Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters
Substantial increases in the concentrations of the stronger of two Fe(III) complexing organic ligand classes measured during the mesoscale Fe enrichment studies IronEx II and SOIREE appeared to sharply curtailed Fe availability to diatoms and thus limited the efficiency of carbon sequestration to th...
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ftunivnotexas:info:ark/67531/metadc896358 2023-05-15T18:25:39+02:00 Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters Cochlan, William P. United States. Department of Energy. Office of Science. 2008-06-13 9 pages Text https://doi.org/10.2172/929692 http://digital.library.unt.edu/ark:/67531/metadc896358/ English eng San Francisco State University rep-no: DOEER63430 grantno: FG02-02ER63430 doi:10.2172/929692 osti: 929692 http://digital.library.unt.edu/ark:/67531/metadc896358/ ark: ark:/67531/metadc896358 Efficiency Monitoring Pacific Ocean Diatoms Carbon Cycle Ecosystems Cyanobacteria Seawater 54 Environmental Sciences Iron Carbon Availability Carbon Sequestration Report 2008 ftunivnotexas https://doi.org/10.2172/929692 2016-11-05T23:11:58Z Substantial increases in the concentrations of the stronger of two Fe(III) complexing organic ligand classes measured during the mesoscale Fe enrichment studies IronEx II and SOIREE appeared to sharply curtailed Fe availability to diatoms and thus limited the efficiency of carbon sequestration to the deep. Detailed observations during IronEx II (equatorial Pacific Ocean) and SOIREE (Southern Ocean –Pacific sector) indicate that the diatoms began re-experiencing Fe stress even though dissolved Fe concentrations remained elevated in the patch. This surprising outcome likely is related to the observed increased concentrations of strong Fe(III)-complexing ligands in seawater. Preliminary findings from other studies indicate that diatoms may not readily obtain Fe from these chemical species whereas Fe bound by strong ligands appears to support growth of cyanobacteria and nanoflagellates. The difficulty in assessing the likelihood of these changes with in-situ mesoscale experiments is the extended monitoring period needed to capture the long-term trajectory of the carbon cycle. A more detailed understanding of Fe complexing ligand effects on long-term ecosystem structure and carbon cycling is essential to ascertain not only the effect of Fe enrichment on short-term carbon sequestration in the oceans, but also the potential effect of Fe enrichment in modifying ecosystem structure and trajectory. Report Southern Ocean University of North Texas: UNT Digital Library Pacific Southern Ocean |
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Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Efficiency Monitoring Pacific Ocean Diatoms Carbon Cycle Ecosystems Cyanobacteria Seawater 54 Environmental Sciences Iron Carbon Availability Carbon Sequestration |
spellingShingle |
Efficiency Monitoring Pacific Ocean Diatoms Carbon Cycle Ecosystems Cyanobacteria Seawater 54 Environmental Sciences Iron Carbon Availability Carbon Sequestration Cochlan, William P. Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
topic_facet |
Efficiency Monitoring Pacific Ocean Diatoms Carbon Cycle Ecosystems Cyanobacteria Seawater 54 Environmental Sciences Iron Carbon Availability Carbon Sequestration |
description |
Substantial increases in the concentrations of the stronger of two Fe(III) complexing organic ligand classes measured during the mesoscale Fe enrichment studies IronEx II and SOIREE appeared to sharply curtailed Fe availability to diatoms and thus limited the efficiency of carbon sequestration to the deep. Detailed observations during IronEx II (equatorial Pacific Ocean) and SOIREE (Southern Ocean –Pacific sector) indicate that the diatoms began re-experiencing Fe stress even though dissolved Fe concentrations remained elevated in the patch. This surprising outcome likely is related to the observed increased concentrations of strong Fe(III)-complexing ligands in seawater. Preliminary findings from other studies indicate that diatoms may not readily obtain Fe from these chemical species whereas Fe bound by strong ligands appears to support growth of cyanobacteria and nanoflagellates. The difficulty in assessing the likelihood of these changes with in-situ mesoscale experiments is the extended monitoring period needed to capture the long-term trajectory of the carbon cycle. A more detailed understanding of Fe complexing ligand effects on long-term ecosystem structure and carbon cycling is essential to ascertain not only the effect of Fe enrichment on short-term carbon sequestration in the oceans, but also the potential effect of Fe enrichment in modifying ecosystem structure and trajectory. |
author2 |
United States. Department of Energy. Office of Science. |
format |
Report |
author |
Cochlan, William P. |
author_facet |
Cochlan, William P. |
author_sort |
Cochlan, William P. |
title |
Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
title_short |
Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
title_full |
Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
title_fullStr |
Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
title_full_unstemmed |
Final Technical Report: The Effects of Iron Complexing Ligands on the Long Term Ecosystem Response to Iron Enrichment of HNLC waters |
title_sort |
final technical report: the effects of iron complexing ligands on the long term ecosystem response to iron enrichment of hnlc waters |
publisher |
San Francisco State University |
publishDate |
2008 |
url |
https://doi.org/10.2172/929692 http://digital.library.unt.edu/ark:/67531/metadc896358/ |
geographic |
Pacific Southern Ocean |
geographic_facet |
Pacific Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
rep-no: DOEER63430 grantno: FG02-02ER63430 doi:10.2172/929692 osti: 929692 http://digital.library.unt.edu/ark:/67531/metadc896358/ ark: ark:/67531/metadc896358 |
op_doi |
https://doi.org/10.2172/929692 |
_version_ |
1766207250843566080 |