Sr. Vardy et al., HOLOCENE CLIMATE EFFECTS ON THE DEVELOPMENT OF A PEATLAND ON THE TUKTOYAKTUK PENINSULA, NORTHWEST-TERRITORIES, Quaternary research, 47(1), 1997, pp. 90-104
Six cores were collected from a small peatland on the Tuktoyaktuk Peni
nsula, yielding up to 1.8 m of organic material and 1.2 m of ice-rich
material. Stratigraphic relationships, radiocarbon dating, and pollen,
plant macrofossil, and isotopic analyses are used to reconstruct the
developmental history of the peatland. Organic matter began to accumul
ate in the basin about 7200 yr B.P., during a period when the climate
is thought to have been warmer than present. Initially the permafrost
table was probably below the bottom of the basin, and an open-water mi
neral wetland with emergent and submergent aquatic vegetation occupied
the site, Enriched delta(18)O values from ice samples confirm the exi
stence of an open water body with a water balance strongly affected by
evaporation. Transformation to a graminoid fen peatland was underway
by 6300 yr B.P. Permafrost and ice began to form in the peatland at th
is time. Low-centered polygons probably began to develop by 4700 yr B.
P. and subsequently evolved into the high-centered polygons which char
acterise the southwestern part of the peatland today, Feat accumulatio
n in the polygons has been extremely slow for the last 4000 years. The
eastern, wetter part of the basin has largely remained unchanged sinc
e its inception about 7000 yr B.P. Development of the peatland may be
linked to permafrost formation that was controlled by regional climate
changes during the Holocene. (C) 1997 University of Washington.