نمایش نتایج جستجو برای
نویسنده: Martin Schobben
موارد یافت شده: 16
1 - Gradual warming prior to the end‐Permian mass extinction (چکیده)2 - The Changhsingian (Late Permian) ammonoids from Baghuk Mountain (Central Iran) (چکیده)
3 - Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian–Triassic boundary section (چکیده)
4 - Aras Valley (northwest Iran): high-resolution stratigraphy of a continuous central Tethyan Permian–Triassic boundary section (چکیده)
5 - Latest Permian carbonate carbon isotope variability traces heterogeneous organic carbon accumulation and authigenic carbonate formation (چکیده)
6 - Pre-mass extinction decline of latest Permian Ammonoids (چکیده)
7 - Disparate Permian-Triassic carbonate-carbon isotope trends explained by a diagenetic model forced with spatially heterogeneous organic matter fluxes (چکیده)
8 - Limitations and opportunities for Permian-Triassic carbonate-carbon isotope stratigraphy posed by microbial-controlled diagenetic mineral additions (چکیده)
9 - Eutrophication, microbial-sulfate reduction and mass extinctions (چکیده)
10 - The ammonoids from the Late PermianParatirolitesLimestone of Julfa (East Azerbaijan, Iran) (چکیده)
11 - Flourishing ocean drives the end-Permian marine mass extinction (چکیده)
12 - Stable carbon and nitrogen isotopes of Permian-Triassic Boundary sections in the regions of Julfa (NW Iran) and Abadeh (Central Iran) (چکیده)
13 - The role of microbial anaerobic respiration in the end-Permian mass extinction (چکیده)
14 - High-resolution of the Changhsingian succession in Iran and correlation with China (چکیده)
15 - The Lilliput Effect in the latest Permian ammonoids from Iran (چکیده)
16 - High-resolution stratigraphy of the Changhsingian (Late Permian) successions of NW Iran and the Transcaucasus based on lithological features, conodonts and ammonoids (چکیده)
