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The environmental conditions and the biotic crisis during the Permo-Triassic (Tr/P) transition received increasing attention in the past decades. Presented herein are the molecular fossil records of cyano-bacteria and green sulfur bacteria,the base of the marine ecosystem,to highlight the episodic nature of both the environment and the biotic crisis during this critical period. At least two episodes of cyano-bacterial expansion are documented by 2-methylhopanes ranging from C28 to C32 in carbon number,indicative of the instable marine ecosystem and the fluctuant aquatic nutrients. Meanwhile,the index of 2-alkyl-1,3,4-trimethylbenzenes (biomarkers of green sulfur bacteria) and the ratio of pristane to phy-tane (Pr/Ph) witness the fluctuation of sedimentary environmental redox conditions. The above mo-lecular evidence suggests the occurrence of highly fluctuating environmental conditions during the Tr/P transition,which is consistent with,and probably the cause of,the multi-phased biotic crisis and the prolonged faunal recovery.
The environmental conditions and the biotic crisis during the Permo-Triassic (Tr / P) transition received attention in the past decades. Presented herein are the molecular fossil records of cyano-bacteria and green sulfur bacteria, the base of the marine ecosystem, to highlight the episodic nature of both the environment and the biotic crisis during this critical period. At least two episodes of cyano-bacterial expansion were documented by 2-methylhopanes ranging from C28 to C32 in carbon number, indicative of the instable marine ecosystem and the fluctuant aquatic nutrients. Meanwhile, the index of 2-alkyl-1,3,4-trimethylbenzenes (biomarkers of green sulfur bacteria) and the ratio of pristane to phytast (Pr / Ph) witness the fluctuation of sedimentary environmental redox conditions. above mo-lecular evidence suggests the occurrence of highly fluctuating environmental conditions during the Tr / P transition, which is consistent with, and probably the cause of, the multi-phased biotic crisis and the prolonged faunal recovery