911:
2595:
2584:
1162:(PETM), known as the Latest Danian Event (LDE). The event, which took place over a 170-230 kyr time interval, is evidenced in the geologic record by two negative carbon isotope excursions and is believed to have led to a 2–3 °C (3.6–5.4 °F) warming of both deep and surface seawater. This hyperthermal also led to a shallowing of the oceanic
1273:
Schmitz, B.; Pujalte, V.; Molina, E.; Monechi, S.; Orue-Etxebarria, X.; Speijer, R. P.; Alegret, L.; Apellaniz, E.; Arenillas, I.; Aubry, M.-P.; Baceta, J.-I.; Berggren, W. A.; Bernaola, G.; Caballero, F.; Clemmensen, A.; Dinarès-Turell, J.; Dupuis, C.; Heilmann-Clausen, C.; Orús, A. H.; Knox, R.;
989:) for this important boundary. The Danian is the oldest age of the Paleocene, defined at its base by the K-Pg boundary. It is very important because the readily recognized iridium anomaly and primitive Danian planktonic foraminifers define the base of the Danian. Danian
1240:
Molina, Eustoquio; Alegret, Laia; Arenillas, Ignacio; José A. Arz; Gallala, Njoud; Hardenbol, Jan; Katharina von Salis; Steurbaut, Etienne; Vandenberghe, Noel; Dalila
Zaghibib-Turki (2006).
1762:
in Ryder, G., Fastovsky, D., and
Gartner, S., eds., The Cretaceous-Tertiary Event and other catastrophes in Earth history: Geological Society of America Special Paper 307, pp. 263–277.
1242:"The Global Boundary Stratotype Section and Point for the base of the Danian Stage (Paleocene, Paleogene, "Tertiary", Cenozoic) at El Kef, Tunisia - Original definition and revision"
1734:
The Global
Boundary Stratotype Section and Point for the base of the Danian Stage (Paleocene, Paleogene, "Tertiary", Cenozoic) at El Kef, Tunisia: original definition and revision
1276:"The global Stratotype Sections and Points for the bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene Paleocene) stages at Zumaia, Spain"
1964:
993:
repopulated the
Paleocene seas after the Cretaceous mass extinction (Olsson et al., 1996). The first replacement foraminiferan of the Paleogene is the
1726:
Molina, E.; Alegret, L.; Arenillas, I.; Arz, J.A.; Gallala, N.; Hardenbol, J.; Salis, K. von; Steurbaut, E.; Vandenberghe, N. & Zaghbib-Turki, D.
1502:
1494:
1338:"Disused Paleogene regional stages from Belgium: Montian, Heersian, Landenian, Paniselian, Bruxellian, Laekenian, Ledian, Wemmelian and Tongrian"
1425:
Sprong, M.; Youssef, J. A.; Bornemann, André; Schulte, P.; Steurbaut, E.; Stassen, P.; Kouwenhoven, T. J.; Speijer, Robert P. (September 2011).
1320:
1158:
Close to the end of the Danian, around 62.2 Ma, occurred a hyperthermal, similar to but smaller in magnitude compared to the more famous
1789:
1832:
1957:
1804:
882:
576:
661:
594:
1183:
Zachos, J. C.; Kump, L. R. (2005). "Carbon cycle feedbacks and the initiation of
Antarctic glaciation in the earliest Oligocene".
1619:
997:
which is used to define the base of the Danian Age (Stainforth et al., 1975). This foraminiferan replaced the
Cretaceous genus
1613:
Bornemann, André; Jehle, Sofie; Lägel, Friederike; Deprez, Arne; Petrizzo, Maria Rose; Speijer, Robert P. (22 February 2021).
790:
1950:
536:
1495:"Paleoceanographic changes across the Latest Danian Event in the South Atlantic Ocean and planktic foraminiferal response"
1426:
910:
1274:
MartĂn-Rubio, M.; Ortiz, S.; Payros, A.; Petrizzo, M. R.; von Salis, K.; Sprong, J.; Steurbaut, E.; Thomsen, E. (2011).
