Phytoplankton niche generation by interspecific stoichiometric variation

被引:13
作者
Goethlich, L. [1 ]
Oschlies, A. [1 ]
机构
[1] GEOMAR, Helmholtz Ctr Ocean Res Kiel, D-24105 Kiel, Germany
关键词
CLIMATE-CHANGE; PLANKTON; PARADOX; MODEL; BIODIVERSITY; OSCILLATIONS; CHLOROPHYLL; COMMUNITIES; LIMITATION; DIVERSITY;
D O I
10.1029/2011GB004042
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
For marine biogeochemical models used in simulations of climate change scenarios, the ability to account for adaptability of marine ecosystems to environmental change becomes a concern. The potential for adaptation is expected to be larger for a diverse ecosystem compared to a monoculture of a single type of (model) algae, such as typically included in biogeochemical models. Recent attempts to simulate phytoplankton diversity in global marine ecosystem models display remarkable qualitative agreement with observed patterns of species distributions. However, modeled species diversity tends to be systematically lower than observed and, in many regions, is smaller than the number of potentially limiting nutrients. According to resource competition theory, the maximum number of coexisting species at equilibrium equals the number of limiting resources. By simulating phytoplankton communities in a chemostat model and in a global circulation model, we show here that a systematic underestimate of phytoplankton diversity may result from the standard modeling assumption of identical stoichiometry for the different phytoplankton types. Implementing stoichiometric variation among the different marine algae types in the models allows species to generate different resource supply niches via their own ecological impact. This is shown to increase the level of phytoplankton coexistence both in a chemostat model and in a global self-assembling ecosystem model.
引用
收藏
页数:8
相关论文
共 38 条
[11]   Emergent biogeography of microbial communities in a model ocean [J].
Follows, Michael J. ;
Dutkiewicz, Stephanie ;
Grant, Scott ;
Chisholm, Sallie W. .
SCIENCE, 2007, 315 (5820) :1843-1846
[12]   Redfield revisited:: variability of C:N:P in marine microalgae and its biochemical basis [J].
Geider, RJ ;
La Roche, J .
EUROPEAN JOURNAL OF PHYCOLOGY, 2002, 37 (01) :1-17
[13]   Recent trends in global ocean chlorophyll [J].
Gregg, WW ;
Casey, NW ;
McClain, CR .
GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (03) :1-5
[14]   Phytoplankton and iron: validation of a global three-dimensional ocean biogeochemical model [J].
Gregg, WW ;
Ginoux, P ;
Schopf, PS ;
Casey, NW .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2003, 50 (22-26) :3143-3169
[15]   COMPETITIVE EXCLUSION PRINCIPLE [J].
HARDIN, G .
SCIENCE, 1960, 131 (3409) :1292-1297
[16]   Climate change and marine plankton [J].
Hays, GC ;
Richardson, AJ ;
Robinson, C .
TRENDS IN ECOLOGY & EVOLUTION, 2005, 20 (06) :337-344
[17]   The Impact of Climate Change on the World's Marine Ecosystems [J].
Hoegh-Guldberg, Ove ;
Bruno, John F. .
SCIENCE, 2010, 328 (5985) :1523-1528
[18]  
Huisman J, 2001, ECOLOGY, V82, P2682
[19]   Biodiversity of plankton by species oscillations and chaos [J].
Huisman, J ;
Weissing, FJ .
NATURE, 1999, 402 (6760) :407-410
[20]  
HUTCHINSON GE, 1961, AM NAT, V95, P137, DOI 10.1086/282171