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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| creator | Li, Zhe Zhang, Zhongsheng Li, Min Wu, Haitao Jiang, Ming |
| description | 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. |
| doi_str_mv | 10.1007/s13157-020-01340-2 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2919739062</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2919739062</sourcerecordid><originalsourceid>FETCH-LOGICAL-c319t-df4339485162a015d19ab2033d889e888d38b88b7284a5df99843472f9fbba8a3</originalsourceid><addsrcrecordid>eNp9kMtOwzAQRS0EEqXwA6wssTb4lcReovCUSot4CLGynMQpqYxd7LSo4udxCRI7VqOZuffO6ABwTPApwbg4i4SRrECYYoQJ4xjRHTAikjOUU57vghGmRYEySug-OIhxgTHJKSUj8HXnralXVgd41bm5CcvQuT5C38JH31k4C3PtuhqWOlTewc7BF9Nb7ZoIS782wTSw2sCp7ru1gWkMp94hN7T3SZeikqd_M_DVWOs_4UPaBHhhbK8PwV6rbTRHv3UMnq8un8obNJld35bnE1QzInvUtJwxyUWWXtaYZA2RuqKYsUYIaYQQDROVEFVBBddZ00opOOMFbWVbVVpoNgYnQ-4y-I-Vib1a-FVw6aSiksiCSZzTpKKDqg4-xmBalVC867BRBKstZDVAVgmy-oGstiY2mOKWW8L3F_2P6xsIn37c</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2919739062</pqid></control><display><type>article</type><title>Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta</title><source>ProQuest Central UK/Ireland</source><source>SpringerLink Journals - AutoHoldings</source><source>ProQuest Central</source><creator>Li, Zhe ; Zhang, Zhongsheng ; Li, Min ; Wu, Haitao ; Jiang, Ming</creator><creatorcontrib>Li, Zhe ; Zhang, Zhongsheng ; Li, Min ; Wu, Haitao ; Jiang, Ming</creatorcontrib><description>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.</description><identifier>ISSN: 0277-5212</identifier><identifier>EISSN: 1943-6246</identifier><identifier>DOI: 10.1007/s13157-020-01340-2</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Absorption spectra ; Acids ; Aquatic plants ; Biomedical and Life Sciences ; Carbon ; Chemical fingerprinting ; Chromatography ; Climate change ; Coastal Sciences ; Ecology ; Environmental Management ; Fourier transforms ; Freshwater & Marine Ecology ; Gas chromatography ; General Wetland Science ; Humic acids ; Hydrogeology ; Indigenous plants ; Infrared spectroscopy ; Invasive plants ; Ion currents ; Landscape Ecology ; Life Sciences ; Lignin ; Mass spectrometry ; Mass spectroscopy ; Native species ; Nitrogen ; Organic carbon ; Organic soils ; Phenols ; Polysaccharides ; Pyrolysis ; Respiration ; River ecology ; Rivers ; Saccharides ; Salt ; Salt marshes ; Scientific imaging ; Soil erosion ; Soils ; Spartina alterniflora ; Surface water ; Vegetation ; Water analysis ; Wetlands</subject><ispartof>Wetlands (Wilmington, N.C.), 2020-12, Vol.40 (6), p.2189-2198</ispartof><rights>Society of Wetland Scientists 2020</rights><rights>Society of Wetland Scientists 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-df4339485162a015d19ab2033d889e888d38b88b7284a5df99843472f9fbba8a3</citedby><cites>FETCH-LOGICAL-c319t-df4339485162a015d19ab2033d889e888d38b88b7284a5df99843472f9fbba8a3</cites><orcidid>0000-0001-6534-6748</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13157-020-01340-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2919739062?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,21388,27924,27925,33744,41488,42557,43805,51319,64385,64389,72469</link.rule.ids></links><search><creatorcontrib>Li, Zhe</creatorcontrib><creatorcontrib>Zhang, Zhongsheng</creatorcontrib><creatorcontrib>Li, Min</creatorcontrib><creatorcontrib>Wu, Haitao</creatorcontrib><creatorcontrib>Jiang, Ming</creatorcontrib><title>Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta</title><title>Wetlands (Wilmington, N.C.)</title><addtitle>Wetlands</addtitle><description>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.</description><subject>Absorption spectra</subject><subject>Acids</subject><subject>Aquatic plants</subject><subject>Biomedical and Life Sciences</subject><subject>Carbon</subject><subject>Chemical fingerprinting</subject><subject>Chromatography</subject><subject>Climate change</subject><subject>Coastal Sciences</subject><subject>Ecology</subject><subject>Environmental Management</subject><subject>Fourier transforms</subject><subject>Freshwater & Marine Ecology</subject><subject>Gas chromatography</subject><subject>General Wetland Science</subject><subject>Humic acids</subject><subject>Hydrogeology</subject><subject>Indigenous plants</subject><subject>Infrared spectroscopy</subject><subject>Invasive plants</subject><subject>Ion currents</subject><subject>Landscape Ecology</subject><subject>Life Sciences</subject><subject>Lignin</subject><subject>Mass spectrometry</subject><subject>Mass spectroscopy</subject><subject>Native species</subject><subject>Nitrogen</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Phenols</subject><subject>Polysaccharides</subject><subject>Pyrolysis</subject><subject>Respiration</subject><subject>River ecology</subject><subject>Rivers</subject><subject>Saccharides</subject><subject>Salt</subject><subject>Salt marshes</subject><subject>Scientific imaging</subject><subject>Soil