2429:
2418:
1148:
The Ordian stage, which is use in
Australian chronostratigraphical scale, was originally supposed to be the lowest stage of the Miaolingian, but may belong to upper Series 2. As of 2024, the base of the Ordian is not defined yet.
1161:. Correlating this event on different continents has proven difficult and resolving this is essential for the definition of the lower boundary of this series. Currently the oldest trilobite known is
1490:
Zhang, Wenhao; et al. (2014). "Mass-occurrence of oncoids at the
Cambrian Series 2βSeries 3 transition: Implications for microbial resurgence following an Early Cambrian extinction".
1798:
1182:
and the marine environment are posited as the most likely cause of this extinction. At the Series 2βMiaolingian boundary, the first major trilobite extinction, known as the
1109:
yet. In part the new name will replace the older terms "Lower
Cambrian" and "Early Cambrian". The nomenclature used in Siberia uses the term "Yakutian" for this series.
1247:"Global Standard Stratotype-Section and Point (GSSP) for the conterminous base of the Miaolingian Series and Wuliuan Stage (Cambrian) at Balang, Jianhe, Guizhou, China"
1587:
1558:
1476:
1359:
1261:
1317:"Age of the lower Cambrian Vanadium deposit, East Guizhou, South China: Evidences from age of tuff and carbon isotope analysis along the Bagong section"
1791:
1650:
1118:
1102:
1082:
915:
866:
1447:
John R. Laurie, Peter D. Kruse, Glenn A. Brock, James D. Holmes, James B. Jago, Marissa J. Betts, John R. Paterson, Patrick M. Smith (April 2024).
1784:
1609:
1294:
1621:
1519:"Chemostratigraphic correlations across the first major trilobite extinction and faunal turnovers between Laurentia and South China"
1402:
2457:
1643:
1374:
1129:. Both of these stages also lack formal definition. The Siberian nomenclature distinguishes three stages (lowest first):
1025:
1807:
904:
2462:
2452:
1246:
1183:
1636:
1574:"Chronostratigraphy of the Cambrian Series 2 -Miaolingian boundary, western Stansbury Basin, South Australia"
2080:
2075:
1086:
999:
975:
800:
1290:
1552:
1517:
Jih-Pai Lin, Frederick A. Sundberg, Ganqing Jiang, Isabel P. MontaΓ±ez, Thomas Wotte (22 November 2019).
1470:
949:
1011:
2411:
1085:, lacking a precise lower boundary and subdivision into stages. The proposed lower boundary is the
1187:
780:
740:
2428:
1174:
The end of the 2nd series of the
Cambrian is marked by the first major biotic extinction of the
2173:
1760:
1581:
1572:
Courtney
Birksmith, Glenn A. Brock, Marissa J. Betts, James D. Holmes, Zhiliang Zhang (2023).
1338:
1207:
519:
1605:
2303:
2178:
2147:
1944:
1718:
1713:
1702:
1538:
1530:
1499:
1456:
1413:
1328:
1126:
1122:
698:
461:
448:
435:
2272:
2168:
2106:
2001:
1970:
1939:
1617:
1179:
939:
1360:"The 13th International Field Conference of the Cambrian Stage Subdivision Working Group"
1423:
2422:
2241:
2111:
2006:
1975:
1543:
1142:
847:
773:
237:
2446:
2142:
2132:
2101:
2064:
1996:
1965:
1573:
1518:
1448:
1403:"Tentative correlation of Cambrian Series 2 between South China and other continents"
748:
677:
657:
636:
596:
61:
2433:
2417:
2364:
2214:
2137:
1755:
1672:
1191:
1074:
508:
319:
1461:
2359:
2228:
2204:
2049:
1844:
1682:
1078:
820:
616:
374:
36:
1534:
1157:
The beginning of the 2nd series of the
Cambrian is marked by the appearance of
2354:
2314:
2257:
2157:
2054:
1928:
1828:
1776:
1739:
1163:
1158:
1130:
1090:
769:
744:
490:
415:
310:
81:
46:
1503:
1418:
1342:
1040:
1027:
2369:
2319:
2293:
2252:
2199:
2044:
2020:
1901:
1891:
1880:
1697:
1687:
1195:
1175:
979:
720:
423:
397:
276:
250:
86:
1333:
2329:
2324:
2288:
2188:
2121:
2090:
1985:
1954:
1915:
1865:
1839:
1815:
1659:
1141:. In general most subdivisions of this series rely on biostratigraphy of
1138:
1134:
1106:
1070:
286:
76:
71:
56:
51:
41:
1316:
2343:
2283:
2033:
1870:
1854:
1750:
1734:
1729:
1206:
fossils are absent, the Series 2βMiaolingian boundary is determined by
1015:
777:
499:
481:
472:
91:
66:
2379:
2262:
1896:
575:
1628:
1019:
1401:
Yuan, J.L.; Zhu, X.J.; Lin, J.P.; Zhu, M.Y. (22 September 2011).
