Knowledge

Piacenzian

Source πŸ“

2564: 2553: 1105:: "Vertebrate fossils record a faunal turnover indicative of more open and probable arid habitats than those reconstructed earlier in this region, in broad agreement with hypotheses addressing the role of environmental forcing in hominin evolution at this time." This interpretation is consistent with hypotheses that emphasize the 978:
the concentration of carbon dioxide peaked at approximately 389 ppm (in the range 381–427 ppm with 95% confidence), thus similar to the concentration during the 2010s. The Piacenzian can therefore be used as an analogue to the future climate and sea level to expect if the carbon dioxide concentration
990:
Climate of the Piacenzian would have started as a somewhat wet and warm period in North America occurring just after a brief cooling period of the Zanclean. Deposition of sediments and mollusks of the Piacenzian correspond with the rise in sea level creating the Tamiami Subsea and Jackson Subsea of
878:
Carbon dioxide levels during the Piacenzian were similar to those of today, making this age, with global mean temperature 2–3 Β°C higher and sea levels about twenty meters higher than today, an important analogue for predictions of the future of our world.
973:
of Antarctica was also less prominent than today and sea levels were approximately twenty meters higher than the present. The global mean temperature was 2–3 Β°C warmer than the pre-industrial temperature. During the
1135:
Krijgsman, W.; GarcΓ©s, M.; Langereis, C. G.; Daams, R.; Van Dam, J.; Van Der Meulen, A. J.; AgustΓ­, J.; Cabrera, L. (1996). "A new chronology for the middle to late Miocene continental record in Spain".
1500:
Petuch, Edward J., Ph.D. Florida Atlantic University, Department of Geodsciences. Cenozoic Seas: The View From Eastern North America. CRC Press, Dec. 29, 2003.
1733:
Thompson, R. S.; Fleming, R. F. (1996). "Middle Pliocene vegetation: reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling".
1933: 1544: 1361: 1926: 1817: 602: 535: 1032:
date to just after the end of the Piacenzian (2.58 Ma), a fossilized jawbone that exhibits traits that are transitional between
1402: 1919: 1784: 979:
stabilizes at this level. In particular, the KM5c interglacial during the Mid-Piacenzian Warm Period occurred during an
1339: 1696: 1505: 868: 757: 677: 860: 853: 1063: 17: 1368: 1810: 1790: 1942: 1778: 1091:). Based on geological evidence from the Afar region, the individual would have lived just after a major 591: 975: 497: 931:
The top of the Piacenzian (the base of the Quaternary System and the Pleistocene Series) is defined
2597: 1654:"The Global Standard Stratotype-section and Point (GSSP) of the Piacenzian Stage (Middle Pliocene)" 1244:"The Global Standard Stratotype-section and Point (GSSP) of the Piacenzian Stage (Middle Pliocene)" 842: 1708:"The Gelasian Stage (Upper Pliocene): A new unit of the global standard chronostratigraphic scale" 1286:"The Gelasian Stage (Upper Pliocene): A new unit of the global standard chronostratigraphic scale" 2215: 2210: 1803: 1768: 944: 940: 1216: 1092: 966: 563: 1149: 1742: 1612: 1438: 1145: 807: 636: 1724: 1707: 1670: 1653: 1593:
Erin N. DiMaggio EN; Campisano CJ; Rowan J; Dupont-Nivet G; Deino AL; et al. (2015).
1571: 1302: 1285: 1263: 8: 2587: 2546: 980: 932: 803: 1746: 1616: 1519: 1442: 1003:. Dates have been established on the basis of the genera and species of mollusks found. 1854: 1787:
at the website of the Norwegian network of offshore records of geology and stratigraphy
1595:"Late Pliocene fossiliferous sedimentary record and the environmental context of early 1461: 1422: 1340:"Global Chronostratigraphical Correlation Table for the Last 2.7 Million Years. v.2011" 1192: 875:
and Waltonian Stage as late Piacenzian, while others regard them as early Pleistocene.
872: 386: 1243: 2592: 2344: 2308: 1754: 1692: 1630: 1603: 1501: 1466: 1398: 1157: 1106: 1100: 559: 1592: 867:
and Romanian regional stages of Europe, and the Waipipian and Mangapanian stages of
2438: 2313: 2282: 2079: 1750: 1719: 1684: 1665: 1620: 1456: 1446: 1317: 1297: 1258: 1184: 1153: 1022: 984: 1421:
de la Vega, E.; Chalk, T. B.; Wilson, P. A.; Bysani, R. P.; Foster, G. L. (2020).
1044:
in 2015. The find was made by Ethiopian student Chalachew Seyoum at a site called
