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Spatiotemporal patterns in the export of dissolved organic carbon and chromophoric dissolved organic matter from a coastal, blackwater river
We examined seasonal and spatial patterns in dissolved organic carbon (DOC) and chromophoric dissolved organic matter (CDOM) in the Chowan River watershed, North Carolina, a blackwater river which discharges into the second largest estuary in the United States, the Albemarle–Pamlico Estuarine System...
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Published in: | Aquatic sciences 2016-10, Vol.78 (4), p.823-836 |
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description | We examined seasonal and spatial patterns in dissolved organic carbon (DOC) and chromophoric dissolved organic matter (CDOM) in the Chowan River watershed, North Carolina, a blackwater river which discharges into the second largest estuary in the United States, the Albemarle–Pamlico Estuarine System. From April 2008 to May 2010, DOC concentration did not significantly vary across seasons (range 7.69–30.39 mg L
−1
); however, CDOM molecular size and aromaticity increased throughout the spring, decreased during the summer and fall, and remained relatively low in the winter. Spectral slope ratios suggested microbial processing of CDOM in the spring and photodegradation of CDOM in the summer and fall. Spatially, DOC and CDOM concentrations were similar in the mainstem and at the mouths of two tributaries, Bennetts Creek and Wiccacon River, but were significantly higher upstream on the tributaries. DOC concentration was positively correlated with CDOM absorbance coefficients at 254 and 350 nm; however, these optical proxies explained only ~60 % of the variance. DOC and CDOM absorption loads to the Albemarle Sound ranged from 2.63 × 10
10
g year
−1
and 9.84 × 10
10
m
2
year
−1
, respectively, in a dry year and 7.9 × 10
10
g year
−1
and 2.2 × 10
11
m
2
year
−1
, respectively, in a wet year, which are comparable to non-blackwater rivers with larger watersheds. Blackwater rivers may therefore represent “hotspots” in coastal carbon chemistry, with seasonal variations in the quality and quantity of DOC and CDOM influencing estuarine food web dynamics and net ecosystem metabolism. |
doi_str_mv | 10.1007/s00027-016-0474-3 |
format | article |
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−1
); however, CDOM molecular size and aromaticity increased throughout the spring, decreased during the summer and fall, and remained relatively low in the winter. Spectral slope ratios suggested microbial processing of CDOM in the spring and photodegradation of CDOM in the summer and fall. Spatially, DOC and CDOM concentrations were similar in the mainstem and at the mouths of two tributaries, Bennetts Creek and Wiccacon River, but were significantly higher upstream on the tributaries. DOC concentration was positively correlated with CDOM absorbance coefficients at 254 and 350 nm; however, these optical proxies explained only ~60 % of the variance. DOC and CDOM absorption loads to the Albemarle Sound ranged from 2.63 × 10
10
g year
−1
and 9.84 × 10
10
m
2
year
−1
, respectively, in a dry year and 7.9 × 10
10
g year
−1
and 2.2 × 10
11
m
2
year
−1
, respectively, in a wet year, which are comparable to non-blackwater rivers with larger watersheds. Blackwater rivers may therefore represent “hotspots” in coastal carbon chemistry, with seasonal variations in the quality and quantity of DOC and CDOM influencing estuarine food web dynamics and net ecosystem metabolism.</description><identifier>ISSN: 1015-1621</identifier><identifier>EISSN: 1420-9055</identifier><identifier>DOI: 10.1007/s00027-016-0474-3</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Biomedical and Life Sciences ; Carbon ; Dissolved organic carbon ; Dissolved organic matter ; Ecology ; Estuaries ; Freshwater & Marine Ecology ; Life Sciences ; Marine & Freshwater Sciences ; Oceanography ; Photodegradation ; Research Article ; River ecology ; Rivers ; Seasonal variations ; Sediment transport ; Spatial analysis ; Spring ; Summer ; Tributaries ; Watersheds</subject><ispartof>Aquatic sciences, 2016-10, Vol.78 (4), p.823-836</ispartof><rights>Springer International Publishing 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c415t-261fc5a55ac56af7090fcf3de5cb984ba628cdfef504dfe44e0bfac747ab91b33</citedby><cites>FETCH-LOGICAL-c415t-261fc5a55ac56af7090fcf3de5cb984ba628cdfef504dfe44e0bfac747ab91b33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27922,27923</link.rule.ids></links><search><creatorcontrib>Leech, Dina M.