The Permian-Triassic boundary (PTB) and the lowest Triassic in the Yangtze region are considered to be the sediments of dysaeroxic and even anoxic environments, due to the dark thin-bedded fine deposits, the highly developed parallel beddings with pyrites, the suppression of bio-disturbance, and the monotonoas fossils. However, the trace fossils there show a rather weak effect of the anoxic event. Meanwhile, the high-resolution geochemical data are analyzed with 2-cm interval in the PTB and the lowest Triassic at the Majiashan Section, Chaohu, Anhui Province. The results show that the water depth of Chaohu region in the earliest Triassic was shallow, which might be a feature of the neritic environment. The high-resolution geochemical proxies for anoxia have some contrary results. The geochemical data often indicate the dysaeroxic and even anoxic environments during that time, whereas other proxies (such as w(V)/w(Cr), w(Ni)/w(Co)) denote that they are normal marine sediments.