Response Of Carbon Cycling To Hydroclimate Changes In The Subtropical Carbon-rich Wetland Ecosystem During The Late Pleistocene.

Y. Yang

doi:10.3997/2214-4609.202134064

oa Response Of Carbon Cycling To Hydroclimate Changes In The Subtropical Carbon-rich Wetland Ecosystem During The Late Pleistocene.
By Y. Yang¹
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Affiliations: ¹ China University Of Geosciences, , Wuhan
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 30th International Meeting on Organic Geochemistry (IMOG 2021), Sep 2021, Volume 2021, p.1 - 2
DOI: https://doi.org/10.3997/2214-4609.202134064

Abstract

Summary

A borehole core (ZK7) was collected in the Dajiuhu Basin, in the middle reaches of the Yangtze River. Lipid and bulk geochemical analyses were conducted to exploit the responses of past geochemical processes to hydroclimate changes. These preliminary results clearly showed a drastic shift of paleoecological processes during the transition from a lacustrine phase to a peat accumulating condition. More work is conducting to infer how is the methane dynamic during this shift.

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2021-09-12

2024-04-24

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References

Yu, Z., Loisel, J., Charman, D.J., et al.
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oa Response Of Carbon Cycling To Hydroclimate Changes In The Subtropical Carbon-rich Wetland Ecosystem During The Late Pleistocene.

Abstract

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Most Cited This Month Most Cited RSS feed

The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture