Molecular underpinnings and biogeochemical consequences of enhanced diatom growth in a warming Southern Ocean.
Molecular underpinnings and biogeochemical consequences of enhanced diatom growth in a warming Southern Ocean.
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DOI:
10.1073/pnas.2107238118
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发表时间:
2021-07-27
影响因子:
11.1
通讯作者:
Bertrand EM
中科院分区:
文献类型:
--
作者:
Jabre LJ;Allen AE;McCain JSP;McCrow JP;Tenenbaum N;Spackeen JL;Sipler RE;Green BR;Bronk DA;Hutchins DA;Bertrand EM
Phytoplankton contribute to the Southern Ocean’s (SO) ability to absorb atmospheric CO2 and shape the stoichiometry of northward macronutrient delivery. Climate change is altering the SO environment, yet we know little about how resident phytoplankton will react to these changes. Here, we studied a natural SO community and compared responses of two prevalent, bloom-forming diatom groups to changes in temperature and iron that are projected to occur by 2100 to 2300. We found that one group, Pseudo-nitzschia, grows better under warmer low-iron conditions by managing cellular iron demand and efficiently increasing photosynthetic capacity. This ability to grow and draw down nutrients in the face of warming, regardless of iron availability, has major implications for ocean ecosystems and global nutrient cycles. The Southern Ocean (SO) harbors some of the most intense phytoplankton blooms on Earth. Changes in temperature and iron availability are expected to alter the intensity of SO phytoplankton blooms, but little is known about how these changes will influence community composition and downstream biogeochemical processes. We performed light-saturated experimental manipulations on surface ocean microbial communities from McMurdo Sound in the Ross Sea to examine the effects of increased iron availability (+2 nM) and warming (+3 and +6 °C) on nutrient uptake, as well as the growth and transcriptional responses of two dominant diatoms, Fragilariopsis and Pseudo-nitzschia. We found that community nutrient uptake and primary productivity were elevated under both warming conditions without iron addition (relative to ambient −0.5 °C). This effect was greater than additive under concurrent iron addition and warming. Pseudo-nitzschia became more abundant under warming without added iron (especially at 6 °C), while Fragilariopsis only became more abundant under warming in the iron-added treatments. We attribute the apparent advantage Pseudo-nitzschia shows under warming to up-regulation of iron-conserving photosynthetic processes, utilization of iron-economic nitrogen assimilation mechanisms, and increased iron uptake and storage. These data identify important molecular and physiological differences between dominant diatom groups and add to the growing body of evidence for Pseudo-nitzschia’s increasingly important role in warming SO ecosystems. This study also suggests that temperature-driven shifts in SO phytoplankton assemblages may increase utilization of the vast pool of excess nutrients in iron-limited SO surface waters and thereby influence global nutrient distribution and carbon cycling.
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影响因子:
4.9
作者:
Frolicher, Thomas L.;Sarmiento, Jorge L.;Winton, Michael
通讯作者:
Winton, Michael
影响因子:
3.7
作者:
Andrew, Sarah M.;Morell, Hugh T.;Ellwood, Michael J.
通讯作者:
Ellwood, Michael J.
DOI:
10.1073/pnas.1309345110
发表时间:
2013-12-17
影响因子:
11.1
作者:
Assmy, Philipp;Smetacek, Victor;Wolf-Gladrow, Dieter
通讯作者:
Wolf-Gladrow, Dieter
影响因子:
3.7
作者:
Coello-Camba, Alexandra;Agusti, Susana
通讯作者:
Agusti, Susana
影响因子:
4.5
作者:
Cohen, Natalie R.;Mann, Elizabeth;Marchetti, Adrian
通讯作者:
Marchetti, Adrian