Stable isotopes of inorganic and organic carbon are commonly used in chemostratigraphy to correla... more Stable isotopes of inorganic and organic carbon are commonly used in chemostratigraphy to correlate marine and terrestrial sedimentary sequences based on the assumption that the carbon isotopic signature of the exogenic carbon pool dominates other sources of variability. Here, sediment samples from four Permian–Triassic boundary (PTB) sections of western Guizhou and eastern Yunnan provinces in South China, representing a terrestrial to marine transitional setting, were analyzed for δ 13 C of organic matter (δ 13 C org). These values were subsequently compared to published δ 13 C values of carbonates (δ 13 C carb) from the Global Stratotype Section and Point at Meishan and many other marine and terrestrial sections. A similar isotopic trend evident through all four sections is characterized by a negative shift of 2–3‰ at the top of the Xuanwei Formation, where we tentatively place the PTB. This negative shift also corresponds to a turnover in the vegetation and the occurrence of fungal spores, which is generally interpreted as a proliferation of decomposers and collapse of complex ecosystems during the end-Permian mass extinction event. Moreover, the absolute values of δ 13 C org are more extreme in the more distal (marine) deposits. The δ 13 C org values for the studied sediments are more variable compared to coeval δ 13 C carb records from marine records especially in the interval below the extinction horizon. We contend that the deposi-tional environment influenced the δ 13 C org values, but that the persisting geographic δ 13 C org pattern through the extinction event across the four independent sections is an indication that the atmospheric δ 13 C signal left an indelible imprint on the geologic record related to the profound ecosystem change during the end-Permian extinction event.
Well-preserved marine fossils in carbonate rocks permit detailed studies of the end-Permian extin... more Well-preserved marine fossils in carbonate rocks permit detailed studies of the end-Permian extinction event in the marine realm. However, the rarity of fossils in terrestrial depositional environments makes it more challenging to attain a satisfactory degree of resolution to describe the biotic turnover on land. Here we present new sedimentological, paleontological and geochemical (X-ray fluorescence) analysis from the study of four terrestrial sections (Chahe, Zhejue, Mide and Jiucaichong) in Western Guizhou and Eastern Yunnan (Yangtze Platform, South China) to evaluate paleoenvironmental changes through the Permian-Triassic transition.
Stable isotopes of inorganic and organic carbon are commonly used in chemostratigraphy to correla... more Stable isotopes of inorganic and organic carbon are commonly used in chemostratigraphy to correlate marine and terrestrial sedimentary sequences based on the assumption that the carbon isotopic signature of the exogenic carbon pool dominates other sources of variability. Here, sediment samples from four Permian–Triassic boundary (PTB) sections of western Guizhou and eastern Yunnan provinces in South China, representing a terrestrial to marine transitional setting, were analyzed for δ 13 C of organic matter (δ 13 C org). These values were subsequently compared to published δ 13 C values of carbonates (δ 13 C carb) from the Global Stratotype Section and Point at Meishan and many other marine and terrestrial sections. A similar isotopic trend evident through all four sections is characterized by a negative shift of 2–3‰ at the top of the Xuanwei Formation, where we tentatively place the PTB. This negative shift also corresponds to a turnover in the vegetation and the occurrence of fungal spores, which is generally interpreted as a proliferation of decomposers and collapse of complex ecosystems during the end-Permian mass extinction event. Moreover, the absolute values of δ 13 C org are more extreme in the more distal (marine) deposits. The δ 13 C org values for the studied sediments are more variable compared to coeval δ 13 C carb records from marine records especially in the interval below the extinction horizon. We contend that the deposi-tional environment influenced the δ 13 C org values, but that the persisting geographic δ 13 C org pattern through the extinction event across the four independent sections is an indication that the atmospheric δ 13 C signal left an indelible imprint on the geologic record related to the profound ecosystem change during the end-Permian extinction event.
Well-preserved marine fossils in carbonate rocks permit detailed studies of the end-Permian extin... more Well-preserved marine fossils in carbonate rocks permit detailed studies of the end-Permian extinction event in the marine realm. However, the rarity of fossils in terrestrial depositional environments makes it more challenging to attain a satisfactory degree of resolution to describe the biotic turnover on land. Here we present new sedimentological, paleontological and geochemical (X-ray fluorescence) analysis from the study of four terrestrial sections (Chahe, Zhejue, Mide and Jiucaichong) in Western Guizhou and Eastern Yunnan (Yangtze Platform, South China) to evaluate paleoenvironmental changes through the Permian-Triassic transition.
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