Nj. Anderson et al., CLIMATE-LAKE INTERACTIONS RECORDED IN VARVED SEDIMENTS FROM A SWEDISHBOREAL FOREST LAKE, Global change biology, 2(4), 1996, pp. 399-405
A 1100-year long record of lake ecosystem response to climate and catc
hment change with precise chronological control is reported. Diatom an
d pollen assemblages of an annually laminated (varved) sediment from a
northern Swedish lake (Kassjon, Vasterbotten) were used as records of
lake diatom communities and catchment vegetation. These data were com
pared with summer temperature estimates based on tree-ring records of
the same geographical area to identify the effects of climate change a
nd catchment disturbance on diatom assemblages in the lake. In a canon
ical ordination, 23% of the variability in the total diatom assemblage
s for the period AD1040-1804 was accounted for by changes in pollen da
ta which reflect agricultural development in the catchment. Diatom spe
cies richness, however, exhibited a stronger relationship with summer
temperature and, significantly, declined with the lower temperatures a
ssociated with the Little Ice Age minimum (early 17th century). Summer
temperature accounted for 23% of the variability in diatom species ri
chness 20 years later. The mechanism behind this time-lag is unclear,
but may be related to catchment-mediated effects, given recent evidenc
e for lags in the response of boreal-forest vegetation regeneration cy
cles to climatic variability. These results suggest that climate-relat
ed effects on lakes occurring over medium timescales can be resolved i
n lake sediments. Moreover, it is possible to identify these effects d
espite cultural-related signals, but as the latter become more extreme
in the late 20th century the climate signal is obscured.