erosion</subject><subject>Soils</subject><subject>Spartina alterniflora</subject><subject>Surface water</subject><subject>Vegetation</subject><subject>Water analysis</subject><subject>Wetlands</subject><issn>0277-5212</issn><issn>1943-6246</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kMtOwzAQRS0EEqXwA6wssTb4lcReovCUSot4CLGynMQpqYxd7LSo4udxCRI7VqOZuffO6ABwTPApwbg4i4SRrECYYoQJ4xjRHTAikjOUU57vghGmRYEySug-OIhxgTHJKSUj8HXnralXVgd41bm5CcvQuT5C38JH31k4C3PtuhqWOlTewc7BF9Nb7ZoIS782wTSw2sCp7ru1gWkMp94hN7T3SZeikqd_M_DVWOs_4UPaBHhhbK8PwV6rbTRHv3UMnq8un8obNJld35bnE1QzInvUtJwxyUWWXtaYZA2RuqKYsUYIaYQQDROVEFVBBddZ00opOOMFbWVbVVpoNgYnQ-4y-I-Vib1a-FVw6aSiksiCSZzTpKKDqg4-xmBalVC867BRBKstZDVAVgmy-oGstiY2mOKWW8L3F_2P6xsIn37c</recordid><startdate>20201201</startdate><enddate>20201201</enddate><creator>Li, Zhe</creator><creator>Zhang, Zhongsheng</creator><creator>Li, Min</creator><creator>Wu, Haitao</creator><creator>Jiang, Ming</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><orcidid>https://orcid.org/0000-0001-6534-6748</orcidid></search><sort><creationdate>20201201</creationdate><title>Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta</title><author>Li, Zhe ; Zhang, Zhongsheng ; Li, Min ; Wu, Haitao ; Jiang, Ming</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-df4339485162a015d19ab2033d889e888d38b88b7284a5df99843472f9fbba8a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Absorption spectra</topic><topic>Acids</topic><topic>Aquatic plants</topic><topic>Biomedical and Life Sciences</topic><topic>Carbon</topic><topic>Chemical fingerprinting</topic><topic>Chromatography</topic><topic>Climate change</topic><topic>Coastal Sciences</topic><topic>Ecology</topic><topic>Environmental Management</topic><topic>Fourier transforms</topic><topic>Freshwater & Marine Ecology</topic><topic>Gas chromatography</topic><topic>General Wetland Science</topic><topic>Humic acids</topic><topic>Hydrogeology</topic><topic>Indigenous plants</topic><topic>Infrared spectroscopy</topic><topic>Invasive plants</topic><topic>Ion currents</topic><topic>Landscape Ecology</topic><topic>Life Sciences</topic><topic>Lignin</topic><topic>Mass spectrometry</topic><topic>Mass spectroscopy</topic><topic>Native species</topic><topic>Nitrogen</topic><topic>Organic carbon</topic><topic>Organic soils</topic><topic>Phenols</topic><topic>Polysaccharides</topic><topic>Pyrolysis</topic><topic>Respiration</topic><topic>River ecology</topic><topic>Rivers</topic><topic>Saccharides</topic><topic>Salt</topic><topic>Salt marshes</topic><topic>Scientific imaging</topic><topic>Soil erosion</topic><topic>Soils</topic><topic>Spartina alterniflora</topic><topic>Surface water</topic><topic>Vegetation</topic><topic>Water analysis</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Zhe</creatorcontrib><creatorcontrib>Zhang, Zhongsheng</creatorcontrib><creatorcontrib>Li, Min</creatorcontrib><creatorcontrib>Wu, Haitao</creatorcontrib><creatorcontrib>Jiang, Ming</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Environmental Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><jtitle>Wetlands (Wilmington, N.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Zhe</au><au>Zhang, Zhongsheng</au><au>Li, Min</au><au>Wu, Haitao</au><au>Jiang, Ming</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta</atitle><jtitle>Wetlands (Wilmington, N.C.)</jtitle><stitle>Wetlands</stitle><date>2020-12-01</date><risdate>2020</risdate><volume>40</volume><issue>6</issue><spage>2189</spage><epage>2198</epage><pages>2189-2198</pages><issn>0277-5212</issn><eissn>1943-6246</eissn><abstract>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.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s13157-020-01340-2</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0001-6534-6748</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0277-5212 |
| ispartof | Wetlands (Wilmington, N.C.), 2020-12, Vol.40 (6), p.2189-2198 |
| issn | 0277-5212 1943-6246 |
| language | eng |
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| source | ProQuest Central UK/Ireland; SpringerLink Journals - AutoHoldings; ProQuest Central |
| subjects | Absorption spectra Acids Aquatic plants Biomedical and Life Sciences Carbon Chemical fingerprinting Chromatography Climate change Coastal Sciences Ecology Environmental Management Fourier transforms Freshwater & Marine Ecology Gas chromatography General Wetland Science Humic acids Hydrogeology Indigenous plants Infrared spectroscopy Invasive plants Ion currents Landscape Ecology Life Sciences Lignin Mass spectrometry Mass spectroscopy Native species Nitrogen Organic carbon Organic soils Phenols Polysaccharides Pyrolysis Respiration River ecology Rivers Saccharides Salt Salt marshes Scientific imaging Soil erosion Soils Spartina alterniflora Surface water Vegetation Water analysis Wetlands |
| title | Molecular Fingerprints of Soil Organic Carbon in Wetlands Covered by Native and Non-native Plants in the Yellow River Delta |
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