Permian-Triassic boundary interval in the Middle East (Iran and N. Oman) : Progressive environmental change from detailed carbonate carbon isotope marine curve and sedimentary evolution
The end Permian negative δ13C excursion is well known but its cause and chronology are still in question. In an attempt to decipher the timing and reasons for this strong decrease, we established high-resolution sedimentological, biostratigraphical and carbonate carbon isotopic studies in four sections in Iran (Abadeh, Shareeza, Zal and Djulfa) and two in Oman (Wadi Sahtan). The position of the se
