TRANSGRESSIONS, CLIMATIC CHANGE AND DIVERSITY OF CALCAREOUS NANNOPLANKTON

[1] BRAMLETTE M. N., 1964, MICROPALEONTOLOGY, V10, P291, DOI 10.2307/1484577

[2] MASSIVE EXTINCTIONS IN BIOTA AT END OF MESOZOIC TIME - ANY PROPOSED EXPLANATION SHOULD ACCOUNT FOR PROFOUND EFFECT ON MARINE PLANKTONIC LIFE OF THAT TIME [J]. SCIENCE, 1965, 148 (3678) : 1696 - +

[3] BREGGREN WA, 1969, MICROPALEONTOLOGY, V15, P351

[4] Brinkmann Roland., 1960, GEOLOGIC EVOLUTION E

[5] RADIATION OF CENOZOIC PLANKTONIC FORAMINIFERA [J]. SYSTEMATIC ZOOLOGY, 1969, 18 (02): : 154 - &

[6] DEVEREUX I, 1967, NEW ZEAL J SCI, V10, P988

[7] SOME AUSTRALIAN OXYGEN ISOTOPE TEMPERATURES AND A THEORY FOR A 30-MILLION-YEAR WORLD-TEMPERATURE CYCLE [J]. JOURNAL OF GEOLOGY, 1968, 76 (03) : 297 - &

[8] Gignoux M, 1955, STRATIGRAPHIC GEOLOG

[9] Haq B.U., 1971, STOCKHOLM CONTRIBUTI, V25, P129

[10] Hay W. W, 1960, INT GEOL C REP SESS, V5, P70

[1] BRAMLETTE M. N., 1964, MICROPALEONTOLOGY, V10, P291, DOI 10.2307/1484577

[2] MASSIVE EXTINCTIONS IN BIOTA AT END OF MESOZOIC TIME - ANY PROPOSED EXPLANATION SHOULD ACCOUNT FOR PROFOUND EFFECT ON MARINE PLANKTONIC LIFE OF THAT TIME [J]. SCIENCE, 1965, 148 (3678) : 1696 - +

[3] BREGGREN WA, 1969, MICROPALEONTOLOGY, V15, P351

[4] Brinkmann Roland., 1960, GEOLOGIC EVOLUTION E

[5] RADIATION OF CENOZOIC PLANKTONIC FORAMINIFERA [J]. SYSTEMATIC ZOOLOGY, 1969, 18 (02): : 154 - &

[6] DEVEREUX I, 1967, NEW ZEAL J SCI, V10, P988

[7] SOME AUSTRALIAN OXYGEN ISOTOPE TEMPERATURES AND A THEORY FOR A 30-MILLION-YEAR WORLD-TEMPERATURE CYCLE [J]. JOURNAL OF GEOLOGY, 1968, 76 (03) : 297 - &

[8] Gignoux M, 1955, STRATIGRAPHIC GEOLOG

[9] Haq B.U., 1971, STOCKHOLM CONTRIBUTI, V25, P129

[10] Hay W. W, 1960, INT GEOL C REP SESS, V5, P70