2004:
1993:
25:
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in the
Atlantic domain. The anoxic event lasted till the Middle Santonian (from 87.3 to 84.6 Ma) and is the longest and last such event during the Cretaceous period.
970:(Co1, at 87,0 Ma) separates the Middle from the Upper Coniacian Substage. An even shorter third order cycle caused a new transgression during the Late Coniacian.
1237:
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After a maximum of the global sea level during the early
Turonian, the Coniacian was characterized by a gradual fall of the sea level. This cycle is in
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584:
1085:"The Global Boundary Stratotype and Section Point (GSSP) for the base of the Santonian Stage, "Cantera de Margas", Olazagutia, northern Spain"
962:
seen as a first order cycle. During the middle
Coniacian a shorter, second order cycle, caused a temporary rise of the sea level (and global
1182:
Origins and accumulation of organic matter in expanded Albian to
Santonian black shale sequences on the Demerara Rise, South American margin
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The top of the
Coniacian (the base of the Santonian Stage) is defined by the appearance of the inoceramid
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The
Coniacian is often subdivided into Lower, Middle and Upper Substages. It encompasses three
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1212:, at the website of Norges Network of offshore records of geology and stratigraphy
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and 86.3 Β± 0.7 Ma (million years ago). The
Coniacian is preceded by the
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The base of the
Coniacian Stage is at the first appearance of the
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1970:
912:
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the
Coniacian overlaps just one ammonite biozone: that of
915:) is located in Salzgitter-Salder, Lower Saxony, Germany.
1083:
Lamolda, M.; Paul, C.; Peryt, D.; Pons, J. (March 2014).
966:) on top of the longer first order trend. The following
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49:. Unsourced material may be challenged and removed.
950:, a relatively long period with normal polarity.
911:. The official reference profile for the base (a
1174:Meyers, P.A.; Bernasconi, S.M. & Forster, A.
583:Subdivision of the Cretaceous according to the
1367:
1231:
8:
1156:Gradstein, F.M.; Ogg, J.G. & Smith, A.G.
891:. It was first defined by French geologist
590:Vertical axis scale: millions of years ago.
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1210:Stratigraphic chart of the Late Cretaceous
1064:International Commission on Stratigraphy.
1100:
879:The Coniacian is named after the city of
109:Learn how and when to remove this message
1056:
973:Beginning in the Middle Coniacian, an
954:Sequence stratigraphy and geochemistry
120:
1126:(2004) for a detailed version of the
7:
981:, causing large scale deposition of
930:The Coniacian overlaps the regional
859:and spans the time between 89.8 Β± 1
557:
47:adding citations to reliable sources
1973:= kiloannum (thousands years ago);
1977:= megaannum (millions years ago);
14:
1981:= gigaannum (billions years ago).
2002:
1991:
23:
1102:10.18814/epiiugs/2014/v37i1/001
1011:Paratexanites serratomarginatus
34:needs additional citations for
948:Cretaceous Magnetic Quiet Zone
908:Cremnoceramus deformis erectus
765:FAD of the Inoceramid Bivalve
698:Cremnoceramus deformis erectus
1:
1420:Pleistocene (11.7 kaβ2.58 Ma)
924:Cladoceramus undulatoplicatus
845:. It is a subdivision of the
768:Cladoceramus undulatoplicatus
1199:GeoWhen Database - Coniacian
1383:Geological history of Earth
942:, the Coniacian is part of
2059:
1656:Mississippian (323β359 Ma)
1651:Pennsylvanian (299β323 Ma)
1415:Holocene (presentβ11.7 ka)
1168:Cambridge University Press
1164:A Geologic Time Scale 2004
1040:Forresteria petrocoriensis
16:Age of the Late Cretaceous
1968:
1940:Paleoarchean (3.2β3.6 Ga)
1790:Terreneuvian (521β539 Ma)
1253:
1204:Late Cretaceous timescale
875:Stratigraphic definitions
762:Upper boundary definition
683:Lower boundary definition
580:
214:
128:
2043:Cretaceous geochronology
1935:Mesoarchean (2.8β3.2 Ga)
1780:Miaolingian (497β509 Ma)
1625:Guadalupian (260β272 Ma)
1477:Paleocene (56.0β66.0 Ma)
1467:Oligocene (23.0β33.9 Ma)
1066:"ICS - Chart/Time Scale"
977:(OAE-3) occurred in the
