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作 者:王约[1]
出 处:《地质论评》2007年第4期539-555,I0007-I0010,共21页Geological Review
基 金:国家自然科学基金资助项目(编号40372023);贵州省科学技术基金资助项目(编号J-2006-2099);中石化项目(编号G0800-06-ZS-319);贵州大学学科建设基金项目;中国地质大学(北京)优秀博士论文扶持奖励基金项目的成果
摘 要:贵州剑河凯里组中产有丰富的遗迹化石,本文描述了其中的节肢动物遗迹9个属23个种(其中1个新属,9个新种)和3种类型的趾迹。发现并讨论了节肢动物(三叶虫)的捕食迹和求偶迹及其形成过程;研究了节肢动物生活行为所产生行迹之间的变化,认为节肢动物各行迹之间的过渡类型的变化具有停息→爬行→行走→游泳和游泳→行走→爬行→停息两向性变化的特点,并认为在运动弯道上形成的过渡行迹可能与造迹生物在转弯处的运动惯性或与水动力造成造迹生物身体的倾斜有关。含丰富节肢动物遗迹的凯里生物群的沉积环境为正常浪基面和风暴浪基面之间的浅海软质基底低能环境。Abundant arthropods tracks, including Beaconichnus , Cruziana , Did ymaulichnus , Dimorphichnus , Diplichnites, Monoaulichnus (n. igen. ), Monomorphichnus, Parallehelcura and Rusophycus, have been fond in the Lower--Middle Cambrian Kaili Formation at Balang Village, Jianhe County, Guizhou Province, China. The arthropods tracks described herein contain 9 ichnogenera, 23 ichnospecies, of which 1 ichnogenera and 9 ichnospecies are new. The preying and courting tracks produced by trilobites (or arthropods) are found in the Kaili Formation. The track transformations of the arthropods moving tracks have two changes: from resting trace to furrowing trace to walking trace to swimming trace, and from swimming trace to walking trace to furrowing trace to resting trace. The transforming tracks in turnings reasoned that the bodies of track-makers were tilted due to the water energy or the moving inertia in turnings. The Kaili Formation yielding the Kaili ichnocoenosis was deposited in shallow sea with lower energy and softground, between daily wave base and storm wave base.
关 键 词:节肢动物遗迹 遗迹群落 凯里组 寒武纪 贵州剑河
分 类 号:Q915[天文地球—古生物学与地层学]
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