Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta
This study compared soil organic carbon (SOC) in wetlands dominated by native and one invasive plant specie to better understand how short-term Spartina alterniflora colonization affected carbon circulation in the Yellow River Delta (YRD). Freshwater marsh dominated by Phragmites australis ( FM ) ha...
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Veröffentlicht in: | Wetlands (Wilmington, N.C.) N.C.), 2020-12, Vol.40 (6), p.2189-2198 |
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Zusammenfassung: | This study compared soil organic carbon (SOC) in wetlands dominated by native and one invasive plant specie to better understand how short-term
Spartina alterniflora
colonization affected carbon circulation in the Yellow River Delta (YRD). Freshwater marsh dominated by
Phragmites australis
(
FM
) had the highest SOC, total nitrogen (TN), and water-extractable organic carbon (WEOC) contents, whereas SOC contents varied only slightly among salt marshes covered by
Suaeda salsa
(
SM2
),
S. alterniflora
(
SM3
) and bare flat (
MD
). Invasion by
S. alterniflora
substantially changed the molecular characteristics of SOC. The spectral characteristics of Fourier-transform infrared spectroscopy (FTIR) of humic acids (HAs) were similar from 4000 to 1800 cm
−1
but differed greatly from 1800 to 1000 cm
−1
among four wetlands. Pyrolysis-gas chromatography/mass spectrometry technology (Py-GC/MS) was used to characterize molecular fingerprints of HAs. Aliphatics (27.38%), lignin (16.64%), nitrogen-containing compounds (Nc) (16.16%), polysaccharides (16.93%), and phenol (13.42%) were dominant in
FM
, and aliphatics, alkyl, and Nc were primary in HAs from
MD
,
SM2
, and
SM3.
Lignin moieties were only found in HAs from
FM
and
SM3
, which accounted for about 16.64% and 1.6% of the total ion current, respectively. The absorption bands of the FTIR spectrum around 3340 and 1650 cm
−1
in
FM
samples were much larger than those in the other three wetlands. However, the ratio of the peak areas at 1620 and 2930 cm
−1
(
R
1620/2930
) in
SM3
, was lower than that in
MD
and
SM2
, and it meant carbon in
SM3
was less stable. Proportions of lignin and phenol moieties to total ion counts (TIC) in
MD
and
SM2
were 3.3% and 3.4%, while these proportions in FM and SM were 30% and 7.5%, respectively. It showed
S. alterniflora
invasion into salt marsh would increase SOC contents and its stability, while it will inverse if freshwater marsh was supplanted by
S. alterniflora
in the YRD. |
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ISSN: | 0277-5212 1943-6246 |
DOI: | 10.1007/s13157-020-01340-2 |