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Title: Carbon budget of the Harvard Forest Long-Term Ecological Research site: pattern, process, and response to global change

Abstract

How, where, and why carbon (C) moves into and out of an ecosystem through time are long-standing questions in biogeochemistry. Here, we bring together hundreds of thousands of C-cycle observations at the Harvard Forest in central Massachusetts, USA, a mid-latitude landscape dominated by 80–120-yr-old closed-canopy forests. These data answered four questions: (1) where and how much C is presently stored in dominant forest types; (2) what are current rates of C accrual and loss; (3) what biotic and abiotic factors contribute to variability in these rates; and (4) how has climate change affected the forest’s C cycle? Harvard Forest is an active C sink resulting from forest regrowth following land abandonment. Soil and tree biomass comprise nearly equal portions of existing C stocks. Net primary production (NPP) averaged 680–750 g C·m–2·yr–1; belowground NPP contributed 38–47% of the total, but with large uncertainty. Mineral soil C measured in the same inventory plots in 1992 and 2013 was too heterogeneous to detect change in soil-C pools; however, radiocarbon data suggest a small but persistent sink of 10–30 g C·m–2·yr–1. Net ecosystem production (NEP) in hardwood stands averaged ~300 g C·m–2·yr–1. NEP in hemlock-dominated forests averaged ~450 g C·m–2·yr–1 until infestation by themore » hemlock woolly adelgid turned these stands into a net C source. Since 2000, NPP has increased by 26%. For the period 1992–2015, NEP increased 93%. The increase in mean annual temperature and growing season length alone accounted for ~30% of the increase in productivity. Interannual variations in GPP and NEP were also correlated with increases in red oak biomass, forest leaf area, and canopy-scale light-use efficiency. Compared to long-term global change experiments at the Harvard Forest, the C sink in regrowing biomass equaled or exceeded C cycle modifications imposed by soil warming, N saturation, and hemlock removal. Furthermore, the results of this synthesis and comparison to simulation models suggest that forests across the region are likely to accrue C for decades to come but may be disrupted if the frequency or severity of biotic and abiotic disturbances increases.« less

Authors:
ORCiD logo [1];  [1]; ORCiD logo [2];  [3]; ORCiD logo [2]; ORCiD logo [4]; ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3];  [5]; ORCiD logo [6];  [7]; ORCiD logo [5]; ORCiD logo [8]; ORCiD logo [3]; ORCiD logo [2]; ORCiD logo [2];  [9];  [7];  [7] more »; ORCiD logo [2]; ORCiD logo [10]; ORCiD logo [5];  [3];  [2] « less
  1. Boston Univ., MA (United States)
  2. Harvard Univ., Petersham, MA (United States)
  3. Univ. of New Hampshire, Durham, NH (United States)
  4. Univ. of Maryland Center for Environmental Science, Frostburg, MD (United States)
  5. Harvard Univ., Cambridge, MA (United States)
  6. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Univ. of California, Berkeley, CA (United States)
  7. Marine Biological Laboratory, Woods Hole, MA (United States)
  8. Univ. of Michigan, Ann Arbor, MI (United States)
  9. Northern Arizona Univ., Flagstaff, AZ (United States)
  10. Clark Univ., Worcester, MA (United States)
Publication Date:
Research Org.:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
1840936
Grant/Contract Number:  
AC02-05CH11231
Resource Type:
Accepted Manuscript
Journal Name:
Ecological Monographs
Additional Journal Information:
Journal Volume: 90; Journal Issue: 4; Journal ID: ISSN 0012-9615
Publisher:
Wiley
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; forest ecosystems; ecosystem ecology; carbon cycling; net primary production; gross primary production; belowground production; disturbance; eddy covariance; permanent plots; climate change; long-term ecological research