</creatorcontrib><creatorcontrib>Ensign, Scott H.</creatorcontrib><creatorcontrib>Piehler, Michael F.</creatorcontrib><title>Spatiotemporal patterns in the export of dissolved organic carbon and chromophoric dissolved organic matter from a coastal, blackwater river</title><title>Aquatic sciences</title><addtitle>Aquat Sci</addtitle><description>We examined seasonal and spatial patterns in dissolved organic carbon (DOC) and chromophoric dissolved organic matter (CDOM) in the Chowan River watershed, North Carolina, a blackwater river which discharges into the second largest estuary in the United States, the Albemarle–Pamlico Estuarine System. From April 2008 to May 2010, DOC concentration did not significantly vary across seasons (range 7.69–30.39 mg L
−1
); however, CDOM molecular size and aromaticity increased throughout the spring, decreased during the summer and fall, and remained relatively low in the winter. Spectral slope ratios suggested microbial processing of CDOM in the spring and photodegradation of CDOM in the summer and fall. Spatially, DOC and CDOM concentrations were similar in the mainstem and at the mouths of two tributaries, Bennetts Creek and Wiccacon River, but were significantly higher upstream on the tributaries. DOC concentration was positively correlated with CDOM absorbance coefficients at 254 and 350 nm; however, these optical proxies explained only ~60 % of the variance. DOC and CDOM absorption loads to the Albemarle Sound ranged from 2.63 × 10
10
g year
−1
and 9.84 × 10
10
m
2
year
−1
, respectively, in a dry year and 7.9 × 10
10
g year
−1
and 2.2 × 10
11
m
2
year
−1
, respectively, in a wet year, which are comparable to non-blackwater rivers with larger watersheds. Blackwater rivers may therefore represent “hotspots” in coastal carbon chemistry, with seasonal variations in the quality and quantity of DOC and CDOM influencing estuarine food web dynamics and net ecosystem metabolism.</description><subject>Biomedical and Life Sciences</subject><subject>Carbon</subject><subject>Dissolved organic carbon</subject><subject>Dissolved organic matter</subject><subject>Ecology</subject><subject>Estuaries</subject><subject>Freshwater & Marine Ecology</subject><subject>Life Sciences</subject><subject>Marine & Freshwater Sciences</subject><subject>Oceanography</subject><subject>Photodegradation</subject><subject>Research Article</subject><subject>River ecology</subject><subject>Rivers</subject><subject>Seasonal variations</subject><subject>Sediment transport</subject><subject>Spatial analysis</subject><subject>Spring</subject><subject>Summer</subject><subject>Tributaries</subject><subject>Watersheds</subject><issn>1015-1621</issn><issn>1420-9055</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp1kctKxDAUhosoOI4-gLuAGxdWz2mTXpYyeAPBhboOp2niVNumJh0v7-BDmzouRHF1bt_5-eGPon2EYwTITzwAJHkMmMXAcx6nG9EMeQJxCUJshh5QxJgluB3teP8IgEmRF7Po43agsbGj7gbrqGVhGrXrPWt6Ni41029hPzJrWN14b9sXXTPrHqhvFFPkKtsz6mumls52dlhaF_Z_ye5LlZkAMWLKkh-pPWJVS-rplaaTa1602422DLVe733XeXR_fna3uIyvby6uFqfXseIoxjjJ0ChBQpASGZkcSjDKpLUWqioLXlGWFKo22gjgoXCuoTKkcp5TVWKVpvPocK07OPu80n6UXeOVblvqtV15iQWWyIUQGNCDX-ijXbk-uJsoXohEcBEoXFPKWe-dNnJwTUfuXSLIKR-5zkeGfOSUj5xMJOsfH9j-Qbsfyv8-fQL_ApbF</recordid><startdate>20161001</startdate><enddate>20161001</enddate><creator>Leech, Dina M.</creator><creator>Ensign, Scott H.</creator><creator>Piehler, Michael F.