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Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages

Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages
Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages

Iron availability and temperature are important limiting factors for the biota in many areas of the world ocean, and both have been predicted to change in future climate scenarios. However, the impacts of combined changes in these two key factors on microbial trophic dynamics and nutrient cycling are unknown. We examined the relative effects of iron addition (+1 nM) and increased temperature (+4°C) on plankton assemblages of the Ross Sea, Antarctica, a region characterized by annual algal blooms and an active microbial community. Increased iron and temperature individually had consistently significant but relatively minor positive effects on total phytoplankton abundance, phytoplankton and microzooplankton community composition, as well as photosynthetic parameters and nutrient drawdown. Unexpectedly, increased iron had a consistently negative impact on microzooplankton abundance, most likely a secondary response to changes in phytoplankton community composition. When iron and temperature were increased in concert, the resulting interactive effects were greatly magnified. This synergy between iron and temperature increases would not have been predictable by examining the effects of each variable individually. Our results suggest the possibility that if iron availability increases under future climate regimes, the impacts of predicted temperature increases on plankton assemblages in polar regions could be significantly enhanced. Such synergistic and antagonistic interactions between individual climate change variables highlight the importance of multivariate studies for marine global change experiments.

1726-4170
3131-3147
Rose, J.M.
44a58751-c840-4e84-aff2-db49d5994d7f
Feng, Y.
61d40a9c-6864-49a4-a26a-c4b1b0df73c5
DiTullio, G.R.
a724c495-e556-4352-aae9-2ebb61ed536e
Dunbar, R.B.
f24660ba-5649-4bbd-88b1-55e7993a1ef8
Hare, C. E.
79e04724-f7fd-4a4d-a8e7-be4424a0c6db
Lee, P.A.
bdb8eb83-976e-4396-ab99-4d03ea0f1a2f
Lohan, M.
6ca10597-2d0f-40e8-8e4f-7619dfac5088
Long, M.
0f591e7a-892b-4e3e-9e2f-c0c4891f6786
Smith, W.O.
e261e4f0-21a9-47a4-a198-e914fc51e2d7
Sohst, B.
99417f40-f100-4abd-baf2-59f386a9c56e
Tozzi, S.
e0932789-8c2a-46c0-91df-ca8b33322746
Zhang, Y.
f812509d-2a3c-41aa-8ba1-68210952d5a6
Hutchins, D.A.
bd90dd2f-634c-4fab-a562-006da365298e
Rose, J.M.
44a58751-c840-4e84-aff2-db49d5994d7f
Feng, Y.
61d40a9c-6864-49a4-a26a-c4b1b0df73c5
DiTullio, G.R.
a724c495-e556-4352-aae9-2ebb61ed536e
Dunbar, R.B.
f24660ba-5649-4bbd-88b1-55e7993a1ef8
Hare, C. E.
79e04724-f7fd-4a4d-a8e7-be4424a0c6db
Lee, P.A.
bdb8eb83-976e-4396-ab99-4d03ea0f1a2f
Lohan, M.
6ca10597-2d0f-40e8-8e4f-7619dfac5088
Long, M.
0f591e7a-892b-4e3e-9e2f-c0c4891f6786
Smith, W.O.
e261e4f0-21a9-47a4-a198-e914fc51e2d7
Sohst, B.
99417f40-f100-4abd-baf2-59f386a9c56e
Tozzi, S.
e0932789-8c2a-46c0-91df-ca8b33322746
Zhang, Y.
f812509d-2a3c-41aa-8ba1-68210952d5a6
Hutchins, D.A.
bd90dd2f-634c-4fab-a562-006da365298e

Rose, J.M., Feng, Y., DiTullio, G.R., Dunbar, R.B., Hare, C. E., Lee, P.A., Lohan, M., Long, M., Smith, W.O., Sohst, B., Tozzi, S., Zhang, Y. and Hutchins, D.A. (2009) Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages. Biogeosciences, 6 (12), 3131-3147. (doi:10.5194/bg-6-3131-2009).

Record type: Article

Abstract

Iron availability and temperature are important limiting factors for the biota in many areas of the world ocean, and both have been predicted to change in future climate scenarios. However, the impacts of combined changes in these two key factors on microbial trophic dynamics and nutrient cycling are unknown. We examined the relative effects of iron addition (+1 nM) and increased temperature (+4°C) on plankton assemblages of the Ross Sea, Antarctica, a region characterized by annual algal blooms and an active microbial community. Increased iron and temperature individually had consistently significant but relatively minor positive effects on total phytoplankton abundance, phytoplankton and microzooplankton community composition, as well as photosynthetic parameters and nutrient drawdown. Unexpectedly, increased iron had a consistently negative impact on microzooplankton abundance, most likely a secondary response to changes in phytoplankton community composition. When iron and temperature were increased in concert, the resulting interactive effects were greatly magnified. This synergy between iron and temperature increases would not have been predictable by examining the effects of each variable individually. Our results suggest the possibility that if iron availability increases under future climate regimes, the impacts of predicted temperature increases on plankton assemblages in polar regions could be significantly enhanced. Such synergistic and antagonistic interactions between individual climate change variables highlight the importance of multivariate studies for marine global change experiments.

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More information

Accepted/In Press date: 11 November 2009
Published date: 21 December 2009

Identifiers

Local EPrints ID: 413858
URI: http://eprints.soton.ac.uk/id/eprint/413858
ISSN: 1726-4170
PURE UUID: 83cfc9cd-70ec-4401-8646-ec068102a2d3
ORCID for M. Lohan: ORCID iD orcid.org/0000-0002-5340-3108

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Date deposited: 07 Sep 2017 16:34
Last modified: 16 Mar 2024 04:13

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Contributors

Author: J.M. Rose
Author: Y. Feng
Author: G.R. DiTullio
Author: R.B. Dunbar
Author: C. E. Hare
Author: P.A. Lee
Author: M. Lohan ORCID iD
Author: M. Long
Author: W.O. Smith
Author: B. Sohst
Author: S. Tozzi
Author: Y. Zhang
Author: D.A. Hutchins

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