1554:"The Impact of the Latest Danian Event on Planktic Foraminiferal Faunas at ODP Site 1210 (Shatsky Rise, Pacific Ocean)"
1086:
were gone, the mammals and other land animals remained small, most not even bigger than a sheep; however; a few (like
2628:
1373:
974:
2623:
1159:
1398:
1615:"Planktic foraminiferal response to an early Paleocene transient warming event and biostratigraphic implications"
1063:
17:
1324:
1825:
28:
934:
in 1847 following a study of fossils found in France and
Denmark. He identified this stage in deposits from
800:
738:
1798:
931:
1973:
650:
1493:
Jehle, Sofie; Bornemann, André; Lägel, Anna
Friederike; Deprez, Arne; Speijer, Robert P. (1 July 2019).
1719:
1818:
717:
2633:
2246:
2241:
1337:
1336:
De Geyter G.; De Man E.; Herman J.; Jacobs P.; Moorkens T.; Steurbat E.; Vandenberghe N. (2006).
1745:
1698:
1614:
1218:
1088:
1071:
1067:
1786:
866:
858:
622:
1306:
1628:
1567:
1511:
1441:
1192:
850:
695:
1292:
1275:
1258:
1241:
8:
2577:
1135:
1004:
The top of the Danian Stage (the base of the
Selandian) is close to the boundary between
1632:
1571:
1515:
1445:
1427:"A multi-proxy record of the Latest Danian Event at Gebel Qreiya, Eastern Desert, Egypt"
1196:
1654:
1590:
1553:
1527:
1457:
497:
2375:
2339:
1741:
1694:
1658:
1595:
1552:
Jehle, Sofie; Bornemann, André; Deprez, Arne; Speijer, Robert P. (25 November 2015).
1531:
618:
1461:
1204:
2469:
2344:
2313:
2110:
1644:
1636:
1585:
1575:
1519:
1449:
1287:
1253:
1200:
1012:. It is slightly after the first appearances of many new species of the calcareous
1807:, at the website of Norges Network of offshore records of geology and stratigraphy
2618:
2569:
2565:
2561:
2438:
2334:
2272:
2167:
2136:
2105:
1793:
1580:
1523:
1150:) still being around at this time, although they did not survive the Danian age.
1112:
1009:
970:
313:
48:
2594:
962:) is now known to be roughly equivalent to the Upper Danian and is considered a
2588:
2407:
2277:
2172:
2141:
1640:
1465:
990:
963:
1942:
1801:, at the website of the subcommission for stratigraphic information of the ICS
1766:
Stainforth, R.M., Lamb, J.L., Lutherbacher H., Beard, J.H., and
Jeffords, R.M.
1166:, as evidenced by the significant decrease in calcium carbonate preservation.
2612:
2308:
2298:
2267:
2230:
2162:
2131:
1693:, Bulletin de la Société Géologique de France, série 2, 3, pp. 179–181,
959:
878:
846:
815:
802:
753:
740:
685:
406:
79:
1774:
Cenozoic planktonic foraminifera zonation and characteristics of index forms
1453:
939:
2599:
2530:
2380:
2303:
1599:
1147:
1124:
1045:
1013:
2525:
2394:
2370:
2215:
2010:
1143:
1060:
927:
54:
1776:: The University of Kansas Paleontological Institute, Article 62, 425 p.
2520:
2480:
2423:
2323:
2220:
2094:
1994:
1910:
1649:
1335:
1272:
1103:
1094:
716:
enriched layer associated with a major meteorite impact and subsequent
471:
269:
99:
64:
2583:
893:
2535:
2485:
2459:
2418:
2365:
2210:
2186:
2067:
2057:
2046:
1905:
1884:
1879:
1864:
1854:
1841:
1163:
1139:
1128:
1108:
1098:
915:
899:
862:
854:
556:
462:
435:
425:
371:
325:
279:
104:
886:
2495:
2490:
2454:
2354:
2287:
2256:
2151:
2120:
2081:
2031:
2005:
1981:
1926:
1921:
1900:
1895:
1810:
1760:
The Cretaceous-Tertiary catastrophe event at Millers Ferry, Alabama
1558:
1083:
870:
615:
489:
480:
453:
444:
245:
232:
94:
89:
74:
69:
59:
2509:
2449:
2199:
2036:
2020:
1415:
Squid Empire: The Rise and Fall of the Cephalopods by Danna Staaf
1239:
1116:
1056:
1005:
982:
977:(K–T boundary) in stratigraphic sections worldwide. A section in
955:
951:
947:
923:
874:
732:
713:
395:
305:
109:
84:
2545:
2428:
2062:
1859:
1120:
978:
728:
352:
1093:
reached the size of a medium-sized bear. Numerous lineages of
1424:
943:
794:
877:. The beginning of the Danian (and the end of the preceding
1551:
986:
935:
1115:
seas, only that there was less life, few remaining marine
1612:
1492:
1358:
The GSSP for the Danian Stage was established by Molina
1182:
922:
The Danian was introduced in scientific literature by
1066:
and the Shanghuan and lowest part of the Nongshanian
1488:
1486:
1329:
132:
1044:) and close to the first appearance of calcareous
1503:Palaeogeography, Palaeoclimatology, Palaeoecology
1483:
1378:Fossilworks: Gateway to the Paleobiology Database
1111:region. The oceans remained much the same as the
2610:
1316:
1314:
781:Onset of sea-level drop and carbon isotope shift
1972:
1691:Sur le terrain Danien, nouvel Ă©tage de la craie
1097:also survived, particularly in the area around
918:landscape might have looked like in the Danian.
