TY - JOUR
T1 - Boom and bust carbon-nitrogen dynamics during reforestation
AU - Parolari, Anthony J.
AU - Mobley, Megan L.
AU - Bacon, Allan R.
AU - Katul, Gabriel G.
AU - Richter, Daniel de B.
AU - Porporato, Amilcare
N1 - Funding Information:
The authors acknowledge the following funding sources: the US Department of Energy (DOE) through the Office of Biological and Environmental Research (BER) Terrestrial Carbon Processes (TCP) program (DE-SC0006967); the National Science Foundation (NSF) to the Calhoun Critical Zone Observatory through the Geosciences Directorate's Division of Earth Sciences Critical Zone Observatory Program (EAR-1331846) and Ecosystem Grants Program (DEB-0717368); and the United States Department of Agriculture through the Agriculture and Food Research Initiative (2011-67003-30222). MLM also acknowledges support from an NSF Doctoral Dissertation Improvement Grant (DEB-1011186) and the Duke University E. Bayard Halstead and James B. Duke Fellowships. The authors thank Norm Christensen and Dan Binkley for insightful discussion and comments. The data for this paper are available by contacting the corresponding author (anthony.parolari@marquette.edu).
Publisher Copyright:
© 2017 Elsevier B.V.
PY - 2017/9/24
Y1 - 2017/9/24
N2 - Legacies of historical land use strongly shape contemporary ecosystem dynamics. In old-field secondary forests, tree growth embodies a legacy of soil changes affected by previous cultivation. Three patterns of biomass accumulation during reforestation have been hypothesized previously, including monotonic to steady state, non-monotonic with a single peak then decay to steady state, and multiple oscillations around the steady state. In this paper, the conditions leading to the emergence of these patterns is analyzed. Using observations and models, we demonstrate that divergent reforestation patterns can be explained by contrasting time-scales in ecosystem carbon-nitrogen cycles that are influenced by land use legacies. Model analyses characterize non-monotonic plant-soil trajectories as either single peaks or multiple oscillations during an initial transient phase controlled by soil carbon-nitrogen conditions at the time of planting. Oscillations in plant and soil pools appear in modeled systems with rapid tree growth and low initial soil nitrogen, which stimulate nitrogen competition between trees and decomposers and lead the forest into a state of acute nitrogen deficiency. High initial soil nitrogen dampens oscillations, but enhances the magnitude of the tree biomass peak. These model results are supported by data derived from the long-running Calhoun Long-Term Soil-Ecosystem Experiment from 1957 to 2007. Observed carbon and nitrogen pools reveal distinct tree growth and decay phases, coincident with soil nitrogen depletion and partial re-accumulation. Further, contemporary tree biomass loss decreases with the legacy soil C:N ratio. These results support the idea that non-monotonic reforestation trajectories may result from initial transients in the plant-soil system affected by initial conditions derived from soil changes associated with land-use history.
AB - Legacies of historical land use strongly shape contemporary ecosystem dynamics. In old-field secondary forests, tree growth embodies a legacy of soil changes affected by previous cultivation. Three patterns of biomass accumulation during reforestation have been hypothesized previously, including monotonic to steady state, non-monotonic with a single peak then decay to steady state, and multiple oscillations around the steady state. In this paper, the conditions leading to the emergence of these patterns is analyzed. Using observations and models, we demonstrate that divergent reforestation patterns can be explained by contrasting time-scales in ecosystem carbon-nitrogen cycles that are influenced by land use legacies. Model analyses characterize non-monotonic plant-soil trajectories as either single peaks or multiple oscillations during an initial transient phase controlled by soil carbon-nitrogen conditions at the time of planting. Oscillations in plant and soil pools appear in modeled systems with rapid tree growth and low initial soil nitrogen, which stimulate nitrogen competition between trees and decomposers and lead the forest into a state of acute nitrogen deficiency. High initial soil nitrogen dampens oscillations, but enhances the magnitude of the tree biomass peak. These model results are supported by data derived from the long-running Calhoun Long-Term Soil-Ecosystem Experiment from 1957 to 2007. Observed carbon and nitrogen pools reveal distinct tree growth and decay phases, coincident with soil nitrogen depletion and partial re-accumulation. Further, contemporary tree biomass loss decreases with the legacy soil C:N ratio. These results support the idea that non-monotonic reforestation trajectories may result from initial transients in the plant-soil system affected by initial conditions derived from soil changes associated with land-use history.
KW - Dynamical systems
KW - Land use legacy
KW - Nutrient cycling
KW - Plant-soil feedbacks
KW - Reforestation
KW - Soil nitrogen
UR - http://www.scopus.com/inward/record.url?scp=85024115830&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85024115830&partnerID=8YFLogxK
U2 - 10.1016/j.ecolmodel.2017.06.023
DO - 10.1016/j.ecolmodel.2017.06.023
M3 - Article
AN - SCOPUS:85024115830
SN - 0304-3800
VL - 360
SP - 108
EP - 119
JO - Ecological Modelling
JF - Ecological Modelling
ER -