二叠纪末生物大灭绝后 Skolithos遗迹化石的古环境意义:以豫西和尚沟组为例*
邢智峰1,2,3, 李婉颖1, 齐永安1,2,3, 郑伟1,2,3, 许欣1, 张湘赟1, 李妲1,2,3, 吴盼盼1

Paleoenvironmental significance of ichnogenus Skolithos in the aftermath of the end-Permian mass extinction: a case study of the Lower Triassic Heshanggou Formation in western Henan Province
Xing Zhi-Feng1,2,3, Li Wan-Ying1, Qi Yong-An1,2,3, Zheng Wei1,2,3, Xu Xin1, Zhang Xiang-Yun1, Li Da1,2,3, Wu Pan-Pan1
豫西下三叠统和尚沟组 Skolithos 与现代生物似 Skolithos 潜穴形态对比 A,B—虎甲虫幼虫( The tiger larvae )的垂直潜穴(据 Nascimento and Netto,2019 改);C—宜阳 Skolithos serratus 的垂直潜穴;D—蛴螬( Grub )的垂直潜穴(据 王媛媛等,2019 改);E,F—竹蛏( Solen strictus )的垂直潜穴(据 王媛媛等,2019 改);G—登封 S. verticalis 的垂直潜穴;H—螃蟹( Brachyura )的垂直潜穴(据 王海邻,2018 改);I—登封剖面, Skolithos verticalis 的垂直潜穴;J—沙蚕( Nereis succinea )的垂直潜穴(据 王海邻,2018 改);K—宜阳剖面 S. linearis 的垂直潜穴