593:Subdivision of the Paleogene according to the
1958:
1826:
1311:
1307:International Commission on Stratigraphy 2017
1235:
1233:
1231:
1708:Gradstein, F.M.; Ogg, J.G. & Smith, A.G.
905:
1805:Stratigraphic chart of the Paleogene (2006)
1224:. International Commission on Stratigraphy.
1965:
1951:
1833:
1819:
1399:"†family Scaphitidae Gill 1871 (ammonite)"
1228:
600:Vertical axis scale: millions of years ago
1752:Olsson, R.K., Liu, C., and Van Fossen, M.
1648:
1589:
1579:
1291:
1257:
1219:"International Chronostratigraphic Chart"
969:The base of the Danian is defined at the
1176:
909:
1620:International Journal of Earth Sciences
14:
2611:
1153:
985:was appointed as a reference profile (
958:stratigraphy (named after the city of
590:
1946:
1814:
883:Cretaceous–Paleogene extinction event
1840:
565:
544:
526:
2564:= kiloannum (thousands years ago);
1131:), and other lesser-known animals.
1074:, all included in the 1 - 5 group.
24:
2568:= megaannum (millions years ago);
25:
2645:
2572:= gigaannum (billions years ago).
1780:
1371:
1365:
1160:Palaeocene-Eocene Thermal Maximum
2593:
2582:
52:
34:First age of the Paleocene Epoch
1606:
1545:
1418:
1409:
1391:
1293:10.18814/epiiugs/2011/v34i4/002
1259:10.18814/epiiugs/2006/v29i4/004
1205:10.1016/j.gloplacha.2005.01.001
1077:
1064:North American land mammal ages
1352:
1300:
1266:
1211:
1055:The Danian Stage overlaps the
525:
27:For the villages in Iran, see
13:
1:
2011:Pleistocene (11.7 ka–2.58 Ma)
1676:
1434:Journal of Micropalaeontology
1169:
975:Cretaceous–Paleogene boundary
1581:10.1371/journal.pone.0141644
1524:10.1016/j.palaeo.2019.03.024
1325:Den Store Danske Encyklopædi
914:Artist impression of what a
7:
1974:Geological history of Earth
1185:Global and Planetary Change
591:
227:
10:
2650:
2247:Mississippian (323–359 Ma)
2242:Pennsylvanian (299–323 Ma)
2006:Holocene (present–11.7 ka)
1799:Paleogene timescale (2008)
1720:Cambridge University Press
1716:A Geologic Time Scale 2004
1641:10.1007/s00531-020-01972-z
26:
2559:
2544:
2531:Paleoarchean (3.2–3.6 Ga)
2508:
2468:
2437:
2406:
2393:
2381:Terreneuvian (521–539 Ma)
2353:
2322:
2286:
2255:
2229:
2198:
2185:
2150:
2119:
2093:
2080:
2045:
2019:
1993:
1980:
1848:
1787:GeoWhen Database – Danian
1101:but also elsewhere, e.g.
1070:. It includes the oldest
1050:Neochiastozygus perfectus
966:and is no longer in use.