1227:
2403:
2399:
2395:
30:
1780:
1632:
1315:
Wu, Tong; Yang, Ruidong; Gao, Junbo; Li, Jun (1 January 2021).
1576:. Conference: Palaeo Down Under 3 at Perth, Western Australia.
836:
107:
1285:
1283:
1281:
1202:
appear after this global extinction, and in areas where
1093:
which is estimated to be around 521 million years ago.
1186:, occurred. In particular, trilobites of the families
1453:
2378:
2342:
2302:
2271:
2240:
2227:
2187:
2156:
2120:
2089:
2063:
2032:
2019:
1984:
1953:
1927:
1914:
1879:
1853:
1827:
1814:
1056:
1007:
993:
985:
971:
963:
955:
945:
935:
930:
922:
910:
900:
895:
887:
882:
100:
21:
1449:"The quest for an Australian Cambrian stage scale"
1354:
1352:
1081:. Series 2 has not been formally defined by the
1117:The 2nd series is currently subdivided by the
1792:
1644:
865:Subdivision of the Cambrian according to the
8:
1620:. International Commission on Stratigraphy.
1586:: CS1 maint: multiple names: authors list (
1557:: CS1 maint: multiple names: authors list (
1475:: CS1 maint: multiple names: authors list (
1396:
1394:
1234:. International Commission on Stratigraphy.
2237:
2029:
1924:
1824:
1799:
1785:
1777:
1668:
1651:
1637:
1629:
872:Vertical axis scale: millions of years ago
1542:
1460:
1417:
1332:
1198:and South China, respectively. The first
1103:International Commission on Stratigraphy
1083:International Commission on Stratigraphy
986:Lower boundary GSSP candidate section(s)
1219:
832:
1579:
1550:
1468:
18:
7:
1105:has not named the 2nd series of the
972:Lower boundary definition candidates
809:
789:
757:
729:
708:
687:
666:
646:
625:
605:
585:
564:
2398:= kiloannum (thousands years ago);
2402:= megaannum (millions years ago);
1618:"GSSPs - The Cambrian System 2019"
16:Unnamed 2nd series of the Cambrian
14:
2406:= gigaannum (billions years ago).
1167:which marks the beginning of the
1069:is the unnamed 2nd series of the
2427:
2416:
1624:from the original on 2023-07-21.
1612:from the original on 2023-10-08.
1297:from the original on 2023-10-08
1267:from the original on 2022-03-04
1245:Zhao; et al. (June 2019).
