New evidence of Holocene climate and atmospheric circulation variability, inferred
from lacustrine stable isotope records from Gotland, southern Sweden Francesco Muschitiello, Dan Hammarlund, Barbara Wohlfarth
Not exact matches
«I analyze
lacustrine sediments for charcoal, wood ash, micromorphology using thin sections, stable C and N isotopes, XRF, pollen and non-pollen palynomorphs to reconstruct fire history and vegetational and environmental changes
from LGM to the Holocene.»
A 2100 - yr decadal - resolution salinity and aridity proxy record of
lacustrine ostracode - shell Mg / Ca ratios
from a closed - basin lake in the northern Great Plains shows statistically significant periodicities of ∼ 400, 200, 130, and 100 yr.
Rapid
lacustrine response to recent High Arctic warming: a diatom record
from Sawtooth Lake, Ellesmere Island, Nunavut.
A similar negative trend is seen in most other Holocene paleoclimate records
from northern Sweden, e.g. changes in tree - limit (Karlén 1976; Kullman 1995); pollen (Barnekow 1999); chironomids (Larocque and Bigler 2004); oxygen - isotopes in
lacustrine biogenic silica (Shemesh et al. 2001) and in
lacustrine carbonates (Hammarlund et al. 2002).