</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7SN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>20161001</creationdate><title>Spatiotemporal patterns in the export of dissolved organic carbon and chromophoric dissolved organic matter from a coastal, blackwater river</title><author>Leech, Dina M. ; Ensign, Scott H. ; Piehler, Michael F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c415t-261fc5a55ac56af7090fcf3de5cb984ba628cdfef504dfe44e0bfac747ab91b33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Biomedical and Life Sciences</topic><topic>Carbon</topic><topic>Dissolved organic carbon</topic><topic>Dissolved organic matter</topic><topic>Ecology</topic><topic>Estuaries</topic><topic>Freshwater & Marine Ecology</topic><topic>Life Sciences</topic><topic>Marine & Freshwater Sciences</topic><topic>Oceanography</topic><topic>Photodegradation</topic><topic>Research Article</topic><topic>River ecology</topic><topic>Rivers</topic><topic>Seasonal variations</topic><topic>Sediment transport</topic><topic>Spatial analysis</topic><topic>Spring</topic><topic>Summer</topic><topic>Tributaries</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Leech, Dina M.</creatorcontrib><creatorcontrib>Ensign, Scott H.</creatorcontrib><creatorcontrib>Piehler, Michael F.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Science Journals</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic 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><collection>ProQuest Central Basic</collection><jtitle>Aquatic sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Leech, Dina M.</au><au>Ensign, Scott H.</au><au>Piehler, Michael F.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatiotemporal patterns in the export of dissolved organic carbon and chromophoric dissolved organic matter from a coastal, blackwater river</atitle><jtitle>Aquatic sciences</jtitle><stitle>Aquat Sci</stitle><date>2016-10-01</date><risdate>2016</risdate><volume>78</volume><issue>4</issue><spage>823</spage><epage>836</epage><pages>823-836</pages><issn>1015-1621</issn><eissn>1420-9055</eissn><abstract>We examined seasonal and spatial patterns in dissolved organic carbon (DOC) and chromophoric dissolved organic matter (CDOM) in the Chowan River watershed, North Carolina, a blackwater river which discharges into the second largest estuary in the United States, the Albemarle–Pamlico Estuarine System. From April 2008 to May 2010, DOC concentration did not significantly vary across seasons (range 7.69–30.39 mg L
−1
); however, CDOM molecular size and aromaticity increased throughout the spring, decreased during the summer and fall, and remained relatively low in the winter. Spectral slope ratios suggested microbial processing of CDOM in the spring and photodegradation of CDOM in the summer and fall. Spatially, DOC and CDOM concentrations were similar in the mainstem and at the mouths of two tributaries, Bennetts Creek and Wiccacon River, but were significantly higher upstream on the tributaries. DOC concentration was positively correlated with CDOM absorbance coefficients at 254 and 350 nm; however, these optical proxies explained only ~60 % of the variance. DOC and CDOM absorption loads to the Albemarle Sound ranged from 2.63 × 10
10
g year
−1
and 9.84 × 10
10
m
2
year
−1
, respectively, in a dry year and 7.9 × 10
10
g year
−1
and 2.2 × 10
11
m
2
year
−1
, respectively, in a wet year, which are comparable to non-blackwater rivers with larger watersheds. Blackwater rivers may therefore represent “hotspots” in coastal carbon chemistry, with seasonal variations in the quality and quantity of DOC and CDOM influencing estuarine food web dynamics and net ecosystem metabolism.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s00027-016-0474-3</doi><tpages>14</tpages></addata></record> |
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subjects | Biomedical and Life Sciences Carbon Dissolved organic carbon Dissolved organic matter Ecology Estuaries Freshwater & Marine Ecology Life Sciences Marine & Freshwater Sciences Oceanography Photodegradation Research Article River ecology Rivers Seasonal variations Sediment transport Spatial analysis Spring Summer Tributaries Watersheds |
title | Spatiotemporal patterns in the export of dissolved organic carbon and chromophoric dissolved organic matter from a coastal, blackwater river |
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