Soil temperatures near the distribution limit of the mountain birch (Betula pubescens ssp czerepanovii): Implications for seedling nitrogen economy and survival
Ps. Karlsson et M. Weih, Soil temperatures near the distribution limit of the mountain birch (Betula pubescens ssp czerepanovii): Implications for seedling nitrogen economy and survival, ARCT ANTARC, 33(1), 2001, pp. 88-92
This paper (1) describes soil temperature conditions in an area close to th
e altitudinal and latitudinal distribution Limit of the mountain birch, and
(2) evaluates whether soil temperature is likely to impose a limit on nitr
ogen uptake and subsequent reductions in growth and survival. Soil temperat
ure was monitored at two depths (-5 and -10 cm) during 3 yr in forested and
nearby nonforested sites both at low altitude (ca. 400 m) and at forest li
ne (ca. 650 m) in the Tornetrask area, northern Swedish Lapland (68 degrees
21'N, 18 degrees 49'E). The mean summer soil temperature was ca. +6 to +7
degreesC and +5 to +7 degreesC at -5 and -10 cm, respectively. Forest-line
soils were on average 0.8 degreesC warmer than valley soils. We found no st
atistically significant differences in soil temperature between sites colon
ized by mountain birch and nearby nonforested habitats. Given present soil
temperatures, there is thus no reason why (mature) trees should not survive
also on alpine and subalpine heaths currently not colonized by birch. Howe
ver, relating these temperature recordings to experimentally determined rel
ationships between soil temperature and seedling nitrogen (N) uptake, and b
etween N uptake and survival, indicates that the mountain birch seedlings a
re unlikely to survive their first winter under soil temperature conditions
normally prevailing in this area. Our analysis suggests that successful se
edling establishment can be expected on disturbed sites when the growing se
ason (15 June to 15 August) mean soil temperature is ca. 12 degreesC or hig
her. In comparison, growing season soil temperature under undisturbed veget
ation (at -5 cm) was on average ca 8.2 degreesC during our 3 yr of soil tem
perature measurements. Air temperature during the same period was 1.1 degre
esC warmer than the average for the last 86 yr (1913-1998, 11.0 versus 9.9
degreesC).