131:89.8 Β± 0.3 β 86.3 Β± 0.5
1930:Neoarchean (2.5β2.8 Ga)
1895:Orosirian (1.8β2.05 Ga)
1890:Statherian (1.6β1.8 Ga)
1833:Cryogenian (635β720 Ma)
1723:Llandovery (433β444 Ma)
1630:Cisuralian (272β299 Ma)
1441:Pliocene (2.59β5.33 Ma)
1184:, Organic Geochemistry
1027:Peroniceras tridorsatum
262:−100 —
252:−110 —
242:−120 —
232:−130 —
222:−140 —
1900:Rhyacian (2.05β2.3 Ga)
1869:Calymmian (1.4β1.6 Ga)
1828:Ediacaran (539β635 Ma)
1775:Furongian (485β497 Ma)
1620:Lopingian (252β260 Ma)
1446:Miocene (5.33β23.0 Ma)
1260:Lower/Early Cretaceous
292:−70 —
282:−80 —
272:−90 —
1905:Siderian (2.3β2.5 Ga)
1864:Ectasian (1.2β1.4 Ga)
1785:Series 2 (509β521 Ma)
1472:Eocene (33.9β56.0 Ma)
1265:Upper/Late Cretaceous
1019:Gauthiericeras margae
960:sequence stratigraphy
1945:Eoarchean (3.6β4 Ga)
1838:Tonian (720 Maβ1 Ga)
1718:Wenlock (427β433 Ma)
1708:Pridoli (419β423 Ma)
1130:' geologic timescale
1070:www.stratigraphy.org
867:and followed by the
43:improve this article
2000: •
1989: •
1987:Geologic time scale
1749:Middle (458β470 Ma)
1713:Ludlow (423β427 Ma)
1682:Middle (383β393 Ma)
1577:Middle (237β247 Ma)
1546:Middle (164β174 Ma)
946:C34, the so-called
944:magnetic chronozone
940:magnetostratigraphy
820:Upper GSSP ratified
800: /
775:Upper boundary GSSP
754:Lower GSSP ratified
738:52.1243Β°N 10.3295Β°E
734: /
705:Lower boundary GSSP
675:Time span formality
1998:Geology portal
1859:Stenian (1β1.2 Ga)
1754:Early (470β485 Ma)
1687:Early (393β419 Ma)
1582:Early (247β252 Ma)
1551:Early (174β201 Ma)
1520:Early (100β145 Ma)
1515:Late (66.0β100 Ma)
843:geologic timescale
804:42.8668Β°N 2.1968Β°W
665:Stratigraphic unit
655:Chronological unit
642:Time scale(s) used
2015:
2014:
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1912:
1879:Paleoproterozoic
1798:
1797:
1744:Late (444β458 Ma)
1677:Late (359β383 Ma)
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1572:Late (201β237 Ma)
1541:Late (145β164 Ma)
1485:
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1406:(presentβ2.58 Ma)
1394:(presentβ66.0 Ma)
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1247:Cretaceous Period
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615:Usage information
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854:Upper Cretaceous
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1817:Neoproterozoic
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1804:Proterozoic Eon
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979:Atlantic Ocean
964:transgressions
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1596:Paleozoic Era
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1558:
1552:
1549:
1547:
1544:
1542:
1539:
1538:
1536:
1534:
1527:
1521:
1518:
1516:
1513:
1512:
1510:
1508:
1506:(66.0β145 Ma)
1501:
1498:
1496:
1494:(66.0β252 Ma)
1488:
1478:
1475:
1473:
1470:
1468:
1465:
1464:
1462:
1460:
1453:
1447:
1444:
1442:
1439:
1438:
1436:
1434:
1427:
1421:
1418:
1416:
1413:
1412:
1410:
1408:
1401:
1398:
1396:
1388:
1384:
1377:
1372:
1370:
1365:
1363:
1358:
1357:
1354:
1337:
1336:Maastrichtian
1334:
1332:
1329:
1327:
1324:
1322:
1319:
1317:
1314:
1312:
1309:
1308:
1306:
1301:
1298:
1296:
1293:
1291:
1288:
1286:
1283:
1281:
1278:
1276:
1273:
1272:
1270:
1269:
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1234:
1229:
1227:
1222:
1221:
1218:
1211:
1208:
1205:
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1200:
1197:
1196:
1192:
1187:
1183:
1179:
1172:
1169:
1165:
1161:
1154:
1153:
1149:
1142:
1136:
1133:
1129:
1125:
1119:
1116:
1103:
1098:
1094:
1090:
1086:
1079:
1076:
1071:
1067:
1060:
1057:
1051:
1046:
1044:
1043:
1041:
1036:
1035:boreal domain
1029:
1028:
1023:
1021:
1020:
1015:
1013:
1012:
1007:
1006:
1005:
1003:
1002:Tethys domain
999:
996:
988:
986:
984:
980:
976:
971:
969:
965:
961:
953:
951:
949:
945:
941:
937:
933:
928:
926:
925:
921:
916:
914:
910:
909:
904:
901:
896:
894:
893:Henri Coquand
890:
886:
882:
874:
872:
870:
866:
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848:
844:
840:
836:
832:
822:
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813:
784:
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770:
769:
764:
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752:
747:
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714:
710:
707:
703:
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688:
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681:
677:
673:
670:
667:
663:
660:
657:
653:
648:
644:
640:
636:
632:
628:
625:
622:
618:
613:
609:
605:
600:
588:
587:, as of 2022.