932:Pierre Jean Édouard Desor
906:Stratigraphic definitions
831:
785:
778:Upper boundary definition
777:
769:
723:
710:Lower boundary definition
709:
701:
691:
681:
676:
668:
656:
646:
641:
633:
628:
611:
130:
125:
44:
39:
2629:Danian first appearances
2526:Mesoarchean (2.8–3.2 Ga)
2371:Miaolingian (497–509 Ma)
2216:Guadalupian (260–272 Ma)
2068:Paleocene (56.0–66.0 Ma)
2058:Oligocene (23.0–33.9 Ma)
1374:"Mammal Paleogene zones"
1008:NP4 and NP5 from marine
973:which characterized the
898:, being followed by the
135:
2624:Paleocene geochronology
2521:Neoarchean (2.5–2.8 Ga)
2486:Orosirian (1.8–2.05 Ga)
2481:Statherian (1.6–1.8 Ga)
2424:Cryogenian (635–720 Ma)
2314:Llandovery (433–444 Ma)
2221:Cisuralian (272–299 Ma)
2032:Pliocene (2.59–5.33 Ma)
1454:10.1144/0262-821X10-023
942:and named it after the
2491:Rhyacian (2.05–2.3 Ga)
2460:Calymmian (1.4–1.6 Ga)
2419:Ediacaran (539–635 Ma)
2366:Furongian (485–497 Ma)
2211:Lopingian (252–260 Ma)
2037:Miocene (5.33–23.0 Ma)
1089:Ankalagon saurognathus
1072:Mammal Paleogene zones
1068:Asian land mammal ages
919:
218:−25 —
208:−30 —
198:−35 —
188:−40 —
178:−45 —
168:−50 —
158:−55 —
148:−60 —
138:−65 —
2496:Siderian (2.3–2.5 Ga)
2455:Ectasian (1.2–1.4 Ga)
2376:Series 2 (509–521 Ma)
2063:Eocene (33.9–56.0 Ma)
1136:controversial reports
1082:Though the non-avian
995:Globigerina eugubina,
913:
718:K–Pg extinction event
2536:Eoarchean (3.6–4 Ga)
2429:Tonian (720 Ma–1 Ga)
2309:Wenlock (427–433 Ma)
2299:Pridoli (419–423 Ma)
1740:, pp. 263–273,
557:permanent ice-sheets
2591: •
2580: •
2578:Geologic time scale
2340:Middle (458–470 Ma)
2304:Ludlow (423–427 Ma)
2273:Middle (383–393 Ma)
2168:Middle (237–247 Ma)
2137:Middle (164–174 Ma)
1633:2021IJEaS.110..583B
1572:2015PLoSO..1041644J
1516:2019PPP...525....1J
1446:2011JMicP..30..167S
1197:2005GPC....47...51Z
1154:Latest Danian Event
832:Upper GSSP ratified
812: /
786:Upper boundary GSSP
770:Lower GSSP ratified
750: /
724:Lower boundary GSSP
702:Time span formality
2589:Geology portal
2450:Stenian (1–1.2 Ga)
2345:Early (470–485 Ma)
2278:Early (393–419 Ma)
2173:Early (247–252 Ma)
2142:Early (174–201 Ma)
2111:Early (100–145 Ma)
2106:Late (66.0–100 Ma)
1792:2010-08-24 at the
920:
816:43.2992°N 2.2610°W
754:36.1537°N 8.6486°E
692:Stratigraphic unit
682:Chronological unit
669:Time scale(s) used
2606:
2605:
2504:
2503:
2470:Paleoproterozoic
2389:
2388:
2335:Late (444–458 Ma)
2268:Late (359–383 Ma)
2181:
2180:
2163:Late (201–237 Ma)
2132:Late (145–164 Ma)
2076:
2075:
1997:(present–2.58 Ma)
1985:(present–66.0 Ma)
1940:
1939:
1935:
1934:
1342:Geologica Belgica
839:
838:
642:Usage information
606:
605:
586:
585:
564:
563:
543:
542:
16:(Redirected from
2641:
2600:World portal
2598:
2597:
2587:
2586:
2549:
2513:
2473:
2442:
2439:Mesoproterozoic
2411:
2404:
2403:
2399:
2358:
2327:
2291:
2260:
2234:
2203:
2196:
2195:
2191:
2155:
2124:
2098:
2091:
2090:
2086:
2050:
2024:
1998:
1991:
1990:
1986:
1967:
1960:
1953:
1944:
1943:
1851:
1850:
1842:Paleogene Period
1835:
1828:
1821:
1812:
1811:
1767:
1753:
1727:
1709:
1704:
1684:
1670:
1669:
1667:
1665:
1652:
1610:
1604:
1603:
1593:
1583:
1566:(11): e0141644.
