J. Svavarsson, DIVERSITY OF ISOPODS (CRUSTACEA) - NEW DATA FROM THE ARCTIC AND ATLANTIC OCEANS, Biodiversity and conservation, 6(11), 1997, pp. 1571-1579
New data on the diversity pattern of isopods (Crustacea) from the nort
hern most part of the North Atlantic and the Arctic Oceans is presente
d. The pattern of diversity with depth is similar at depths < 1000 m,
but differs considerably below about 1000 m. In the Arctic the diversi
ty of isopods (expressed both as numbers of species per sled and expec
ted number of species) increased with increased depth to a maximum at
depths of about 320 to 1100 m, but then declined towards deeper waters
. There was a significant increase in numbers per sled and in the expe
cted number of species with increased depth in the northernmost part o
f the North Atlantic Ocean. Additionally, changes occurred in the rela
tive composition of the shallow and deep water fauna, with asellote is
opods being relatively larger part of the isopod fauna in the Arctic t
han in the northern most part of the North Atlantic. This indicates ma
jor faunistic changes occurring at the Greenland-Iceland-Faeroe Ridge,
possibly caused by rapid changes in the temperature. Furthermore, tha
t the low diversity of the Arctic deep-sea is a regional phenomenon, a
nd not a part of a large scale latitudinal pattern in the North Atlant
ic.