1:
1845:Pleistocene (11.7 kaβ2.58 Ma)
1462:10.1080/03115518.2024.2327045
1606:"GSSP Table - Paleozoic Era"
1373:(4): 440β441. Archived from
1291:"GSSP Table - Paleozoic Era"
1808:Geological history of Earth
2479:
2081:Mississippian (323β359 Ma)
2076:Pennsylvanian (299β323 Ma)
1840:Holocene (presentβ11.7 ka)
1535:10.1038/s41598-019-53685-2
1184:Olenellid Biomere boundary
2393:
2365:Paleoarchean (3.2β3.6 Ga)
2215:Terreneuvian (521β539 Ma)
1666:
994:Upper boundary definition
964:Lower boundary definition
862:
858:
835:
105:
26:
2360:Mesoarchean (2.8β3.2 Ga)
2205:Miaolingian (497β509 Ma)
2050:Guadalupian (260β272 Ma)
1902:Paleocene (56.0β66.0 Ma)
1892:Oligocene (23.0β33.9 Ma)
1504:10.1016/j.gr.2014.03.015
1419:10.3140/bull.geosci.1274
2355:Neoarchean (2.5β2.8 Ga)
2320:Orosirian (1.8β2.05 Ga)
2315:Statherian (1.6β1.8 Ga)
2258:Cryogenian (635β720 Ma)
2148:Llandovery (433β444 Ma)
2055:Cisuralian (272β299 Ma)
1866:Pliocene (2.59β5.33 Ma)
1410:Bulletin of Geosciences
743:diversification, first
223:−485 —
213:−490 —
203:−495 —
193:−500 —
183:−505 —
173:−510 —
163:−515 —
153:−520 —
143:−525 —
133:−530 —
123:−535 —
113:−540 —
2458:Cambrian geochronology
2325:Rhyacian (2.05β2.3 Ga)
2294:Calymmian (1.4β1.6 Ga)
2253:Ediacaran (539β635 Ma)
2200:Furongian (485β497 Ma)
2045:Lopingian (252β260 Ma)
1871:Miocene (5.33β23.0 Ma)
1000:Oryctocephalus indicus
801:Baykonurian glaciation
2330:Siderian (2.3β2.5 Ga)
2289:Ectasian (1.2β1.4 Ga)
2210:Series 2 (509β521 Ma)
1897:Eocene (33.9β56.0 Ma)
1334:10.1515/geo-2020-0287
1194:have been extinct in
1077:series and below the
2370:Eoarchean (3.6β4 Ga)
2263:Tonian (720 Maβ1 Ga)
2143:Wenlock (427β433 Ma)
2133:Pridoli (419β423 Ma)
1073:. It lies above the
1041:26.0807Β°N 108.4138Β°E
967:Not formally defined
2425: •
2414: •
2412:Geologic time scale
2174:Middle (458β470 Ma)
2138:Ludlow (423β427 Ma)
2107:Middle (383β393 Ma)
2002:Middle (237β247 Ma)
1971:Middle (164β174 Ma)
1057:Upper GSSP ratified
1037: /
1008:Upper boundary GSSP
956:Time span formality
2423:Geology portal
2284:Stenian (1β1.2 Ga)
2179:Early (470β485 Ma)
2112:Early (393β419 Ma)
2007:Early (247β252 Ma)
1976:Early (174β201 Ma)
1945:Early (100β145 Ma)
1940:Late (66.0β100 Ma)
1523:Scientific Reports
1228:"Chart/Time Scale"
1208:chemostratigraphic
946:Stratigraphic unit
936:Chronological unit
923:Time scale(s) used
2463:Geological epochs
2453:Cambrian Series 2
2440:
2439:
2338:
2337:
2304:Paleoproterozoic
2223:
2222:
2169:Late (444β458 Ma)
2102:Late (359β383 Ma)
2015:
2014:
1997:Late (201β237 Ma)
1966:Late (145β164 Ma)
1910:
1909:
1831:(presentβ2.58 Ma)
1819:(presentβ66.0 Ma)
1774:
1773:
1769:
1768:
1492:Gondwana Research
1121:into two stages:
1067:Cambrian Series 2
1064:
1063:
1046:26.0807; 108.4138
896:Usage information
877:
876:
854:
853:
829:
828:
808:
807:
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755:
728:
727:
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706:
686:
685:
665:
664:
645:
644:
624:
623:
604:
603:
584:
583:
22:Cambrian Series 2
2470:
2434:World portal
2432:
2431:
2421:
2420:
2383:
2347:
2307:
2276:
2273:Mesoproterozoic
2245:
2238:
2233:
2192:
2161:
2125:
2094:
2068:
2037:
2030:
2025:
1989:
1958:
1932:
1925:
1920:
1884:
1858:
1832:
1825:
1820:
1801:
1794:
1787:
1778:
1669:
1653:
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1613:
