地球学报
地毬學報
지구학보
ACTA GEOSCIENTIA SINICA
2010年
2期
163-169
,共7页
姜红霞%吴亚生%刁建波%陈建阳
薑紅霞%吳亞生%刁建波%陳建暘
강홍하%오아생%조건파%진건양
全脐螺%侏儒化%灾变环境%二叠-三叠系界线%重庆北碚
全臍螺%侏儒化%災變環境%二疊-三疊繫界線%重慶北碚
전제라%주유화%재변배경%이첩-삼첩계계선%중경북배
euomphalidae%microgastropod%disastrous environment%Permian-Triassic boundary%Beibei,Chongqing
本文首次报道重庆北碚老龙洞剖面二叠-三叠系界线附近的全脐螺科的微型腹足类动物群.全脐螺科个体微小,多为盘形、圆锥形,具明显的脐,方解石质的壳壁.区分出研究层内的两类全脐螺,一类是碗形,脐宽而大,脐部深凹;壳壁厚度变化很大,螺环可能上有棱、角或瘤等装饰.另一类是胎壳呈平旋状,呈开放式旋绕;壳壁厚度均匀,未见装饰特征显示.全脐螺类为优势分子的群落在二叠纪末大绝灭事件后盛极一时,如此异常现象可能与浅海区在缺氧之后暂时改善为有氧环境有关,此后随着早三叠世腹足类的全面复苏,它们只能退居为极次要的角色.
本文首次報道重慶北碚老龍洞剖麵二疊-三疊繫界線附近的全臍螺科的微型腹足類動物群.全臍螺科箇體微小,多為盤形、圓錐形,具明顯的臍,方解石質的殼壁.區分齣研究層內的兩類全臍螺,一類是碗形,臍寬而大,臍部深凹;殼壁厚度變化很大,螺環可能上有稜、角或瘤等裝飾.另一類是胎殼呈平鏇狀,呈開放式鏇繞;殼壁厚度均勻,未見裝飾特徵顯示.全臍螺類為優勢分子的群落在二疊紀末大絕滅事件後盛極一時,如此異常現象可能與淺海區在缺氧之後暫時改善為有氧環境有關,此後隨著早三疊世腹足類的全麵複囌,它們隻能退居為極次要的角色.
본문수차보도중경북배로룡동부면이첩-삼첩계계선부근적전제라과적미형복족류동물군.전제라과개체미소,다위반형、원추형,구명현적제,방해석질적각벽.구분출연구층내적량류전제라,일류시완형,제관이대,제부심요;각벽후도변화흔대,라배가능상유릉、각혹류등장식.령일류시태각정평선상,정개방식선요;각벽후도균균,미견장식특정현시.전제라류위우세분자적군락재이첩기말대절멸사건후성겁일시,여차이상현상가능여천해구재결양지후잠시개선위유양배경유관,차후수착조삼첩세복족류적전면복소,타문지능퇴거위겁차요적각색.
This paper has reported for the first time an euomphalid microgastropod fauna from the Permian-Triassic boundary section at Laolongdong,Chongqing.The euomphalids are characterized by planispiral or trochiform shell,obvious umbilicus,and calcite composition of the shell.The euomphalid fauna flourished for a short period after the mass extinction,and its blooming might have been related to the resuming of aerobic environments after an anoxic period.However,in the following time,the abundance of euomphalids kept low and failed to play an important role in the recovery of gastropods in the Early Triassic.