1549:
1543:
1542:
1540:
1538:
1499:
1490:
1481:
1480:
1478:
1476:
1470:
1464:. Archived from
1431:
1422:
1416:
1413:
1407:
1406:
1395:
1389:
1388:
1386:
1384:
1369:
1363:
1356:
1350:
1349:
1333:
1327:
1318:
1309:
1304:
1298:
1297:
1295:
1270:
1264:
1263:
1261:
1237:
1226:
1225:
1223:
1215:
1209:
1208:
1180:
1038:F. tympaniformis
897:
891:. The age ended
890:
827:
826:
824:
823:
822:
821:43.2992; -2.2610
817:
813:
810:
809:
808:
805:
789:Zumaia Section,
765:
764:
762:
761:
760:
755:
751:
748:
747:
746:
743:
727:El Kef Section,
612:Formerly part of
581:
571:
566:
559:
555:First Antarctic
550:
545:
532:
527:
500:
492:
483:
474:
465:
456:
447:
438:
429:
419:
409:
400:
390:
365:
346:
318:
299:
263:
238:
224:
219:
214:
209:
204:
199:
194:
189:
184:
179:
174:
169:
164:
159:
154:
149:
144:
139:
133:
121:
51:
37:
36:
21:
2649:
2648:
2644:
2643:
2642:
2640:
2639:
2638:
2634:Geological ages
2609:
2608:
2607:
2602:
2592:
2581:
2573:
2555:
2547:
2540:
2511:
2500:
2471:
2464:
2440:
2433:
2409:
2408:Neoproterozoic
2398:(539 Ma–2.5 Ga)
2397:
2396:
2395:Proterozoic Eon
2385:
2356:
2349:
2325:
2318:
2289:
2282:
2258:
2251:
2232:
2225:
2201:
2189:
2188:
2177:
2153:
2146:
2122:
2115:
2096:
2084:
2083:
2072:
2048:
2041:
2022:
2015:
1996:
1984:
1983:
1976:
1971:
1941:
1936:
1931:
1915:
1889:
1865:Oligocene Epoch
1855:Paleocene Epoch
1844:
1839:
1794:Wayback Machine
1783:
1765:
1751:
1725:
1707:
1702:
1682:
1679:
1674:
1673:
1663:
1661:
1611:
1607:
1550:
1546:
1536:
1534:
1497:
1491:
1484:
1474:
1472:
1471:on 28 June 2023
1468:
1429:
1423:
1419:
1414:
1410:
1397:
1396:
1392:
1382:
1380:
1370:
1366:
1357:
1353:
1348:(1–2): 203–213.
1334:
1330:
1319:
1312:
1305:
1301:
1271:
1267:
1238:
1229:
1221:
1217:
1216:
1212:
1181:
1177:
1172:
1156:
1142:(mainly of the
1113:Late Cretaceous
1080:
1010:biostratigraphy
971:iridium anomaly
908:
892:
885:
820:
818:
814:
811:
806:
803:
801:
799:
798:
797:
759:36.1537; 8.6486
758:
756:
752:
749:
744:
741:
739:
737:
736:
735:
607:
602:
601:
599:
582:
578:
575:
569:
560:
554:
548:
539:
530:
523:
522:
518:
517:
513:
512:
508:
507:
503:
502:
498:
494:
493:
488:
485:
484:
479:
476:
475:
470:
467:
466:
461:
458:
457:
452:
449:
448:
443:
440:
439:
434:
431:
430:
428:
424:
421:
420:
415:
412:
411:
407:
403:
402:
398:
396:
392:
391:
387:
385:
383:
381:
379:
377:
375:
373:
370:
367:
366:
362:
360:
358:
356:
354:
351:
348:
347:
345:
344:
341:
339:
337:
335:
333:
331:
329:
327:
324:
321:
320:
316:
314:
310:
309:
301:
300:
295:
293:
291:
289:
287:
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2250:
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2231:Carboniferous
2227:
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2207:
2205:
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2179:
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2100:
2088:
2078:
2077:
2074:
2073:
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2070:
2065:
2060:
2054:
2052:
2049:(23.0–66.0 Ma)
2043:
2042:
2040:
2039:
2034:
2028:
2026:
2023:(2.58–23.0 Ma)
2017:
2016:
2014:
2013:
2008:
2002:
2000:
1988:
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1955:
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1781:External links
1779:
1778:
1777:
1763:
1749:
1723:
1705:
1678:
1675:
1672:
1671:
1627:(2): 583–594.
