Sentences with phrase «ka bp»

ka BP, indicating that the climate was then as least as warm as present.

ka BP and was followed by a period of lower temperatures 9 — 8.2 cal.

ka BP, when this species lived there.

Stalagmite DP1, a speleothem 1.6 m in length from Dante Cave in northeastern Namibia, provides a paleoclimate record of a gradual transition from wetter to drier conditions from 4.6 to 3.3 ka BP [before present], a variable but pronounced dry period from 3.3 to 1.8 ka, and a wetter but variable period from 1.8 ka to the present.

It has been established experimentally that, at ca 4.0 ka BP, there occurred a global change in the structure of atmospheric circulation, which coincided in time with the discharge of glacial masses from Greenland to North Atlantic and a solar activity minimum.

Maybe for > 10,000 years, but isn't it a bit misleading, since the Holocene temperature maximum was about 8 ka BP and sea levels reached their maximum ~ 7 ka BP.

Probably the most relative information to the discussion at hand is Vasskog et al.'s investigation of the GrIS during the last interglacial period (130 - 116 ka BP).

The WAIS Divide deep ice core WD2014 chronology - Part 1: Methane synchronization (68 - 31 ka BP) and the gas age - ice age difference.

Development and comparison of layer - counted chronologies from the WAIS Divide and EDML ice cores, Antarctica, over the last glacial transition (10 - 15 ka BP).

Here we present a chronology for the deep part of the core (67.8 - 31.2 ka BP), which is based on stratigraphic matching to annual - layer - counted Greenland ice cores using globally well - mixed atmospheric methane.

The upper 2850 m (back to 31.2 ka BP) have been dated using annual - layer counting.

The WAIS Divide deep ice core WD2014 chronology - Part 1: Methane synchronization (68 - 31 ka BP) and the gas age - ice age difference, Clim.

The WAIS Divide deep ice core WD2014 chronology — Part 1: Methane synchronization (68 - 31 ka BP) and the gas age — ice age difference Climate of the Past, 11, 153 - 173 \ nBuizert, C., and 15 others.

The WAIS Divide deep ice core WD2014 chronology — Part 1: Methane synchronization (68 - 31 ka BP) and the gas age — ice age difference Climate of the Past, 11, 153 - 173

The carbonates gave an isochron age of 9.59 ± 1.38 ka BP, i.e. belonging to the initial Holocene.

Not exact matches

De Ravin SS, Wu X, Moir S, Kardava L, O'Brien SA, Ulrick J, Kwatemaa N, Little P, Theobald N, Choi U, Su L, Marquesen M, Hilligoss D, Lee J, Buckner CM, Zarember KA, O'Connor G, McVicar D, Kuhns D, Throm RE, Zhou S, Notarangelo LD, Hanson IC, Cowan MJ, Kang E, Hadigan C, Meagher M, Gray JT, Sorrentino BP, Malech HL.

40 ka cal BP in any other region of Western Eurasia, including the Caucasus.»