1592:
1591:
1585:
1577:
1569:
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1556:
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1514:
1508:
1507:
1487:
1481:
1480:
1474:
1466:
1464:
1444:
1438:
1437:
1435:
1434:
1428:
1422:. Archived from
1421:
1407:
1398:
1389:
1388:
1386:
1385:
1379:
1364:
1356:
1347:
1346:
1336:
1321:Open Geosciences
1312:
1306:
1305:
1303:
1302:
1287:
1276:
1275:
1273:
1272:
1266:
1251:
1242:
1236:
1235:
1232:stratigraphy.org
1224:
1127:Cambrian Stage 4
1123:Cambrian Stage 3
1087:first appearance
1052:
1051:
1049:
1048:
1047:
1042:
1038:
1035:
1034:
1033:
1030:
1012:Wuliu-Zengjiayan
842:
837:
815:
810:
795:
790:
763:
758:
735:
730:
714:
709:
693:
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33:
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2407:
2389:
2381:
2374:
2345:
2334:
2305:
2298:
2274:
2267:
2243:
2242:Neoproterozoic
2232:(539 Maβ2.5 Ga)
2231:
2230:
2229:Proterozoic Eon
2219:
2190:
2183:
2159:
2152:
2123:
2116:
2092:
2085:
2066:
2059:
2035:
2023:
2022:
2011:
1987:
1980:
1956:
1949:
1930:
1918:
1917:
1906:
1882:
1875:
1856:
1849:
1830:
1818:
1817:
1810:
1805:
1775:
1770:
1765:
1744:
1723:
1707:
1662:
1660:Cambrian Period
1657:
1616:
1604:
1601:
1596:
1595:
1578:
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1570:
1566:
1549:
1516:
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1405:
1400:
1399:
1392:
1383:
1381:
1377:
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1358:
1357:
1350:
1327:(1): 999β1012.
1314:
1313:
1309:
1300:
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1289:
1288:
1279:
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1216:
1180:ocean chemistry
1155:
1153:Biostratigraphy
1143:trilobite zones
1115:
1099:
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2165:
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2065:Carboniferous
2061:
2060:
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2047:
2041:
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2016:
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2012:
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1912:
1911:
1908:
1907:
1905:
1904:
1899:
1894:
1888:
1886:
1883:(23.0β66.0 Ma)
1877:
1876:
1874:
1873:
1868:
1862:
1860:
1857:(2.58β23.0 Ma)
1851:
1850:
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1599:External links
1597:
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1482:
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1390:
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1307:
1277:
1237:
1218:
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1004:
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987:
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969:
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960:
957:
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942:
937:
933:
932:
928:
927:
926:ICS Time Scale
924:
920:
919:
912:
911:Regional usage
908:
907:
902:
901:Celestial body
898:
897:
893:
892:
889:
888:Name formality
885:
884:
880:
879:
875:
874:
863:
860:
859:
856:
855:
852:
851:
848:Glacial period
845:
843:
833:
831:
830:
827:
826:
819:
818:
816:
806:
805:
799:
798:
796:
786:
785:
767:
766:
764:
754:
753:
739:
738:
736:
726:
725:
718:
717:
715:
705:
704:
697:
696:
