DEFINING THE BOUNDARIES OF THE LATE-GLACIAL ISOTOPE EPISODES

[1] LATE-GLACIAL RADIOCARBONSTRATIGRAPHY AND PALYNOSTRATIGRAPHY ON THE SWISS PLATEAU [J]. BOREAS, 1989, 18 (02) : 109 - 126

[2] SEASONAL TEMPERATURES IN BRITAIN DURING THE PAST 22,000 YEARS, RECONSTRUCTED USING BEETLE REMAINS [J]. NATURE, 1987, 325 (6105) : 587 - 592

[3] CALIBRATION OF THE C-14 TIMESCALE OVER THE PAST 30,000 YEARS USING MASS-SPECTROMETRIC U-TH AGES FROM BARBADOS CORALS [J]. NATURE, 1990, 345 (6274) : 405 - 410

[4] RETREAT VELOCITY OF THE NORTH-ATLANTIC POLAR FRONT DURING THE LAST DEGLACIATION DETERMINED BY C-14 ACCELERATOR MASS-SPECTROMETRY [J]. NATURE, 1987, 328 (6133) : 791 - 794

[5] A STABLE-ISOTOPE TREE-RING TIMESCALE OF THE LATE GLACIAL HOLOCENE BOUNDARY [J]. NATURE, 1991, 353 (6345) : 647 - 649

[6] BERGLUND BE, 1979, BOREAS, V8, P89

[7] Birks H.J.B., 1982, STRIAE, V16, P99

[8] Birks HJB, 1973, PRESENT VEGETATION I

[9] THE CHRONOLOGY OF THE LAST DEGLACIATION: IMPLICATIONS TO THE CAUSE OF THE YOUNGER DRYAS EVENT [J]. PALEOCEANOGRAPHY, 1988, 3 (01): : 1 - 19

[10] THE ROLE OF OCEAN-ATMOSPHERE REORGANIZATIONS IN GLACIAL CYCLES [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (10) : 2465 - 2501

[1] LATE-GLACIAL RADIOCARBONSTRATIGRAPHY AND PALYNOSTRATIGRAPHY ON THE SWISS PLATEAU [J]. BOREAS, 1989, 18 (02) : 109 - 126

[2] SEASONAL TEMPERATURES IN BRITAIN DURING THE PAST 22,000 YEARS, RECONSTRUCTED USING BEETLE REMAINS [J]. NATURE, 1987, 325 (6105) : 587 - 592

[3] CALIBRATION OF THE C-14 TIMESCALE OVER THE PAST 30,000 YEARS USING MASS-SPECTROMETRIC U-TH AGES FROM BARBADOS CORALS [J]. NATURE, 1990, 345 (6274) : 405 - 410

[4] RETREAT VELOCITY OF THE NORTH-ATLANTIC POLAR FRONT DURING THE LAST DEGLACIATION DETERMINED BY C-14 ACCELERATOR MASS-SPECTROMETRY [J]. NATURE, 1987, 328 (6133) : 791 - 794

[5] A STABLE-ISOTOPE TREE-RING TIMESCALE OF THE LATE GLACIAL HOLOCENE BOUNDARY [J]. NATURE, 1991, 353 (6345) : 647 - 649

[6] BERGLUND BE, 1979, BOREAS, V8, P89

[7] Birks H.J.B., 1982, STRIAE, V16, P99

[8] Birks HJB, 1973, PRESENT VEGETATION I

[9] THE CHRONOLOGY OF THE LAST DEGLACIATION: IMPLICATIONS TO THE CAUSE OF THE YOUNGER DRYAS EVENT [J]. PALEOCEANOGRAPHY, 1988, 3 (01): : 1 - 19

[10] THE ROLE OF OCEAN-ATMOSPHERE REORGANIZATIONS IN GLACIAL CYCLES [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (10) : 2465 - 2501