuan Province of the upper Yangtze region, are statistically analyzed. Changing regularity in diversity of brachiopod is synthetically investigated based on qualitative and quantitative analysis of transgres-sion-regression cycles. The results show that the diversity of brachiopods in this region in the trans-gression (aggradation) sequence is higher than that in the regression (progradation) sequence. The brachiopods in this area began to diversify in the early Changhsingian. And the species diversity had four peak stages which are respectively in the middle Early Changhsingian, late Early Changhsingian, early Late Changhsingian and late Late Changhsingian. The species diversity reached its highest in the late Late Changhsingian but this is followed by a sharp decrease at the end-hanghsingian, indicating the mass extinction of most brachiopod species which were prosperous in the Late Paleozoic.

关键词： species diversity sea level change brachiopods Changhsingian upper Yangtze region

α-and β-diversity Change of Late Ordovician Hirnantia Fauna of Changning,Sichuan,Southwest China

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Acta Geologica Sinica(English Edition) 2011年第2期85卷 330-339页

作者： ZHAN Renbin LIU Jianbo LIANG Yan LI Guipeng State Key Laboratory of Palaeobiology and Stratigraphy Nanjing Institute of Geology and Palaeontology the Chinese Academy of Sciences Nanjing 210008 China School of Earth and Space Sciences Peking University Beijing 100871 China

A continuous Ordovician-Silurian boundary section from the upper Wufeng Formation through the Kuanyinchiao Formation to the lower Lungmachi Formation has been carefully measured and collected at Shuanghe of Changning, southern Sichuan Province. For the first time, the temporal changes of α- and β-diversities of the Hirnantia fauna have been discussed in great detail. The general trend of brachiopod diversity change, increasing upward, is consistent with the regional trend of the Yangtze Platform, which had been controlled by both intrinsic and extrinsic factors. However, the sudden drop of diversity for a short period in the upper Kuanyinchiao Formation might have been controlled by environmental factors rather than normal faunal turnover. Synecological analysis using numerical methods recognizes two brachiopod-dominated associations of the Hirnantia fauna, the Dalmanella-Kinnella Association and the Mirorthis Association, both living in an offshore, deeper water environment corresponding to BA3-upper BA4, particularly lower BA3.

关键词： brachiopods Kuanyinchiao Formation Ordovician-Silurian transition Shuanghe of Changning

New Findings of Latest Early Olenekian(Early Triassic)Fossils in South Primorye,Russian Far East,and Their Stratigraphical Significance

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Journal of Earth Science 2021年第3期32卷 554-572页

作者： Yuri D.Zakharov Liana G.Bondarenko Alexander M.Popov Olga P.Smyshlyaeva Far Eastern Geological Institute Far Eastern BranchRussian Academy of SciencesVladivostok 690022Russia

Information on latest early Olenekian(latest Smithian)ammonoids is available apparently from only seven regions of the world,including South *** Smithian evidences on this topic are recorded from the West SMID(abbreviation from the Russian name of the quarry:"Building Materials and Details"),East SMID and Golyj Cape areas in South *** provides additional information on systematic composition of latest Smithian ammonoid,as well as conodont and brachiopod assemblages from the recently identified Shimanskyites shimanskyi Zone,located between lower Olenekian Anasibirites nevolini Zone and upper Olenekian Tirolites subcassianus *** are many common ammonoid species in the Shimanskyites shimanskyi Zone and the underlying Anasibirites nevolini Zone,e.g.,Prosphingitoides sp.,Arctoceras septentrionale(Diener),Churkites syskoi Zakharov et Shigeta,Submeekoceras?subhhydaspis(Kiparisova),Prionites markevichi Zakharov et Smyshlyaeva,?Anasibirites?simanenkoi Zakharov et Smyshlyaeva,Xenoceltites?subvariocostatus Zakharov et Smyshlyaeva,and Mianwaliites zimini Zakharov et *** base of the Shimanskyites shimanskyi Zone,marked by a negativeδ13Corg excursion in the Kamenushka-2 Section by our previous study,coincides with the FO(first occurrence)of ammonoids Shimanskyites shimanskyi Zakharov et Smyshlyaeva and Glyptophiceras ***(Waagen)and conodont Hindeodella budurovi *** zone is characterized additionally by some fossils common for the overlying upper Olenekian Tirolites subcassianus Zone:ammonoids of the genus Kamenushkaites,brachiopods Bittnerihyris margaritovi(Bittner)and Lepismatina *** conodont?Neogondolella?(=?Borinella)jubata *** latest Smithian ammonoids recorded from the Shimanskyites shimanskyi Zone totally consist of 30 taxa belonging to 11 families(Sageceratidae,Ussuiriidae,Aspenitidae,Paranannitidae,Arctoceratidae,Proptychitidae,?Galfetitidae,Prionitidae,?Kashmiritidae,Xenoceltitidae and Palaeophyllitidae).Th

关键词： ammonoids conodonts brachiopods biostratigraphy Smithian Russia

Yangtzedonta and the early evolution of shelled molluscs

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Chinese Science Bulletin 2001年第24期46卷 2103-2106页

作者： QIAN YiNanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences Nanjing China

The holotype of Yangtzedonta Yu, 1985 and its type species, Y. primitiva Yu, 1985, is an incomplete specimen of Xianfengella prima He et Yang, 1982. Therefore, based on the principle of priority, the names Yangtzedonta and Y. primitiva Yu (1985) should be abandoned. The fact that ventral valve of Xianfengella is bilaterally symmetrical indicates that they are not the left valve of a bivalved mollusc, as originally proposed by Yu. At present, the oldest certain bivalve is Xianfengoconcha elliptica Zhang, which occurs in the Early Cambrian Qiongzhusi Stage in China. The oldest known rostroconch is Heraultipegma yunnanensis He et Yang, which first occurs in the third small shelly fossil assemblage zone of the Early Cambrian Meishucunian Stage. The oldest known monoplacophoran, Maikhanella pristinis (Jiang), first occurs in the first small shelly fossil assemblage zone (Meishucunian Stage). Evidence derived from analyses of shell morphology, mode of growth, histology, and stratigraphic occurrence suggests

关键词： Yangtzedonta bivalves Xianfengella brachiopods enig- matic fossil.

Significance of Caucasian Sections for Working out Carbon-Isotope Standard for Upper Permian and Lower Triassic (Induan) and Their Correlation with the Permian of North-Eastern Russia

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Journal of China University of Geosciences 2005年第2期16卷 141-151页

作者： Yuri D Zakharov Alexander S Biakov Aymon Baud Heinz Kozur Far Eastern Geological Institute Russian Academy of Sciences (Far Eastern Branch) Vladivostok 690022 Russia North-East Interdisciplinary Scientific Research InstituteRussian Academy of Sciences (Far Eastern Branch)Magadan 685000 RussiaMusee de GeologieBFSH2-UNI 1015 Lausanne Switzerland Rézsü u. 83H-1029 Budapest Hungary

Data obtained on conodont distribution in the Permian-Triassic Sovetashen Section of Transcaucasia provide further limitations on the age of the carbon-isotopic anomalies discovered by Baud et al. (1989). The significance of Caucasian sections for working out the carbon-isotope standard for the Upper Permian and Lower Triassic (Induan) is shown. Original data on carbon-isotope composition of bivalve and brachiopod shells from Permian sediments of North-Eastern Russia (Omolon and Okhotsk areas) have been obtained, which may be used for their correlation.

关键词： Armenia North-Eastern Russia Permian Triassic conodonts ammonoids bivalves brachiopods isotopic composition paleotemperatures correlation