地球学报
地毬學報
지구학보
ACTA GEOSCIENTIA SINICA
2015年
4期
385-393
,共9页
文芠%张启跃%刘俊%胡世学%周长勇%黄金元%谢韬
文芠%張啟躍%劉俊%鬍世學%週長勇%黃金元%謝韜
문문%장계약%류준%호세학%주장용%황금원%사도
罗平生物群%化石库%安尼期%复苏%巨型捕食者%生态系统
囉平生物群%化石庫%安尼期%複囌%巨型捕食者%生態繫統
라평생물군%화석고%안니기%복소%거형포식자%생태계통
Luoping Biota%Lagerst?tten%Anisian%recovery%macropredator%ecosystem
2007年,中国地质调查局成都地质调查中心云南1∶5万区域地质调查项目组在距罗平县城东南15 km的罗雄镇大洼子村附近中三叠统关岭组二段地层中发现了罗平生物群。罗平生物群目前已经发现有海生爬行类、鱼类、节肢动物、棘皮动物、菊石、双壳、腹足类、腕足类、植物等十多个大类的化石,完好地体现了当时海洋生物的多样性,是目前已知化石分异度最高的三叠纪海生化石库之一。根据含化石地层中发现的微体化石牙形石Nicoraella Kockeli带,确认罗平生物群时代为中三叠世安尼期Pelsonian亚期。罗平生物群目前发现的海生爬行类种类丰富,基本涵盖了三叠纪时期主要的海生爬行类别,包括鱼龙类、鳍龙类、原龙类以及初龙类。中生代是对海生爬行类至关重要的时期。由于一直没有发现它们留下的遗迹化石,它们的运动模式还一直存在争议。云南罗平生物群海生爬行类研究中发现数百枚保存完好的幻龙类足迹——罗平双桨迹Dikoposichnus luopingensis,为研究其运动模式提供了直接的证据。另外罗平生物群中巨型捕食者张氏幻龙Nothosaurus zhangi的发现也支持了罗平双桨迹造迹者的存在。张氏幻龙拥有三叠纪世界上最大的头骨,这些处于食物链顶层的海生爬行类的繁盛说明当时生态系统已经很完善,代表了二叠纪末生物大灭绝之后海洋生态系统的全面复苏。
2007年,中國地質調查跼成都地質調查中心雲南1∶5萬區域地質調查項目組在距囉平縣城東南15 km的囉雄鎮大窪子村附近中三疊統關嶺組二段地層中髮現瞭囉平生物群。囉平生物群目前已經髮現有海生爬行類、魚類、節肢動物、棘皮動物、菊石、雙殼、腹足類、腕足類、植物等十多箇大類的化石,完好地體現瞭噹時海洋生物的多樣性,是目前已知化石分異度最高的三疊紀海生化石庫之一。根據含化石地層中髮現的微體化石牙形石Nicoraella Kockeli帶,確認囉平生物群時代為中三疊世安尼期Pelsonian亞期。囉平生物群目前髮現的海生爬行類種類豐富,基本涵蓋瞭三疊紀時期主要的海生爬行類彆,包括魚龍類、鰭龍類、原龍類以及初龍類。中生代是對海生爬行類至關重要的時期。由于一直沒有髮現它們留下的遺跡化石,它們的運動模式還一直存在爭議。雲南囉平生物群海生爬行類研究中髮現數百枚保存完好的幻龍類足跡——囉平雙槳跡Dikoposichnus luopingensis,為研究其運動模式提供瞭直接的證據。另外囉平生物群中巨型捕食者張氏幻龍Nothosaurus zhangi的髮現也支持瞭囉平雙槳跡造跡者的存在。張氏幻龍擁有三疊紀世界上最大的頭骨,這些處于食物鏈頂層的海生爬行類的繁盛說明噹時生態繫統已經很完善,代錶瞭二疊紀末生物大滅絕之後海洋生態繫統的全麵複囌。
2007년,중국지질조사국성도지질조사중심운남1∶5만구역지질조사항목조재거라평현성동남15 km적라웅진대와자촌부근중삼첩통관령조이단지층중발현료라평생물군。라평생물군목전이경발현유해생파행류、어류、절지동물、극피동물、국석、쌍각、복족류、완족류、식물등십다개대류적화석,완호지체현료당시해양생물적다양성,시목전이지화석분이도최고적삼첩기해생화석고지일。근거함화석지층중발현적미체화석아형석Nicoraella Kockeli대,학인라평생물군시대위중삼첩세안니기Pelsonian아기。라평생물군목전발현적해생파행류충류봉부,기본함개료삼첩기시기주요적해생파행유별,포괄어룡류、기룡류、원룡류이급초룡류。중생대시대해생파행류지관중요적시기。유우일직몰유발현타문류하적유적화석,타문적운동모식환일직존재쟁의。운남라평생물군해생파행류연구중발현수백매보존완호적환룡류족적——라평쌍장적Dikoposichnus luopingensis,위연구기운동모식제공료직접적증거。령외라평생물군중거형포식자장씨환룡Nothosaurus zhangi적발현야지지료라평쌍장적조적자적존재。장씨환룡옹유삼첩기세계상최대적두골,저사처우식물련정층적해생파행류적번성설명당시생태계통이경흔완선,대표료이첩기말생물대멸절지후해양생태계통적전면복소。
The Luoping Biota was discovered in 2007 by the Chengdu Center of China Geological Survey during 1:50000 regional mapping works at Dawazi Village, Luoxiong Town, 15 km southeast of Luoping City, Yunnan Province. The interval containing the Luoping biota is the middle to upper part of Member II of the Guanling Formation. The fossil assemblage of the Luoping biota is a mixture of marine animals, terrestrial plants and a few terrestrial animals. To date, more than ten fossil groups have been recovered, which include marine reptiles, fishes, arthropods, echinoderms, ammonites, bivalves, gastropods, lingulid brachiopods, foraminifers, and plants. The Luoping Biota is one of the most diverse Triassic marine fossil Lagerst?tten records in the world. The age of the Luoping biota is assigned to the Pelsonian Substage of the Middle Triassic Anisian Stage based on the index conodontNicoraella Kockeli. Well-preserved, diverse marine reptiles are one of the highlights of the Luoping biota, including ichthyosaurs, sauropterygians, protorosaurs and archosauromorphs. Mesozoic is remarkable for marine reptiles, whose swimming modes, however, remain a topic of much controversy because of the absence of their tracks. Hundreds of seabed tracks found in Luoping Biota, which were assigned toDikoposichnus luopingensis, provide new materials for the study of their locomotive mode. Besides, the macropredator Nothosaurus zhangireported from Luoping Biota also supports the existence of the makers ofDikoposichnus luopingensis. The skull ofNothosaurus zhangi is the largest sauropterygian ever reported in Triassic. The occurrence of a different assemblage of marine reptiles as top predators in the food web indicates a well developed marine ecosystem, showing full rebuilding of the marine ecosystem after the mass extinction that happened about 250 million years ago.