|
|
|
|
|
Bauke, C.; Meier, Kjs; Kinkel, H.; Baumann, K-h. |
Coccolith calcification is known to respond to ocean acidification in culture experiments as well as in present and past oceans. Previous studies basically focus on changes in coccolith weight due to increasing CO2 and the resulting changes in the carbonate system but pay little attention to the influence of other environmental factors. In order to untangle changes in coccolithophore calcification due to environmental factors such as temperature and/or productivity from changes caused by increasing pCO2 and carbonate ion concentration we here present a study on coccolith calcification from the Holocene North Atlantic Ocean. The pre-industrial Holocene with its predominantly stable carbonate system provides the conditions for such a comprehensive analysis.... |
Tipo: Text |
|
Ano: 2013 |
URL: http://archimer.ifremer.fr/doc/00182/29278/27695.pdf |
| |
|
|
Berger, C.; Meier, K. J. S.; Kinkel, H.; Baumann, K. -h.. |
The response of coccolithophore calcification to ocean acidification has been studied in culture experiments as well as in present and past oceans. The response, however, is different between species and strains, and for the relatively small carbonate chemistry changes observed in natural environments, a uniform response of the entire coccolithophore community has not been documented so far. Moreover, previous palaeo-studies basically focus on changes in coccolith weight due to increasing CO2 and the resulting changes in the carbonate system, and only few studies focus on the influence of other environmental factors. In order to untangle changes in coccolithophore calcification due to environmental factors such as temperature and/or productivity from... |
Tipo: Text |
|
Ano: 2014 |
URL: https://archimer.ifremer.fr/doc/00291/40231/38677.pdf |
| |
|
|
|