McConnell, J.R., Maselli, O.J., Sigl, M., Vallelonga, P., Neumann, T., Anschutz, H., Bales, R.C., Curran, M.A.J., Das, S.B., Edwards, R., Kipfstuhl, S., Layman, L. and Thomas, E.R., 2014, Antarctic - wide array of high - resolution
ice core records reveals pervasive lead pollution began in 1889 and persists today.
Not exact matches
Australian scientists have welcomed the success of a five - year Greenland
ice core drilling project that is expected to
reveal a
record of more than 130 000 years and provide an insight into future global climate.
In Greenland lead isotopes in
ice cores reveal a
record of lead pollution from Roman smelting in Spain some 2,000 years ago.
Recent inspection of the sulfate
records from the European project for
ice coring in Antarctica's dronning maud land (EDML)
ice core reveals sulfate peaks that have been correlated to presumed YTT sulfate peaks in the North Greenland
ice core project (NGRIP) and GISP2
ice cores; however, once again no volcanic material has been identified (18).
Marine sediment
cores will
reveal records of past glacial - interglacial cycles while lake sediments and peat
cores will
reveal climate
records since the last
ice age.
An analysis of the GISP2
ice core record from Greenland
reveals that abrupt climate events appear to be paced by a 1,470 - year cycle with a period that is probably stable to within a few percent; with 95 % confidence the period is maintained to better than 12 % over at least 23 cycles.
The climate
record obtained from two long Greenland
ice cores reveals several brief climate oscillations during glacial time.
''... worked with two sediment
cores they extracted from the seabed of the eastern Norwegian Sea, developing a 1000 - year proxy temperature
record «based on measurements of δ18O in Neogloboquadrina pachyderma, a planktonic foraminifer that calcifies at relatively shallow depths within the Atlantic waters of the eastern Norwegian Sea during late summer,» which they compared with the temporal histories of various proxies of concomitant solar activity... This work
revealed, as the seven scientists describe it, that «the lowest isotope values (highest temperatures) of the last millennium are seen ~ 1100 - 1300 A.D., during the Medieval Climate Anomaly, and again after ~ 1950 A.D.» In between these two warm intervals, of course, were the colder temperatures of the Little
Ice Age, when oscillatory thermal minima occurred at the times of the Dalton, Maunder, Sporer and Wolf solar minima, such that the δ18O proxy
record of near - surface water temperature was found to be «robustly and near - synchronously correlated with various proxies of solar variability spanning the last millennium,» with decade - to century - scale temperature variability of 1 to 2 °C magnitude.»
In 2008, research on Antarctic Vostok and EPICA Dome C
ice cores revealed that methane clathrates were also present in deep Antarctic
ice cores and
record a history of atmospheric methane concentrations, dating to 800,000 years ago.
Historical
records from early settlements
reveal glacier boundaries, as does
ice core data taken by drilling down into the annual layers of
ice that make up glaciers.