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Long-range atmospheric transport of terrestrial biomarkers to the western North Atlantic
We analyzed terrestrial plant‐derived leaf wax biomarkers in aerosols collected at Bermuda over a 2.5 years time series. Leaf waxes comprised 60–70% of extractable lipids and 0.5–1.0% of total organic carbon. Biomarker concentrations in biweekly integrated samples varied by over an order of magnitud...
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Published in: | Global biogeochemical cycles 2002-12, Vol.16 (4), p.89-1-89-17 |
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container_title | Global biogeochemical cycles |
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creator | Conte, Maureen H. Weber, J. C. |
description | We analyzed terrestrial plant‐derived leaf wax biomarkers in aerosols collected at Bermuda over a 2.5 years time series. Leaf waxes comprised 60–70% of extractable lipids and 0.5–1.0% of total organic carbon. Biomarker concentrations in biweekly integrated samples varied by over an order of magnitude and indicate that long‐range atmospheric transport is highly episodic. Results indicate that North America is the main source of terrestrial organic carbon in the western North Atlantic and that terrestrial carbon advected from Africa originates mainly in tropical C3 forests to the south of Saharan dust‐source regions. Terrestrial biomarker concentrations were poorly correlated with organic carbon concentrations, which suggest significant source differences. Variations in relative abundance of the major wax compound classes and in their carbon isotopic composition indicate that waxes in aerosols are mainly derived from ablation off living vegetation and reveal a large‐scale seasonal cycle in terrestrial biosphere emissions of wax biomarkers. |
doi_str_mv | 10.1029/2002GB001922 |
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C.</creator><creatorcontrib>Conte, Maureen H. ; Weber, J. C.</creatorcontrib><description>We analyzed terrestrial plant‐derived leaf wax biomarkers in aerosols collected at Bermuda over a 2.5 years time series. Leaf waxes comprised 60–70% of extractable lipids and 0.5–1.0% of total organic carbon. Biomarker concentrations in biweekly integrated samples varied by over an order of magnitude and indicate that long‐range atmospheric transport is highly episodic. Results indicate that North America is the main source of terrestrial organic carbon in the western North Atlantic and that terrestrial carbon advected from Africa originates mainly in tropical C3 forests to the south of Saharan dust‐source regions. Terrestrial biomarker concentrations were poorly correlated with organic carbon concentrations, which suggest significant source differences. 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Variations in relative abundance of the major wax compound classes and in their carbon isotopic composition indicate that waxes in aerosols are mainly derived from ablation off living vegetation and reveal a large‐scale seasonal cycle in terrestrial biosphere emissions of wax biomarkers.</description><subject>aerosols</subject><subject>carbon isotopes</subject><subject>Marine</subject><subject>North Atlantic</subject><subject>plant waxes</subject><subject>Saharan dust</subject><subject>terrestrial biomarkers</subject><issn>0886-6236</issn><issn>1944-9224</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNp9kMFOwzAMhiMEEmNw4wFy4kQhTZumOW4TK0hjXGBDXKImdbdCt4wk09jbk6kIceJiW_Zn6_eP0GVMbmJCxS0lhBZDQmJB6RHqxSJNo1Cmx6hH8jyLMppkp-jMuffApIyJHnqdmPUisuV6Abj0K-M2S7CNxj603MZYj02NPVgLztumbLFqzKq0H2Ad9gb7JeBdGIFd42mgl3jg23LtG32OTuqydXDxk_voZXz3PLqPJk_Fw2gwicqUkzwSXJMaGKcZh7qiaaoUaMWZzpJcC6GSmBOlasEVVEmIdUpYDKriFQNd5nnSR1fd3Y01n9sgRa4ap6ENKsBsnYzD45QxEsDrDtTWOGehlhvbhFf2MibyYJ_8a1_ASYfvmhb2_7KyGI7y7CAl6laaYMjX70pwS2Y84UzOp4V8m5GxeJzNZZ58Ax63gW4</recordid><startdate>200212</startdate><enddate>200212</enddate><creator>Conte, Maureen H.</creator><creator>Weber, J. 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C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4708-97c0fe57267efd244bbecb75c638c99b3170bbf97bed397bf4051ebd7d5eca883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>aerosols</topic><topic>carbon isotopes</topic><topic>Marine</topic><topic>North Atlantic</topic><topic>plant waxes</topic><topic>Saharan dust</topic><topic>terrestrial biomarkers</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Conte, Maureen H.</creatorcontrib><creatorcontrib>Weber, J. C.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Global biogeochemical cycles</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Conte, Maureen H.</au><au>Weber, J. C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Long-range atmospheric transport of terrestrial biomarkers to the western North Atlantic</atitle><jtitle>Global biogeochemical cycles</jtitle><addtitle>Global Biogeochem. 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subjects | aerosols carbon isotopes Marine North Atlantic plant waxes Saharan dust terrestrial biomarkers |
title | Long-range atmospheric transport of terrestrial biomarkers to the western North Atlantic |
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