Abstract

In the central and eastern United States, many forest ecosystems have undergone recent shifts in composition and structure that may conflict with contemporary management objectives. Long-term forest inventory data were used to determine patterns of forest succession over a 48-year period for four forest types in mid-Missouri: bottomlands, dry ridge and slope, glade-like, and mesic slopes. All forest types increased in stand basal area and overstory quadratic mean diameter through time, with concomitant decreases in the number of midstory trees. Sugar maple (Acer saccharum Marshall) increased in importance value on dry ridge and slope and mesic slope forest types, largely due to the accumulation of trees in smaller diameter classes. White oak (Quercus alba L.) increased in overstory basal area in dry ridge and slope plots through the duration of the study, whereas black oak (Quercus velutina Lam.) and Shumard oak (Quercus shumardii Buckley) decreased in overstory density and basal area through time. Oak stems were nearly absent from the midstory across forest types in the recent sampling, suggesting future challenges for maintaining oak-dominated canopies following attrition of canopy trees through time on upland forest types. In glade-like plots, eastern redcedar (Juniperus virginiana L.) increased in both overstory density and basal area through time, and Shumard oak decreased in density. The importance value of chinkapin oak (Quercus muehlenbergii Engelm.) in the overstory decreased through time in glade-like plots, largely due to the increase in density of eastern redcedar rather than the loss of chinkapin oak from the overstory. The patterns of succession in this forest landscape of mid-Missouri suggest that forest management may be needed to address two common contemporary concerns: (1) the need for increasing oak advance reproduction and recruitment to maintain oak as a canopy species; and (2) reducing eastern redcedar encroachment for glade restoration and management.

Highlights

  • Temporal change is a fundamental characteristic of forested ecosystems and has been widely studied in relation to natural processes, such as forest succession and natural disturbance (e.g., [1,2,3]), and anthropogenic influence, such as legacy effects of past land use or modern silvicultural manipulation (e.g., [4,5])

  • Basal area was greatest for bottomland and mesic slope forest types and lowest for the glade-like forest type (Table 1)

  • The pattern was similar for quadratic mean diameter, which increased through time across all forest types, with no interaction between forest type and year (F12,230 = 0.77; p = 0.684)

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Summary

Introduction

Temporal change is a fundamental characteristic of forested ecosystems and has been widely studied in relation to natural processes, such as forest succession and natural disturbance (e.g., [1,2,3]), and anthropogenic influence, such as legacy effects of past land use or modern silvicultural manipulation (e.g., [4,5]). Given the extent of anthropogenic influence, contemporary trajectories of forest change are complex and inexorably linked to both natural processes and human influence [6]. The challenges of managing forest resources to maintain ecological function and meet management needs have been exacerbated by the dynamic uncertainties of contemporary forest change [8]. The Central Hardwood Forest Region of the United States has been variously defined but generally includes most of the area within the states of Missouri, Illinois, Indiana, Ohio, Kentucky, Tennessee, Pennsylvania, and West Virginia, as well as portions of Iowa, Wisconsin, and Arkansas [9,10,11].

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