Citation Formats

Finzi, Adrien C., Giasson, Marc‐André, Barker Plotkin, Audrey A., Aber, John D., Boose, Emery R., Davidson, Eric A., Dietze, Michael C., Ellison, Aaron M., Frey, Serita D., Goldman, Evan, Keenan, Trevor F., Melillo, Jerry M., Munger, J. William, Nadelhoffer, Knute J., Ollinger, Scott V., Orwig, David A., Pederson, Neil, Richardson, Andrew D., Savage, Kathleen, Tang, Jianwu, Thompson, Jonathan R., Williams, Christopher A., Wofsy, Steven C., Zhou, Zaixing, and Foster, David R. Carbon budget of the Harvard Forest Long-Term Ecological Research site: pattern, process, and response to global change. United States: N. p., 2020. Web. doi:10.1002/ecm.1423.
Finzi, Adrien C., Giasson, Marc‐André, Barker Plotkin, Audrey A., Aber, John D., Boose, Emery R., Davidson, Eric A., Dietze, Michael C., Ellison, Aaron M., Frey, Serita D., Goldman, Evan, Keenan, Trevor F., Melillo, Jerry M., Munger, J. William, Nadelhoffer, Knute J., Ollinger, Scott V., Orwig, David A., Pederson, Neil, Richardson, Andrew D., Savage, Kathleen, Tang, Jianwu, Thompson, Jonathan R., Williams, Christopher A., Wofsy, Steven C., Zhou, Zaixing, & Foster, David R. Carbon budget of the Harvard Forest Long-Term Ecological Research site: pattern, process, and response to global change. United States. https://doi.org/10.1002/ecm.1423
Finzi, Adrien C., Giasson, Marc‐André, Barker Plotkin, Audrey A., Aber, John D., Boose, Emery R., Davidson, Eric A., Dietze, Michael C., Ellison, Aaron M., Frey, Serita D., Goldman, Evan, Keenan, Trevor F., Melillo, Jerry M., Munger, J. William, Nadelhoffer, Knute J., Ollinger, Scott V., Orwig, David A., Pederson, Neil, Richardson, Andrew D., Savage, Kathleen, Tang, Jianwu, Thompson, Jonathan R., Williams, Christopher A., Wofsy, Steven C., Zhou, Zaixing, and Foster, David R. Tue . "Carbon budget of the Harvard Forest Long-Term Ecological Research site: pattern, process, and response to global change". United States. https://doi.org/10.1002/ecm.1423. https://www.osti.gov/servlets/purl/1840936.
@article{osti_1840936,
title = {Carbon budget of the Harvard Forest Long-Term Ecological Research site: pattern, process, and response to global change},
author = {Finzi, Adrien C. and Giasson, Marc‐André and Barker Plotkin, Audrey A. and Aber, John D. and Boose, Emery R. and Davidson, Eric A. and Dietze, Michael C. and Ellison, Aaron M. and Frey, Serita D. and Goldman, Evan and Keenan, Trevor F. and Melillo, Jerry M. and Munger, J. William and Nadelhoffer, Knute J. and Ollinger, Scott V. and Orwig, David A. and Pederson, Neil and Richardson, Andrew D. and Savage, Kathleen and Tang, Jianwu and Thompson, Jonathan R. and Williams, Christopher A. and Wofsy, Steven C. and Zhou, Zaixing and Foster, David R.},
abstractNote = {How, where, and why carbon (C) moves into and out of an ecosystem through time are long-standing questions in biogeochemistry. Here, we bring together hundreds of thousands of C-cycle observations at the Harvard Forest in central Massachusetts, USA, a mid-latitude landscape dominated by 80–120-yr-old closed-canopy forests. These data answered four questions: (1) where and how much C is presently stored in dominant forest types; (2) what are current rates of C accrual and loss; (3) what biotic and abiotic factors contribute to variability in these rates; and (4) how has climate change affected the forest’s C cycle? Harvard Forest is an active C sink resulting from forest regrowth following land abandonment. Soil and tree biomass comprise nearly equal portions of existing C stocks. Net primary production (NPP) averaged 680–750 g C·m–2·yr–1; belowground NPP contributed 38–47% of the total, but with large uncertainty. Mineral soil C measured in the same inventory plots in 1992 and 2013 was too heterogeneous to detect change in soil-C pools; however, radiocarbon data suggest a small but persistent sink of 10–30 g C·m–2·yr–1. Net ecosystem production (NEP) in hardwood stands averaged ~300 g C·m–2·yr–1. NEP in hemlock-dominated forests averaged ~450 g C·m–2·yr–1 until infestation by the hemlock woolly adelgid turned these stands into a net C source. Since 2000, NPP has increased by 26%. For the period 1992–2015, NEP increased 93%. The increase in mean annual temperature and growing season length alone accounted for ~30% of the increase in productivity. Interannual variations in GPP and NEP were also correlated with increases in red oak biomass, forest leaf area, and canopy-scale light-use efficiency. Compared to long-term global change experiments at the Harvard Forest, the C sink in regrowing biomass equaled or exceeded C cycle modifications imposed by soil warming, N saturation, and hemlock removal. Furthermore, the results of this synthesis and comparison to simulation models suggest that forests across the region are likely to accrue C for decades to come but may be disrupted if the frequency or severity of biotic and abiotic disturbances increases.},
doi = {10.1002/ecm.1423},
journal = {Ecological Monographs},
number = 4,
volume = 90,
place = {United States},
year = {Tue Aug 04 00:00:00 EDT 2020},
month = {Tue Aug 04 00:00:00 EDT 2020}
}

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Long-Term Impacts of Agriculture on soil Carbon and Nitrogen in new England Forests
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Forest Ecosystem Carbon and Nitrogen Accumulation During the First Century After Agricultural Abandonment
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Potential future dynamics of carbon fluxes and pools in New England forests and their climatic sensitivities: A model-based study
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Carbon, energy and water fluxes at mature and disturbed forest sites, Saskatchewan, Canada
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Carbon cycling and storage in world forests: biome patterns related to forest age
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Landscape and Regional Impacts of Hurricanes in new England
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Gap filling strategies for defensible annual sums of net ecosystem exchange
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Soil Warming and Carbon-Cycle Feedbacks to the Climate System
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Ecological Importance of Large-Diameter Trees in a Temperate Mixed-Conifer Forest
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Experimentally testing the role of foundation species in forests: the Harvard Forest Hemlock Removal Experiment: Foundation species experiments
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The potential to characterize ecological data with terrestrial laser scanning in Harvard Forest, MA
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Nitrogen Addition Increases Carbon Storage in Soils, But Not in Trees, in an Eastern U.S. Deciduous Forest
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Survivors, not invaders, control forest development following simulated hurricane
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Carbon Budget at the Harvard Forest 1992-2015
dataset, January 2019


Carbon Budget at the Harvard Forest 1992-2015
dataset, January 2019


Carbon Budget at the Harvard Forest 1992-2015
dataset, January 2019