Fossil chironomid assemblages and inferred summer temperatures for the past 14,000 years from a low-elevation lake in Pacific Canada

Globorotalia menardii + Globigerinoides ruber

temperature (R3CvZBuTHNk): paleoData_notes: 'ANN (Malmgren & Nordlund (1997)' has been replaced by ''
temperature (R3CvZBuTHNk): paleoData_proxyDetail: 'assemblage' has been replaced by 'ANN (Malmgren & Nordlund (1997)'

Pivel, M.A.G.; Santarosa, A.C.A.; Toledo, F.A.L.; Costa, K.B.

The Holocene onset in the southwestern South Atlantic

Helama, Samuli; Timonen, Mauri; Holopainen, Jari; Ogurtsov, Maxim G.; Mielik _inen, Kari; Eronen, Matti; Lindholm, Markus; Meril _inen, Jouko

Summer temperature variations in Lapland during the Medieval Warm Period and the Little Ice Age relative to natural instability of thermohaline circulation on multi-decadal and multi-centennial scales

van Ommen, Tas Morgan, Vin Elcheikh, Alan Dahl-Jensen, Dorthe

temperature (LPD7abab671): paleoData_proxyDetail: 'borehole' has been replaced by ''

Dahl-Jensen, Dorthe; Morgan, Vin I.; Elcheikh, Alan

<jats:title>Abstract</jats:title>
            <jats:p>The temperature profile in the 1200 m deep Dome Summit South (DSS) borehole near the summit of Law Dome, Antarctica, was measured in 1996, 3 years after the termination of the deep drilling.</jats:p>
            <jats:p>The temperature profile contains information on past surface temperature over the last 4ka. This temperature history is determined by the use of a Monte Carlo inverse method in which no constraints are placed on the unknown temperature history and no solution is assumed to be unique. The temperature history is obtained from a selection of equally well-fitting solutions by a statistical treatment.</jats:p>
            <jats:p>The results show that solutions covering the last 4ka have a well-developed central value, a most likely temperature history. The temperature record has two well-developed minima at AD 1250 and 1850. From 1850 to the present, temperatures have gradually increased by 0.7 K. The reconstructed temperatures are compared with the stable oxygen isotope (<ce><b4><jats:sup>18</jats:sup>O) from the DSS ice core.</jats:p>