694:
684:
683:
676:
675:
673:
663:
662:
656:
655:
653:
643:
642:
635:
634:
632:
622:
621:
615:
614:
612:
602:
601:
595:
594:
592:
582:
581:
574:
573:
571:
562:
558:
557:
553:
552:
548:
547:
543:
542:
538:
537:
533:
532:
528:
527:
515:
514:
506:
505:
497:
496:
488:
487:
479:
478:
470:
469:
457:
456:
444:
443:
431:
430:
421:
420:
414:
413:
395:
394:
372:
371:
350:
349:
317:
316:
308:
307:
283:
282:
274:
273:
247:
246:
234:
233:
231:
226:
221:
216:
211:
206:
201:
196:
191:
186:
181:
176:
171:
166:
161:
156:
151:
146:
141:
136:
131:
126:
121:
116:
111:
106:
103:
102:
98:
97:
90:
85:
80:
75:
70:
65:
60:
55:
50:
45:
40:
35:
34:
29:~521 β ~509
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
2475:
2464:
2461:
2459:
2456:
2454:
2451:
2450:
2448:
2435:
2430:
2424:
2419:
2413:
2410:
2405:
2401:
2397:
2392:
2386:
2384:
2377:
2371:
2368:
2366:
2363:
2361:
2358:
2356:
2353:
2352:
2350:
2348:
2341:
2331:
2328:
2326:
2323:
2321:
2318:
2316:
2313:
2312:
2310:
2308:
2301:
2295:
2292:
2290:
2287:
2285:
2282:
2281:
2279:
2277:
2270:
2264:
2261:
2259:
2256:
2254:
2251:
2250:
2248:
2246:
2244:(539 Maβ1 Ga)
2239:
2236:
2234:
2226:
2216:
2213:
2211:
2208:
2206:
2203:
2201:
2198:
2197:
2195:
2193:
2186:
2180:
2177:
2175:
2172:
2170:
2167:
2166:
2164:
2162:
2155:
2149:
2146:
2144:
2141:
2139:
2136:
2134:
2131:
2130:
2128:
2126:
2119:
2113:
2110:
2108:
2105:
2103:
2100:
2099:
2097:
2095:
2088:
2082:
2079:
2077:
2074:
2073:
2071:
2069:
2062:
2056:
2053:
2051:
2048:
2046:
2043:
2042:
2040:
2038:
2031:
2028:
2026:
2021:Paleozoic Era
2018:
2008:
2005:
2003:
2000:
1998:
1995:
1994:
1992:
1990:
1983:
1977:
1974:
1972:
1969:
1967:
1964:
1963:
1961:
1959:
1952:
1946:
1943:
1941:
1938:
1937:
1935:
1933:
1931:(66.0β145 Ma)
1926:
1923:
1921:
1919:(66.0β252 Ma)
1913:
1903:
1900:
1898:
1895:
1893:
1890:
1889:
1887:
1885:
1878:
1872:
1869:
1867:
1864:
1863:
1861:
1859:
1852:
1846:
1843:
1841:
1838:
1837:
1835:
1833:
1826:
1823:
1821:
1813:
1809:
1802:
1797:
1795:
1790:
1788:
1783:
1782:
1779:
1762:
1759:
1757:
1754:
1752:
1749:
1748:
1746:
1741:
1738:
1736:
1733:
1731:
1728:
1727:
1725:
1720:
1717:
1715:
1712:
1711:
1709:
1704:
1701:
1699:
1696:
1695:
1693:
1692:
1689:
1686:
1684:
1681:
1679:
1676:
1674:
1671:
1670:
1665:
1661:
1654:
1649:
1647:
1642:
1640:
1635:
1634:
1631:
1623:
1619:
1615:
1611:
1607:
1603:
1602:
1598:
1589:
1583:
1575:
1568:
1565:
1560:
1554:
1545:
1540:
1536:
1532:
1528:
1524:
1520:
1513:
1510:
1505:
1501:
1497:
1493:
1486:
1483:
1478:
1472:
1463:
1458:
1454:
1450:
1443:
1440:
1429:on 2024-01-18
1425:
1420:
1415:
1411:
1404:
1397:
1395:
1391:
1380:on 2014-11-05
1376:
1372:
1368:
1361:
1355:
1353:
1349:
1344:
1340:
1335:
1330:
1326:
1322:
1318:
1311:
1308:
1296:
1292:
1286:
1284:
1282:
1278:
1263:
1259:
1255:
1248:
1241:
1238:
1233:
1229:
1223:
1220:
1213:
1211:
1209:
1205:
1201:
1197:
1193:
1189:
1185:
1181:
1178:. Changes in
1177:
1172:
1170:
1166:
1165:
1160:
1152:
1150:
1146:
1144:
1140:
1136:
1132:
1128:
1124:
1120:
1112:
1110:
1108:
1104:
1096:
1094:
1092:
1088:
1084:
1080:
1076:
1072:
1068:
1059:
1055:
1050:
1021:
1017:
1013:
1010:
1006:
1002:
1001:
996:
992:
988:
984:
981:
977:
974:
970:
966:
962:
958:
954:
951:
948:
944:
941:
938:
934:
929:
925:
921:
917:
913:
909:
906:
903:
899:
894:
890:
886:
881:
870:
869:, as of 2022.
