Whole-lake carbon-13 additions reveal terrestrial support of aquatic food webs

被引:464
作者
Pace, ML [1 ]
Cole, JJ
Carpenter, SR
Kitchell, JF
Hodgson, JR
Van de Bogert, MC
Bade, DL
Kritzberg, ES
Bastviken, D
机构
[1] Inst Ecosyst Studies, Box AB, Millbrook, NY 12545 USA
[2] Univ Wisconsin, Ctr Limnol, Madison, WI 53706 USA
[3] St Norbert Coll, Dept Biol, De Pere, WI 54115 USA
[4] Lund Univ, Dept Ecol Limnol, S-22362 Lund, Sweden
[5] Linkoping Univ, Dept Water & Environm Studies, SE-58183 Linkoping, Sweden
基金
中国国家自然科学基金; 英国自然环境研究理事会; 美国国家科学基金会;
关键词
D O I
10.1038/nature02227
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Ecosystems are supported by organic carbon from two distinct sources. Endogenous carbon is produced by photosynthesis within an ecosystem by autotrophic organisms. Exogenous carbon is produced elsewhere and transported into ecosystems. Consumers may use exogenous carbon with consequent influences on population dynamics, predator-prey relationships and ecosystem processes(1). For example, exogenous inputs provide resources that may enhance consumer abundance beyond levels supported by within-system primary production(2). Exogenous fluxes of organic carbon to ecosystems are often large, but this material is recalcitrant and difficult to assimilate, in contrast to endogenously produced organic matter, which is used more easily(3,4). Here we show, by the experimental manipulation of dissolved inorganic C-13 in two lakes, that internal primary production is insufficient to support the food webs of these ecosystems. Additions of NaH (CO3)-C-13 enriched the C-13 content of dissolved inorganic carbon, particulate organic carbon, zooplankton and fish. Dynamics of C-13 indicate that 40-55% of particulate organic carbon and 22-50% of zooplankton carbon are derived from terrestrial sources, showing that there is significant subsidy of these ecosystems by organic carbon produced outside their boundaries.
引用
收藏
页码:240 / 243
页数:4
相关论文
共 29 条
[1]  
[Anonymous], [No title captured]
[2]  
Bastviken D, 2003, ECOLOGY, V84, P969, DOI 10.1890/0012-9658(2003)084[0969:MAASOC]2.0.CO
[3]  
2
[4]   Consistent fractionation of C-13 in nature and in the laboratory: Growth-rate effects in some haptophyte algae [J].
Bidigare, RR ;
Fluegge, A ;
Freeman, KH ;
Hanson, KL ;
Hayes, JM ;
Hollander, D ;
Jasper, JP ;
King, LL ;
Laws, EA ;
Milder, J ;
Millero, FJ ;
Pancost, R ;
Popp, BN ;
Steinberg, PA ;
Wakeham, SG .
GLOBAL BIOGEOCHEMICAL CYCLES, 1997, 11 (02) :279-292
[5]  
BIRGE EA, 1927, P AM PHILOS SOC, V66, P357
[6]  
Carpenter S.R., 1993, The trophic cascades in lakes
[7]   Hydrologic variability of small, Northern Michigan lakes measured by the addition of tracers [J].
Cole, JJ ;
Pace, ML .
ECOSYSTEMS, 1998, 1 (03) :310-320
[8]   SHORT-RANGE ATMOSPHERIC TRANSPORT - A SIGNIFICANT SOURCE OF PHOSPHORUS TO AN OLIGOTROPHIC LAKE [J].
COLE, JJ ;
CARACO, NF ;
LIKENS, GE .
LIMNOLOGY AND OCEANOGRAPHY, 1990, 35 (06) :1230-1237
[9]   Pathways of organic carbon utilization in small lakes:: Results from a whole-lake 13C addition and coupled model [J].
Cole, JJ ;
Carpenter, SR ;
Kitchell, JF ;
Pace, ML .
LIMNOLOGY AND OCEANOGRAPHY, 2002, 47 (06) :1664-1675
[10]   Persistence of net heterotrophy in lakes during nutrient addition and food web manipulations [J].
Cole, JJ ;
Pace, ML ;
Carpenter, SR ;
Kitchell, JF .
LIMNOLOGY AND OCEANOGRAPHY, 2000, 45 (08) :1718-1730