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Dust impact on marine biota and atmospheric CO2 during glacial periods
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| Zeitschriftentitel: | Paleoceanography |
|---|---|
| Personen und Körperschaften: | , , , |
| In: | Paleoceanography, 18, 2003, 2 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
American Geophysical Union (AGU)
|
| Schlagwörter: |
| author_facet |
Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier |
|---|---|
| author |
Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier |
| spellingShingle |
Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier Paleoceanography Dust impact on marine biota and atmospheric CO2 during glacial periods Paleontology Oceanography |
| author_sort |
bopp, laurent |
| spelling |
Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier 0883-8305 1944-9186 American Geophysical Union (AGU) Paleontology Oceanography http://dx.doi.org/10.1029/2002pa000810 <jats:p>We assess the impact of high dust deposition rates on marine biota and atmospheric CO<jats:sub>2</jats:sub> using a state‐of‐the‐art ocean biogeochemistry model and observations. Our model includes an explicit representation of two groups of phytoplankton and colimitation by iron, silicate, and phosphate. When high dust deposition rates from the Last Glacial Maximum (LGM) are used as input, our model shows an increase in the relative abundance of diatoms in today's iron‐limited regions, causing a global increase in export production by 6% and an atmospheric CO<jats:sub>2</jats:sub> drawdown of 15 ppm. When the combined effects of changes in dust, temperature, ice cover, and circulation are included, the model reproduces roughly our reconstruction of regional changes in export production during the LGM based on several paleoceanographic indicators. In particular, the model reproduces the latitudinal dipole in the Southern Ocean, driven in our simulations by the conjunction of dust, sea ice, and circulation changes. In the North Pacific the limited open ocean data suggest that we correctly simulate the east‐west gradient in the open ocean, but more data are needed to confirm this result. From our model‐data comparison and from the timing of the dust record at Vostok, we argue that our model estimate of the role of dust is realistic and that the maximum impact of high dust deposition on atmospheric CO<jats:sub>2</jats:sub> must be <30 ppm.</jats:p> Dust impact on marine biota and atmospheric CO<sub>2</sub> during glacial periods Paleoceanography |
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| title |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_unstemmed |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_full |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_fullStr |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_full_unstemmed |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_short |
Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_sort |
dust impact on marine biota and atmospheric co<sub>2</sub> during glacial periods |
| topic |
Paleontology Oceanography |
| url |
http://dx.doi.org/10.1029/2002pa000810 |
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2003 |
| physical |
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| description |
<jats:p>We assess the impact of high dust deposition rates on marine biota and atmospheric CO<jats:sub>2</jats:sub> using a state‐of‐the‐art ocean biogeochemistry model and observations. Our model includes an explicit representation of two groups of phytoplankton and colimitation by iron, silicate, and phosphate. When high dust deposition rates from the Last Glacial Maximum (LGM) are used as input, our model shows an increase in the relative abundance of diatoms in today's iron‐limited regions, causing a global increase in export production by 6% and an atmospheric CO<jats:sub>2</jats:sub> drawdown of 15 ppm. When the combined effects of changes in dust, temperature, ice cover, and circulation are included, the model reproduces roughly our reconstruction of regional changes in export production during the LGM based on several paleoceanographic indicators. In particular, the model reproduces the latitudinal dipole in the Southern Ocean, driven in our simulations by the conjunction of dust, sea ice, and circulation changes. In the North Pacific the limited open ocean data suggest that we correctly simulate the east‐west gradient in the open ocean, but more data are needed to confirm this result. From our model‐data comparison and from the timing of the dust record at Vostok, we argue that our model estimate of the role of dust is realistic and that the maximum impact of high dust deposition on atmospheric CO<jats:sub>2</jats:sub> must be <30 ppm.</jats:p> |
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| author | Bopp, Laurent, Kohfeld, Karen E., Le Quéré, Corinne, Aumont, Olivier |
| author_facet | Bopp, Laurent, Kohfeld, Karen E., Le Quéré, Corinne, Aumont, Olivier, Bopp, Laurent, Kohfeld, Karen E., Le Quéré, Corinne, Aumont, Olivier |
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| description | <jats:p>We assess the impact of high dust deposition rates on marine biota and atmospheric CO<jats:sub>2</jats:sub> using a state‐of‐the‐art ocean biogeochemistry model and observations. Our model includes an explicit representation of two groups of phytoplankton and colimitation by iron, silicate, and phosphate. When high dust deposition rates from the Last Glacial Maximum (LGM) are used as input, our model shows an increase in the relative abundance of diatoms in today's iron‐limited regions, causing a global increase in export production by 6% and an atmospheric CO<jats:sub>2</jats:sub> drawdown of 15 ppm. When the combined effects of changes in dust, temperature, ice cover, and circulation are included, the model reproduces roughly our reconstruction of regional changes in export production during the LGM based on several paleoceanographic indicators. In particular, the model reproduces the latitudinal dipole in the Southern Ocean, driven in our simulations by the conjunction of dust, sea ice, and circulation changes. In the North Pacific the limited open ocean data suggest that we correctly simulate the east‐west gradient in the open ocean, but more data are needed to confirm this result. From our model‐data comparison and from the timing of the dust record at Vostok, we argue that our model estimate of the role of dust is realistic and that the maximum impact of high dust deposition on atmospheric CO<jats:sub>2</jats:sub> must be <30 ppm.</jats:p> |
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| spelling | Bopp, Laurent Kohfeld, Karen E. Le Quéré, Corinne Aumont, Olivier 0883-8305 1944-9186 American Geophysical Union (AGU) Paleontology Oceanography http://dx.doi.org/10.1029/2002pa000810 <jats:p>We assess the impact of high dust deposition rates on marine biota and atmospheric CO<jats:sub>2</jats:sub> using a state‐of‐the‐art ocean biogeochemistry model and observations. Our model includes an explicit representation of two groups of phytoplankton and colimitation by iron, silicate, and phosphate. When high dust deposition rates from the Last Glacial Maximum (LGM) are used as input, our model shows an increase in the relative abundance of diatoms in today's iron‐limited regions, causing a global increase in export production by 6% and an atmospheric CO<jats:sub>2</jats:sub> drawdown of 15 ppm. When the combined effects of changes in dust, temperature, ice cover, and circulation are included, the model reproduces roughly our reconstruction of regional changes in export production during the LGM based on several paleoceanographic indicators. In particular, the model reproduces the latitudinal dipole in the Southern Ocean, driven in our simulations by the conjunction of dust, sea ice, and circulation changes. In the North Pacific the limited open ocean data suggest that we correctly simulate the east‐west gradient in the open ocean, but more data are needed to confirm this result. From our model‐data comparison and from the timing of the dust record at Vostok, we argue that our model estimate of the role of dust is realistic and that the maximum impact of high dust deposition on atmospheric CO<jats:sub>2</jats:sub> must be <30 ppm.</jats:p> Dust impact on marine biota and atmospheric CO<sub>2</sub> during glacial periods Paleoceanography |
| spellingShingle | Bopp, Laurent, Kohfeld, Karen E., Le Quéré, Corinne, Aumont, Olivier, Paleoceanography, Dust impact on marine biota and atmospheric CO2 during glacial periods, Paleontology, Oceanography |
| title | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_full | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_fullStr | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_full_unstemmed | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_short | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| title_sort | dust impact on marine biota and atmospheric co<sub>2</sub> during glacial periods |
| title_unstemmed | Dust impact on marine biota and atmospheric CO2 during glacial periods |
| topic | Paleontology, Oceanography |
| url | http://dx.doi.org/10.1029/2002pa000810 |