Abstract: The Steptoean Positive Carbon Isotope Excursion (SPICE) is found in the Machari Formation which was interpreted to have been deposited on the middle to outer carbonate ramp environment. The Machari Formation is the Middle to Late Cambrian in age and distributed in the Yeongweol area, Gangweon Province, Korea. The SPICE event in the Machari Formation begins with the first appearance datum of trilobite Glyptagnostus reticulatus and ends with the first appearance of datum of trilobite Irvingella. The SPICE is found in approximately 120 m thick sequence and δ 13 C values in the SPICE interval range from 0.6 to 4.4‰. The SPICE in the Machari Formation is interpreted to be caused by burial of organic matter in the sea floor and subseque...
金沢大学理工研究域理工研究域地球社会基盤学系A time-diagnostic positive excursion (∼1‰) of carbon isotope ratio (δ13C) reco...
An integrated, high-resolution chemostratigraphic (C, O and Sr isotopes) and magnetostratigraphic st...
The carbon isotope of total carbon (δ13Corg), long-chain n-alkanes, and their compound-specifi...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a large (≥4‰ shift) positive carbon isot...
Cambrian carbonates with abundant fossils of agnostoid trilobites deposited on the southern slope (J...
Sedimentary rocks from the Ediacaran-Cambrian boundary record important biological, climatic and geo...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] Several positive carbon isot...
The Middle–Upper Cambrian Xixiangchi Group in the Sichuan Basin is mainly a set of dolomites of plat...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
A positive delta C-13 excursion in Palaeoproterozoic carbonate sequences in Henan, China is reported...
The late Cambrian Steptoean positive carbon isotope excursion (SPICE) represents a major perturbatio...
Global occurrences of Steptoean Positive Carbon Isotope Excursion (SPICE) during Late Cambrian recor...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a prominent +4–5‰ shift in the Cambrian ...
The Cambrian Series 2–Miaolingian transition is a pivotal period during Earth history, which witness...
金沢大学大学院自然科学研究科環境動態金沢大学理学部A positive carbon isotopic excursion across the Cenomanian/Turonian boundar...
金沢大学理工研究域理工研究域地球社会基盤学系A time-diagnostic positive excursion (∼1‰) of carbon isotope ratio (δ13C) reco...
An integrated, high-resolution chemostratigraphic (C, O and Sr isotopes) and magnetostratigraphic st...
The carbon isotope of total carbon (δ13Corg), long-chain n-alkanes, and their compound-specifi...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a large (≥4‰ shift) positive carbon isot...
Cambrian carbonates with abundant fossils of agnostoid trilobites deposited on the southern slope (J...
Sedimentary rocks from the Ediacaran-Cambrian boundary record important biological, climatic and geo...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] Several positive carbon isot...
The Middle–Upper Cambrian Xixiangchi Group in the Sichuan Basin is mainly a set of dolomites of plat...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
A positive delta C-13 excursion in Palaeoproterozoic carbonate sequences in Henan, China is reported...
The late Cambrian Steptoean positive carbon isotope excursion (SPICE) represents a major perturbatio...
Global occurrences of Steptoean Positive Carbon Isotope Excursion (SPICE) during Late Cambrian recor...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a prominent +4–5‰ shift in the Cambrian ...
The Cambrian Series 2–Miaolingian transition is a pivotal period during Earth history, which witness...
金沢大学大学院自然科学研究科環境動態金沢大学理学部A positive carbon isotopic excursion across the Cenomanian/Turonian boundar...
金沢大学理工研究域理工研究域地球社会基盤学系A time-diagnostic positive excursion (∼1‰) of carbon isotope ratio (δ13C) reco...
An integrated, high-resolution chemostratigraphic (C, O and Sr isotopes) and magnetostratigraphic st...
The carbon isotope of total carbon (δ13Corg), long-chain n-alkanes, and their compound-specifi...