586:
579:
571:
565:
560:
559:
556:
532:
522:
521:Maastrichtian
513:
504:
495:
486:
477:
468:
459:
450:
441:
432:
423:
415:
406:
393:
382:
373:
362:
361:
348:
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326:
325:
312:
310:
301:
219:
218:
213:
208:
195:
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185:
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150:
145:
140:
134:
127:
122:
113:
110:
102:
99:February 2024
91:
88:
84:
81:
77:
74:
70:
67:
63:
60: β
59:
55:
54:Find sources:
48:
44:
38:
37:
32:This article
30:
26:
21:
20:
1983:
1919:Archean Eon
1881:(1.6β2.5 Ga)
1766:(485β539 Ma)
1735:(444β485 Ma)
1699:(419β444 Ma)
1668:(359β419 Ma)
1642:(299β359 Ma)
1611:(252β299 Ma)
1599:(252β539 Ma)
1563:(201β252 Ma)
1532:(145β201 Ma)
1491:Mesozoic Era
1391:Cenozoic Era
1320:
1185:
1181:
1177:
1163:
1159:
1140:
1135:
1123:
1118:
1106:. Retrieved
1092:
1088:
1078:
1069:
1059:
1038:
1032:
1025:
1017:
1009:
992:
983:black shales
975:anoxic event
972:
957:
929:
922:
917:
906:
897:
878:
830:
828:
823:January 2013
766:
696:
582:
493:
354:
342:
332:
320:
306:
105:
96:
86:
79:
72:
65:
53:
41:Please help
36:verification
33:
1955:Hadean Eon
1733:Ordovician
1504:Cretaceous
1404:Quaternary
1285:Hauterivian
1280:Valanginian
1139:See Meyers
1108:24 December
1095:(1): 2β13.
989:Subdivision
807: /
741: /
440:Hauterivian
431:Valanginian
58:"Coniacian"
2022:Categories
1957:(4β4.6 Ga)
1921:(2.5β4 Ga)
1850:(1β1.6 Ga)
1456:Paleogene
1311:Cenomanian
1275:Berriasian
1150:Literature
1047:References
968:regression
932:Emscherian
900:inoceramid
887:region of
792:42Β°52β²00β³N
779:Olazagutia
729:10Β°19β²46β³E
726:52Β°07β²27β³N
709:Salzgitter
691:Inoceramid
650:Definition
570:extinction
476:Cenomanian
422:Berriasian
345:Cretaceous
210:Chronology
69:newspapers
2028:Coniacian
1984:See also:
1764:Cambrian
1697:Silurian
1666:Devonian
1561:Triassic
1530:Jurassic
1331:Campanian
1326:Santonian
1321:Coniacian
1290:Barremian
934:Stage of
895:in 1857.
889:Saintonge
869:Santonian
831:Coniacian
795:2Β°11β²48β³W
602:Etymology
568:K-Pg mass
512:Campanian
503:Santonian
494:Coniacian
449:Barremian
413:Tithonian
124:Coniacian
1609:Permian
1430:Neogene
1316:Turonian
1089:Episodes
1024:zone of
1016:zone of
1008:zone of
998:biozones
995:ammonite
905:species
865:Turonian
757:May 2021
715:quarry,
633:Global (
485:Turonian
309:Mesozoic
1033:In the
1000:in the
936:Germany
920:bivalve
903:bivalve
883:in the
841:in the
717:Germany
694:Bivalve
689:of the
562:←
297:–
287:–
277:–
267:–
257:–
247:–
237:–
227:–
200:↓
83:scholar
1963:
1300:Albian
1295:Aptian
1143:(2006)
1141:et al.
1124:et al.
885:French
881:Cognac
857:Series
833:is an
713:Salder
678:Formal
610:Formal
552:
547:
542:
537:
530:Danian
467:Albian
458:Aptian
85:
78:
71:
64:
56:
1052:Notes
850:Epoch
839:stage
783:Spain
669:Stage
624:Earth
381:Early
90:JSTOR
76:books
1178:2006
1160:2004
1110:2020
913:GSSP
829:The
392:Late
139:Preκ
62:news
1128:ICS
1097:doi
852:or
837:or
835:age
687:FAD
659:Age
635:ICS
585:ICS
45:by
2024::
1979:Ga
1975:Ma
1971:ka
1186:37
1180::
1176:;
1166:,
1162::
1158:;
1093:37
1091:.
1087:.
1068:.
1004::
927:.
871:.
861:Ma
781:,
189:Pg
133:Ma
1375:e
1368:t
1361:v
1239:e
1232:t
1225:v
1170:.
1112:.
1099::
1072:.
1042:.
711:-
637:)
404:C
402:P
371:J
369:L
359:g
357:P
334:J
324:Z
322:C
194:N
184:K
179:J
174:T
169:P
164:C
159:D
154:S
149:O
144:κ
112:)
106:(
101:)
97:(
87:Β·
80:Β·
73:Β·
66:Β·
39:.
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