Human impact on the vegetation of South Wales during late historical times: palynological and palaeoenvironmental results from Crymlyn Bog NNR, West Glamorgan, Wales, UK
D. Rosen et L. Dumayne-peaty, Human impact on the vegetation of South Wales during late historical times: palynological and palaeoenvironmental results from Crymlyn Bog NNR, West Glamorgan, Wales, UK, HOLOCENE, 11(1), 2001, pp. 11-23
Palynological and palaeoenvironmental analyses of Crymlyn Bog, a lowland fe
n in South Wales, reveal insights into the effects of documented industrial
activity on the landscape during the last c. 500 years. The pollen and pal
aeoenvironmental profiles suggest that a predominantly wooded landscape in
which some agriculture but little industrial activity took place, occurred
between the sixteenth and early eighteenth centuries. Significant increases
in heavy metals, spheroidal carbonaceous particles and SIRM are coincident
with rapid and substantial industrialization of the Lower Swansea Valley f
rom the mid-eighteenth to early nineteenth centuries, although the pollen e
vidence suggests that the vegetation of the area was dominated by birch-haz
el woodland. The pollen profile suggests that large-scale woodland clearanc
e, that was perhaps caused by increased land-use pressure adjacent to the m
ire, occurred in the late nineteenth and early twentieth centuries. At the
same time, decreases in the profiles of copper, zinc and lead reflect the d
ecline of non-ferrous metal smelting in the Lower Swansea Valley. The spher
oidal carbonaceous particle and SIRM profiles from Crymlyn Bog do not corre
spond with the national trends depicted in such profiles from elsewhere in
the British Isles, probably because of the dominance of locally derived ind
ustrial pollution. The apparent integrity of the copper, lead and SIRM prof
iles suggest that fen peat is an eminently suitable, and thus much under-us
ed, medium from which to reconstruct palaeoenvironmental and industrial his
tories. Limitations in the use of the zinc, and the SCP and pollen profiles
as palaeoenvironmental indicators and dating tools respectively are demons
trated by the lack of correspondence between their profiles and documented
historical land-use records.