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Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological ...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. <1 = present outside the regular counts, # = suspected reworking. -
Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological ...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. <1 = present outside the regular counts, # = suspected reworking. -
Record of 7 acritarch taxa from the Miocene, Pliocene and Pleistocene of ODP ...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. P = present; R = rare; C = common; A = abundant; F = frequent; ? = questionable assignment, - = not... -
Record of 7 acritarch taxa, and palynological preparation data from the Mioce...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. <1 = present outside the regular counts, # = suspected reworking. -
Record of 7 acritarch taxa, Mg/Ca sea-surface temperatures and palynological ...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. <1 = present outside the regular counts, # = suspected reworking. -
Record of 7 acritarch taxa, and palynological preparation data from the Mioce...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. <1 = present outside the regular counts, # = suspected reworking, P = present. -
Record of 7 acritarch taxa from the Miocene, Pliocene and Pleistocene of ODP ...
DEPTH, sediment [m] is given in mbsf. -
Record of 7 acritarch taxa from the Miocene, Pliocene and Pleistocene of ODP ...
DEPTH, sediment [m] is given in mbsf. AGE [ka BP] gives the calibrated ages. Species abundance: P = present; R = rare; C = common; A = abundant; F = frequent; ? = questionable... -
Late Miocene and Pliocene dinoflagellate cysts, acritarchs and terrestrial pa...
The globally warm climate of the early Pliocene gradually cooled from 4 million years ago, synchronous with decreasing atmospheric CO2 concentrations. In contrast,... -
Palynological analyses of the sediments around the Miocene/Pliocene boundary ...
The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak...