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Positive excursion H is consistent with the GICE.
The positive excursion of the Qilang Formation corresponded with the GICE.
The δ13Ccarb and δ18Ocarb curves in the upper Yijiangfang Formation of well S112-1 showed positive excursion features (Fig. 3).
The fluctuation range was more than the corresponding positive excursion in the global Ordovician curve (Fig. 6).
Interval C is a positive excursion, and the δ13Ccarb values fluctuate up to 1.4 ‰ from the top of the Qiaerbak Formation to the bottom of the Lianglitag Formation.
Interval A is a positive excursion, where the δ13Ccarb values shift from 0.1 to 1.3 ‰ from the top of the Yijianfang Formation to the lower Qiaerbak Formation.
Similar(43)
The environmental magnetic susceptibility shows significant enhancement in fluvial and lacustrine sediments and also shows sharp positive excursions at hiatuses where a hard crust is formed, and confirms warm and wet conditions at ∼12 ka and ∼7 ka BP.
The positive excursions have no direct relation with sea level fluctuations.
Positive excursions in pressure are controlled by the constant pressure regulator valve.
Turing pattern is formed when the α-curve has positive excursions.
Massive organic carbon burial was an important factor controlling the genesis of these positive excursions.
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