1605:
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1440:(2): 167–182.
1417:
1408:
1390:
1364:
1351:
1328:
1310:
1299:
1286:(4): 220–243.
1265:
1252:(4): 263–278.
1227:
1210:
1174:
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1155:
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991:foraminiferans
964:junior synonym
907:
904:
845:is the oldest
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47:66.0 – 61.6
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2209:
2208:
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2197:
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2187:Paleozoic Era
2184:
2174:
2171:
2169:
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2161:
2160:
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2149:
2143:
2140:
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2129:
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2109:
2107:
2104:
2103:
2101:
2099:
2097:(66.0–145 Ma)
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2085:(66.0–252 Ma)
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2061:
2059:
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1372:Alroy, John.
1368:
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1031:
1027:
1023:
1019:
1018:Fasciculithus
1015:
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1007:
1002:
1000:
999:Globotruncana
996:
992:
988:
984:
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967:
965:
961:
957:
953:
949:
945:
941:
937:
933:
929:
925:
917:
912:
903:
901:
895:
888:
884:
880:
879:Maastrichtian
876:
872:
869:, and of the
868:
864:
860:
856:
852:
848:
844:
834:
830:
825:
796:
792:
788:
784:
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763:
734:
730:
726:
722:
719:
715:
712:
708:
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690:
687:
684:
680:
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659:
655:
652:
649:
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640:
636:
632:
627:
624:
620:
617:
614:
610:
598:
597:, as of 2021.
596:
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573:
568:
567:
558:
552:
547:
546:
538:
534:
529:
528:
501:
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71:
66:
61:
56:
50:
43:
38:
30:
19:
2574:
2510:Archean Eon
2472:(1.6–2.5 Ga)
2357:(485–539 Ma)
2326:(444–485 Ma)
2290:(419–444 Ma)
2259:(359–419 Ma)
2233:(299–359 Ma)
2202:(252–299 Ma)
2190:(252–539 Ma)
2154:(201–252 Ma)
2123:(145–201 Ma)
2082:Mesozoic Era
1982:Cenozoic Era
1874:
1860:Eocene Epoch
1773:
1769:
1759:
1755:
1737:
1733:
1729:
1715:
1711:
1690:
1686:
1662:. Retrieved
1624:
1618:
1608:
1563:
1557:
1547:
1535:. Retrieved
1507:
1501:
1473:. Retrieved
1466:the original
1437:
1433:
1420:
1411:
1402:
1393:
1381:. Retrieved
1377:
1367:
1359:
1354:
1345:
1341:
1331:
1302:
1283:
1279:
1268:
1249:
1245:
1213:
1191:(1): 51–66.
1188:
1184:
1178:
1157:
1148:Turkmenistan
1133:
1125:choristodera
1102:
1095:modern birds
1087:
1081:
1078:Paleontology
1054:
1049:
1046:nanoplankton
1041:
1037:
1034:F. involutus
1033:
1029:
1025:
1021:
1017:
1014:nanoplankton
1003:
998:
994:
968:
921:
881:) is at the
842:
840:
592:
416:
304:
278:
268:
244:
231:
29:Danian, Iran
2546:Hadean Eon
2324:Ordovician
2095:Cretaceous
1995:Quaternary
1736:, Episodes
1703:(in French)
1664:26 November
1650:2434/817466
1475:26 November
1383:17 December
1144:Scaphitidae
1061:Torrejonian
1042:F. pileatus
954:Stage from
819: /
757: /
408:Maastricht.
2613:Categories
2548:(4–4.6 Ga)
2512:(2.5–4 Ga)
2441:(1–1.6 Ga)
2047:Paleogene
1911:Priabonian
1677:Literature
1537:6 November
1170:References
1134:There are
1129:crocodiles
1104:Scaniornis
940:Møns Klint
930:geologist
916:Patagonian
865:Period or
849:or lowest
804:43°17′57″N
742:36°09′13″N
677:Definition
579:extinction
499:Aquitanian
472:Priabonian
126:Chronology
2575:See also:
2355:Cambrian
2288:Silurian
2257:Devonian
2152:Triassic
2121:Jurassic
1906:Bartonian
1885:Thanetian
1880:Selandian
1746:0705-3797
1699:0037-9409
1659:231981891
1532:134929774
1164:lysocline
1146:class in
1140:ammonites
1109:North Sea
1099:Australia
1084:dinosaurs
1026:F. billii
946:name for
900:Selandian
863:Paleogene
861:, of the
857:Epoch or
855:Paleocene
807:2°15′40″W
745:8°38′55″E
629:Etymology
577:K-Pg mass
463:Bartonian
436:Thanetian
426:Selandian
2200:Permian
2021:Neogene
1927:Chattian
1922:Rupelian
1901:Lutetian
1896:Ypresian
1790:Archived
1600:26606656
1559:PLOS ONE
1510:: 1–13.