868:
861:
857:
849:
844:
839:
838:
834:
822:
817:
812:
811:
802:
797:
792:
791:
782:
779:
775:
771:
765:
760:
759:
750:
749:archaeocyatha
746:
742:
737:
732:
731:
722:
716:
711:
710:
700:
695:
690:
689:
679:
678:Sirius Passet
674:
669:
668:
659:
658:Emu Bay Shale
654:
649:
648:
638:
637:Archaeocyatha
633:
628:
627:
618:
613:
608:
607:
598:
597:Burgess Shale
593:
588:
587:
577:
572:
567:
566:
563:
522:
521:
510:
501:
492:
483:
474:
464:
463:
451:
450:
438:
437:
425:
417:
409:
390:
367:
343:
313:
312:
303:
302:
279:
278:
269:
268:
242:
241:
232:
110:
109:
104:
99:
93:
88:
83:
78:
73:
68:
63:
58:
53:
48:
43:
38:
32:
25:
20:
2408:
2344:Archean Eon
2306:(1.6β2.5 Ga)
2209:
2191:(485β539 Ma)
2160:(444β485 Ma)
2124:(419β444 Ma)
2093:(359β419 Ma)
2067:(299β359 Ma)
2036:(252β299 Ma)
2024:(252β539 Ma)
1988:(201β252 Ma)
1957:(145β201 Ma)
1916:Mesozoic Era
1816:Cenozoic Era
1756:Jiangshanian
1677:
1673:Terreneuvian
1567:
1553:cite journal
1529:(1): 17392.
1526:
1522:
1512:
1495:
1491:
1485:
1471:cite journal
1452:
1442:
1431:. Retrieved
1424:the original
1409:
1382:. Retrieved
1375:the original
1370:
1366:
1324:
1320:
1310:
1299:. Retrieved
1269:. Retrieved
1257:
1253:
1240:
1231:
1222:
1203:
1199:
1192:Redlichiidae
1188:Ollenellidae
1173:
1168:
1162:
1156:
1147:
1116:
1113:Subdivisions
1100:
1075:Terreneuvian
1066:
1065:
998:
864:
518:
509:Jiangshanian
460:
447:
434:
352:
309:
285:
275:
249:
236:
2380:Hadean Eon
2158:Ordovician
1929:Cretaceous
1829:Quaternary
1683:Miaolingian
1498:: 432β450.
1412:: 397β404.
1260:: 165β184.
