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Buffering of native forest edge microclimate by adjoining tree plantations
Author(s) -
DENYER K.,
BURNS B.,
OGDEN J.
Publication year - 2006
Publication title -
austral ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.688
H-Index - 87
eISSN - 1442-9993
pISSN - 1442-9985
DOI - 10.1111/j.1442-9993.2006.01609.x
Subject(s) - transect , microclimate , photosynthetically active radiation , pasture , environmental science , vapour pressure deficit , pinus radiata , atmospheric sciences , ecology , biology , botany , geology , photosynthesis , transpiration
In the Waikato Region of New Zealand, Pinus radiata (D. Don) plantations are becoming increasingly common on land adjacent to native forest fragments. It is unclear whether this juxtaposition is beneficial or detrimental to native forest fragment quality and persistence. We hypothesized that adjacent dense plantations buffer native fragments from microclimatic exposure, reducing edge effects and expanding the area of interior‐like native forest. Microclimate parameters were measured in native forest fragments adjacent to grazed pasture (‘abrupt’ edges) and in fragments adjacent to mature P. radiata plantations (‘embedded’ edges) during late summer. Photosynthetically active radiation, air temperature and vapour pressure deficit (VPD) were measured along transects perpendicular to edges during the mid‐afternoon, when gradients were typically steady and maximal, to investigate spatial variation. At paired abrupt versus embedded edges these same variables were monitored for week‐long periods to determine temporal variation. In fragments adjacent to pasture, conditions were significantly lighter and warmer (but not drier) than the interior along transects at distances up to 20 m from the edge. In contrast, no variables differed significantly along transects adjacent to pine. The different microclimate variables measured at edges (except VPD) contributed to edge effects at different times through a daily cycle. Photosynthetically active radiation was significantly different between abrupt and embedded edges at all times of the day. Air temperature was significantly different during mid‐day and afternoon, but not during the morning nor at night. Vapour pressure deficit varied considerably over time and between sites, but was never consistently higher at one type of edge. We conclude that pine plantations in the Waikato Region provide valuable microclimate buffering during the day, principally due to their effect in reducing light and temperature to interior‐like conditions at native forest edges. Consequently, plantations are a compatible neighbouring land use to forest fragments. Such buffering could be extended through the pine harvesting‐replanting phase with appropriate management, such as leaving an undisturbed margin during harvest.