1462:55038043
1280:Episodes
1246:Episodes
1119:(mostly
1117:reptiles
1048:species
1030:F. janii
1006:biozones
871:Cenozoic
660:Global (
616:Tertiary
490:Chattian
481:Rupelian
454:Lutetian
445:Ypresian
1629:Bibcode
1591:4659543
1568:Bibcode
1512:Bibcode
1442:Bibcode
1193:Bibcode
1121:turtles
1107:of the
1057:Puercan
1022:F. ulii
983:Tunisia
956:Belgian
952:Montian
948:Denmark
875:Erathem
873:Era or
853:of the
733:Tunisia
714:Iridium
570:←
549:←
531:←
223:–
213:–
203:–
193:–
183:–
173:–
163:–
153:–
143:–
116:↓
2619:Danian
2554:
1875:Danian
1744:
1697:
1657:
1598:
1588:
1530:
1460:
1362:(2006)
1360:et al.
1321:Danien
1016:genus
979:El Kef
950:. The
924:German
867:System
859:Series
843:Danian
729:El Kef
705:Formal
637:Formal
623:System
619:Period
521:
516:
511:
506:
417:Danian
40:Danian
1738:29(4)
1655:S2CID
1528:S2CID
1498:(PDF)
1469:(PDF)
1458:S2CID
1430:(PDF)
1222:(PDF)
944:Latin
928:Swiss
851:stage
795:Spain
696:Stage
651:Earth
1770:1975
1756:1996
1742:ISSN
1730:2006
1712:2004
1695:ISSN
1687:1847
1666:2022
1596:PMID
1539:2022
1477:2022
1403:PBDB
1385:2021
1127:and
1059:and
1040:and
987:GSSP
960:Mons
938:and
936:Faxe
894:61.6
841:The
835:2008
773:1991
537:PETM
55:Preęž’
1645:hdl
1637:doi
1625:110
1586:PMC
1576:doi
1520:doi
1508:525
1450:doi
1288:doi
1254:doi
1201:doi
1138:of
847:age
686:Age
662:ICS
595:ICS
2615::
2570:Ga
2566:Ma
2562:ka
1772::
1768:;
1754:;
1732::
1728:;
1718:,
1714::
1710:;
1701:.
1689::
1685:;
1653:.
1643:.
1635:.
1623:.
1617:.
1594:.
1584:.
1574:.
1564:10
1562:.
1556:.
1526:.
1518:.
1506:.
1500:.
1485:^
1456:.
1448:.
1438:30
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1432:.
1401:.
1376:.
1344:.
1340:.
1323:,
1313:^
1284:34
1282:.
1278:.
1250:29
1248:.
1244:.
1230:^
1199:.
1189:47
1187:.
1123:,
1052:.
1036:,
1032:,
1028:,
1024:,
1001:.
981:,
902:.
896:Ma
889:Ma
887:66
793:,
731:,
105:Pg
49:Ma
1966:e
1959:t
1952:v
1834:e
1827:t
1820:v
1758::
1748:.
1722:.
1668:.
1647::
1639::
1631::
1602:.
1578::
1570::
1541:.
1522::
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1452::
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1405:.
1387:.
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1296:.
1290::
1262:.
1256::
1207:.
1203::
1195::
1091:)
1020:(
926:-
664:)
621:/
399:C
397:M
388:e
386:n
384:e
382:c
380:o
378:g
376:i
374:l
372:O
363:e
361:n
359:e
357:c
355:o
353:E
342:e
340:n
338:e
336:c
334:o
332:e
330:l
328:a
326:P
317:K
315:L
306:N
296:e
294:n
292:e
290:g
288:o
286:e
284:l
282:a
280:P
270:K
260:c
258:i
256:o
254:z
252:o
250:n
248:e
246:C
235:Z
233:M
110:N
100:K
95:J
90:T
85:P
80:C
75:D
70:S
65:O
60:ęž’
31:.
20:)
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