Variation Among Biomes in Temporal Dynamics of Aboveground Primary Production
Abstract
Interannual variability in aboveground net primary production (ANPP) was assessed with long-term (mean = 12 years) data from 11 Long Term Ecological Research sites across North America. The greatest interannual variability in ANPP occurred in grasslands and old fields, with forests the least variable. At a continental scale, ANPP was strongly correlated with annual precipitation. However, interannual variability in ANPP was not related to variability in precipitation. Instead, maximum variability in ANPP occurred in biomes where high potential growth rates of herbaceous vegetation were combined with moderate variability in precipitation. In the most dynamic biomes, ANPP responded more strongly to wet than to dry years. Recognition of the fourfold range in ANPP dynamics across biomes and of the factors that constrain this variability is critical for detecting the biotic impacts of global change phenomena.
Get full access to this article
View all available purchase options and get full access to this article.
Already a Subscriber?Sign In
REFERENCES AND NOTES
1
Rosenzweig M. L., Am. Nat. 102, 67 (1968).
2
Lieth H., Human Ecol. 1, 303 (1973).
3
Sala O. E., et al., Science 287, 1770 (2000).
4
Schimel D., et al., Science 287, 2004 (2000).
5
Frank D. A., Inouye R. S., J. Biogeogr. 21, 401 (1994).
6
W. L. Webb, W. K. Lauenroth, S. R. Szarek, R. S. Kinerson. Ecology 64, 134 (1983).
7
H. N. Le Houerou, R. L. Bingham, W. Skerbek. J. Arid Environ. 15, 1 (1988).
8
Goward S. N., Prince S. D., J. Biogeogr. 22, 549 (1995).
9
Karl T. R., Knight R. W., Plummer N., Nature 377, 217 (1995).
10
We also assessed growing season precipitation and evapotranspiration (24). Over the range of productivity encompassed by these sites, annual precipitation was the strongest predictor of variation in ANPP (Fig. 2) {r2 = 0.36 for the relationship between AET and ANPP [as in (1)]}.
11
The LTER network began in 1980 (25). Each LTER site included in this analysis used unique methods for estimating ANPP (see individual site Web pages at ). When multiple communities were sampled, only a representative community type was selected from each site (Table 1). We attempted to include the longest and highest quality data available from each site. Although the length of record of ANPP varied (from 6 to 23 years), there was no relationship between the length of the data set and the means or CVs for ANPP or precipitation. We also constructed data sets of average length (12 years) by random sampling of the longest data sets (Konza Prairie, Cedar Creek, and Shortgrass Steppe). Means and variances calculated for these shorter term data did not differ significantly from those from the long-term data (26).
12
F. I. Woodward, Climate and Plant Distribution (Cambridge Univ. Press, Cambridge, 1987).
13
Easterling D. R., et al., Science 289, 2068 (2000).
14
Lauenroth W. K., Sala O. E., Ecol. Appl. 2, 397 (1992).
15
Paruelo J. M., Lauenroth W. K., Burke I. C., Sala O. E., Ecosystems 2, 64 (1999).
16
Seastedt T. R., Knapp A. K., Am. Nat. 141, 621 (1993).
17
Schimel D. S., Braswell B. H., Parton W. J., Proc. Natl. Acad. Sci. U.S.A. 94, 8280 (1997).
18
Schimel D. S., Participants VEMAP, Braswell B. H., Ecol. Monogr. 67, 251 (1997).
19
Melillo J. M., et al., Nature 363, 234 (1993).
20
T. G. F. Kittel et al., Proceedings of the 10th Conference on Applied Climatology (American Meteorological Society, Boston, MA, 1997).
21
Waide R. B., et al., Annu. Rev. Ecol. Syst. 30, 257 (1999).
22
Karl T. R., Heim R. R., Quayle R. G., Science 251, 1058 (1991).
23
H. E. Wright Jr. et al., Global Climates Since the Last Glacial Maximum (Univ. of Minnesota Press, Minneapolis, MN, 1993).
24
Thornthwaite C. W., Mather J. R., Publ. Climatol. 8, 1 (1955).
25
Callahan J. T., BioScience 34, 363 (1984).
26
A. K. Knapp, M. D. Smith, data not shown.
27
We thank the principal investigators, information managers, and scientists responsible for measuring ANPP at the LTER sites and J. Aber, W. Bowman, D. Schimel, G. Shaver, R. Ruess, T. Fahey, and W. Lauenroth for providing comments on earlier versions of the manuscript. Research was supported and data were provided by the NSF Long-Term Ecological Research Program, the VEMAP data group and sponsors (S. Aulenbach, NASA, the Electric Power Research Institute, and the U.S. Department of Agriculture's Forest Service), and Kansas State University. This paper is dedicated to the memory of Dr. James T. Callahan, whose foresight and support of the LTER program for over 20 years enabled these data to be collected.
Information & Authors
Information
Published In

Science
Volume 291 | Issue 5503
19 January 2001
19 January 2001
Submission history
Received: 10 July 2000
Accepted: 7 December 2000
Published in print: 19 January 2001
Authors
Metrics & Citations
Metrics
Article Usage
Altmetrics
Citations
Export citation
Select the format you want to export the citation of this publication.
Cited by
- Response to Comments on “Drought-Induced Reduction in Global Terrestrial Net Primary Production from 2000 Through 2009”, Science, 333, 6046, (1093-1093), (2021)./doi/10.1126/science.1199169
- Interannual Variability in Net Primary Production and Precipitation, Science, 293, 5536, (1723-1723), (2021)./doi/10.1126/science.293.5536.1723a
- Rainfall Variability, Carbon Cycling, and Plant Species Diversity in a Mesic Grassland, Science, 298, 5601, (2202-2205), (2002)./doi/10.1126/science.1076347
Loading...
View Options
Get Access
Log in to view the full text
AAAS login provides access to Science for AAAS Members, and access to other journals in the Science family to users who have purchased individual subscriptions.
- Become a AAAS Member
- Activate your AAAS ID
- Purchase Access to Other Journals in the Science Family
- Account Help
Log in via OpenAthens.
Log in via Shibboleth.
More options
Purchase digital access to this article
Download and print this article for your personal scholarly, research, and educational use.
Buy a single issue of Science for just $15 USD.
View options
PDF format
Download this article as a PDF file
Download PDF