1169:Fallotaspis
1079:Miaolingian
1044: /
1032:108Β°24β²50β³E
821:Dresbachian
770:halkieriids
745:brachiopods
617:Kaili biota
2447:Categories
2382:(4β4.6 Ga)
2346:(2.5β4 Ga)
2275:(1β1.6 Ga)
1881:Paleogene
1740:Guzhangian
1433:2024-04-02
1384:2024-04-02
1301:2024-04-02
1271:2024-04-02
1214:References
1204:O. indicus
1200:O. indicus
1164:Lemdadella
1159:trilobites
1131:Atdabanian
1091:trilobites
1029:26Β°04β²51β³N
980:Trilobites
931:Definition
823:extinction
721:Trilobites
699:Chengjiang
639:extinction
491:Guzhangian
101:Chronology
2409:See also:
2189:Cambrian
2122:Silurian
2091:Devonian
1986:Triassic
1955:Jurassic
1698:Fortunian
1688:Furongian
1343:2391-5447
1196:Laurentia
1176:Paleozoic
883:Etymology
424:Fortunian
277:Ediacaran
2034:Permian
1855:Neogene
1761:Stage 10
1678:Series 2
1622:Archived
1610:Archived
1582:cite web
1367:Episodes
1295:Archived
1262:Archived
1254:Episodes
1139:Toyonian
1135:Botomian
1107:Cambrian
1071:Cambrian
914:Global (
891:Informal
778:hyoliths
774:mollusΡs
520:Stage 10
1751:Paibian
1735:Drumian
1730:Wuliuan
1719:Stage 4
1714:Stage 3
1703:Stage 2
1544:6874646
1016:Guizhou
997:FAD of
841:
814:←
794:←
762:←
734:←
713:←
692:←
671:←
651:←
630:←
610:←
590:←
569:←
500:Paibian
482:Drumian
473:Wuliuan
462:Stage 4
449:Stage 3
436:Stage 2
416:Early O
228:–
218:–
208:–
198:–
188:–
178:–
168:–
158:–
148:–
138:–
128:–
118:–
2388:
1541:
1341:
1210:data.
1171:zone.
1097:Naming
959:Formal
950:Series
846:Major
768:First
747:&
719:First
576:Orsten
559:
554:
549:
544:
539:
534:
529:
1427:(PDF)
1406:(PDF)
1378:(PDF)
1363:(PDF)
1265:(PDF)
1250:(PDF)
1020:China
940:Epoch
905:Earth
701:biota
680:biota
578:Fauna
1588:link
1559:link
1477:link
1339:ISSN
1190:and
1137:and
1125:and
1101:The
1060:2018
989:None
37:Preκ
1539:PMC
1531:doi
1500:doi
1457:doi
1414:doi
1329:doi
1119:ICS
1089:of
978:of
976:FAD
916:ICS
867:ICS
781:SSF
741:SSF
2449::
2404:Ga
2400:Ma
2396:ka
1608:.
1584:}}
1580:{{
1555:}}
1551:{{
1537:.
1525:.
1521:.
1496:28
1494:.
1473:}}
1469:{{
1455:.
1451:.
1408:.
1393:^
1371:31
1369:.
1365:.
1351:^
1337:.
1325:13
1323:.
1319:.
1293:.
1280:^
1258:42
1256:.
1252:.
1230:.
1145:.
1133:,
1018:,
1014:,
776:,
772:,
408:g.
389:g.
87:Pg
31:Ma
1800:e
1793:t
1786:v
1652:e
1645:t
1638:v
1590:)
1561:)
1547:.
1533::
1527:9
1506:.
1502::
1479:)
1465:.
1459::
1436:.
1416::
1387:.
1345:.
1331::
1304:.
1274:.
1003:.
918:)
523:"
517:"
465:"
459:"
452:"
446:"
439:"
433:"
406:n
404:o
402:r
400:u
398:F
387:n
385:i
383:l
381:o
379:a
377:i
375:M
366:2
363:s
361:e
359:i
357:r
355:e
353:S
342:n
340:a
338:i
336:v
334:u
332:e
330:n
328:e
326:r
324:r
322:e
320:T
311:O
301:n
299:a
297:i
295:r
293:b
291:m
289:a
287:C
267:c
265:i
263:o
261:z
259:o
257:e
255:l
253:a
251:P
240:β
238:N
92:N
82:K
77:J
72:T
67:P
62:C
57:D
52:S
47:O
42:κ
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