The Madeiran islands, located at 33 degrees N in the eastern Atlantic,
were colonized early in the 15th century, and perhaps up to a century
earlier. The woodland and scrub cover was rapidly reduced and the amo
unt of grassland and disturbed ground increased. The effect on the lan
d snail population has been assessed by analysis of fossil assemblages
from a deposit in eastern Madeira. Dates were obtained by measurement
of amino acid epimer ratios (D-alloisoleucine/L-isoleucine) of indivi
dual shells, calibrated against radiocarbon-dated samples. Because thi
s method allows dating of individual shells, it was possible to recons
truct the chronology of various species from mixed-age assemblages. It
also permits dating of shells too young for radiocarbon dating (post-
AD 1650). Fifteen land snail assemblages were analysed from deposits o
f post-settlement age (c. 420-50 yr sp). Of the thirty-four species of
land snails present in the samples, nine have become extinct over the
period. In contrast, only five species became extinct on the island d
uring the previous c. 300,000 years. The majority of the extinctions h
ave occurred within the last two centuries, as a result of habitat des
truction. A major decline in the abundance of woodland species took pl
ace during the 20th century. The extinction of the endemic Caseolus bo
wdichianus, abundant in middle Holocene deposits, occurred about a cen
tury after colonization of the island. Theba pisana, a snail of simila
r size and shape, was introduced around the time of colonization, and
is now abundant in grassy areas. Two endemic grassland species, Discul
a polymorpha and Heterostoma paupercula, have also become more abundan
t and thus apparently benefited from the arrival of man.