Calculated using the Group I calibration slope presented by D'Andrea et al. (2016). As we could not calibrate UK37 values to in-situ temperature observations for this study (no overlap with instrumental period) - we present the relative values generating by this algorithm. /// null

Variable name changed from age14C to ae during update from DKs csv files.

precipitation (M2L54vbu2i5P): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Fluvial origin, gently rolling terrain. Physiography: Lake Plateau. Surrounding vegetation: lichen woodland, black and white spruce.

Average normalized values for d13C, C:N, BSi, SAR, TOC, MS

chronology based on splice of varve counts (back to 3 ka) with PSV-age model (Larsen et al., 2012; 10.1016/j.quascirev.2012.02.006)

Geirsd _ttir, ́slaug; Miller, Gifford H.; Larsen, Darren J.;   lafsd _ttir, S _d _s

Abrupt Holocene climate transitions in the northern North Atlantic region recorded by synchronized lacustrine records in Iceland

Regional pollen stratigraphy, identifiable and well constrained
Regional pollen stratigraphy, identifiable and well constrained
Regional pollen stratigraphy, vague in character or regional occurance

Coutard, S., and M. Clet-Pellerin. 2006. Evolution de la sedimentation et de la vegetation pendant l'Holocene dans les marais arriere-littoraux du Val de Saire (Cotentin, Normandie). In : L'erosion entre Societe, Climat et Paleoenvironnements. Geolab-UMR 6042 CNRS, Presses Universitaires Blaise Pascal, Clermont-Ferrand, coll., Nature-Societe, 271-278.

L'erosion entre Societe, Climat et Paleoenvironnements

Evolution de la sedimentation et de la vegetation pendant l'Holocene dans les marais arriere-littoraux du Val de Saire (Cotentin, Normandie)

Basal date is younger than regional deglaciation.

precipitation (M2Li113vmomP): paleoData_proxyGeneral: '' has been replaced by 'pollen'

Postglacial vegetational history of the eastern Avalon Peninsula, Newfoundland, and Holocene climatic change along the eastern Canadian seaboard

Peat-filled kettle with small pond. Physiography: stagnation moraine on granitic upland. Surrounding vegetation: shrub-tundra with Picea-Abies krummholz.