2538: 2534: 2530: 2407: 2303: 2241: 2136: 2105: 2074: 1172: 943:), and isotopic stage 103. Above this point there are notable extinctions of the 819: 663: 41: 2563: 1134: 2557: 2376: 2246: 2141: 2110: 1451: 1000: 992: 1911: 1781:, at the website of the subcommission for stratigraphic information of the ICS 2581: 2277: 2267: 2236: 2199: 2131: 2100: 1688: 1548: 1078: 1065: 1041: 902:
The base of the Piacenzian is at the base of the Gauss chronozone and at the
846: 811: 772: 759: 692: 679: 626: 72: 1625: 1594: 2568: 2499: 2349: 2272: 1869: 1634: 1470: 1028: 413: 983:
close to the current situation, with similar geographical distribution of
2494: 2363: 2339: 2184: 1979: 1859: 1283: 1241: 1057: 1053: 1049: 1045: 996: 888: 831: 395: 365: 47: 2489: 2449: 2392: 2292: 2189: 2063: 1963: 1367:. Sites of Special Scientific Interest. Natural England. Archived from 1196: 949: 936: 903: 736: 730: 726: 310: 92: 57: 2552: 2504: 2454: 2428: 2387: 2334: 2179: 2155: 2036: 2026: 2015: 1879: 1874: 970: 864: 431: 422: 318: 274: 97: 1188: 2464: 2459: 2423: 2323: 2256: 2225: 2120: 2089: 2050: 2000: 1974: 1950: 1890: 1864: 1844: 1095:, during which forests and waterways were rapidly replaced by arid 907: 896: 827: 823: 815: 556: 457: 440: 404: 376: 351: 250: 87: 82: 67: 62: 52: 1284:
Rio, Domenico; R. Sprovieri; D. Castradori; E. Di Stefano (1998).
2478: 2418: 2168: 2005: 1989: 1839: 1826: 1795: 1109:
as the ancestral environment which shaped the evolution of early
1096: 857: 518: 330: 288: 102: 77: 2514: 2397: 2031: 1706:
Rio, D.; Sprovieri, R.; Castradori, D.; Stefano, E. Di (1998).
1652:
Castradori, D.; Rio, D.; Hilgen, F. J.; Lourens, L. J. (1998).
925: 850: 838: 667: 1026:. While the oldest known fossils unambiguously identified as 891:
stratigrapher Karl Mayer-Eymar in 1858. It is named after the
1705: 910: 892: 822:
and 2.58 Ma (million years ago). The Piacenzian is after the
671: 1427:
during the Mid-Piacenzian Warm Period and the M2 glaciation"
1242:
Castradori, D.; D. Rio; F. J. Hilgen; L. J. Lourens (1998).
1420: 1016: 921: 750: 1791:
Piacenzian Microfossils: images of Piacenzian Foraminifera
1651: 1099:. Regarding the Afar region, and as stated in the journal 887:
The Piacenzian was introduced in scientific literature by
1679:
Gradstein, F. M.; Ogg, J. G.; Smith, A. G., eds. (2005).
1523: 1545:"Oldest known member of human family found in Ethiopia" 1397:(4th ed.). Oxford University Press. p. 626. 969:
started to take hold in the Northern hemisphere. The
722:
Base of magnetic polarity chronozone C2r (Matuyama)
654:
Base of Gauss/Gilbert (C2An/C2Ar) magnetic reversal
125: 1416: 1414: 1678: 1395:Oxford Dictionary of Geology & Earth Sciences 1173:"Neogene Expansion of the North American Prairie" 2579: 1237: 1235: 1233: 1170: 924:for the Piacenzian Stage is at Punta Piccola on 863:. It also correlates with the Astian, Redonian, 1941: 1732: 1411: 1927: 1811: 1683:. Cambridge, UK: Cambridge University Press. 1230: 1537: 1517: 1164: 1128: 534:Subdivision of the Neogene according to the 1006: 965:The Piacenzian was the last age before the 1934: 1920: 1818: 1804: 1014:The late Piacenzian may be when the genus 1723: 1669: 1624: 1511: 1460: 1450: 1301: 1262: 871:. Some authorities describe the British 818:. It spans the time between 3.6 Β± 0.005 14: 2580: 1572:"'First human' discovered in Ethiopia" 1520:"'First human' discovered in Ethiopia" 1392: 531: 1915: 1799: 1569: 1020:developed out of the ancestral genus 541:Vertical axis: millions of years ago. 991:Florida, Duplin Subsea generally of 856:and falls inside the more extensive 506: 486: 2533:= kiloannum (thousands years ago); 1138:Earth and Planetary Science Letters 24: 2537:= megaannum (millions years ago); 1825: 935:as the base of the Matuyama (C2r) 25: 2609: 2541:= gigaannum (billions years ago). 1762: 2562: 2551: 45: 1725:10.18814/epiiugs/1998/v21i2/002 1671:10.18814/epiiugs/1998/v21i2/003 1586: 1563: 1494: 1477: 1303:10.18814/epiiugs/1998/v21i2/002 1264:10.18814/epiiugs/1998/v21i2/003 1570:Ghosh, Pallab (4 March 2015). 1386: 1354: 1332: 1310: 1277: 1209: 861:North American land mammal age 854:South American land mammal age 485: 13: 1: 1980:Pleistocene (11.7 ka–2.58 Ma) 1645: 1518:Pallab Ghosh (4 March 2015). 1116: 995:, and Yorktown Subsea of the 882: 1755:10.1016/0377-8398(95)00051-8 1158:10.1016/0012-821X(96)00109-4 7: 1943:Geological history of Earth 1320:. British Geological Survey 532: 245: 10: 2614: 2216:Mississippian (323–359 Ma) 2211:Pennsylvanian (299–323 Ma) 1975:Holocene (present–11.7 ka) 1681:A Geologic Time Scale 2004 1452:10.1038/s41598-020-67154-8 976:Mid-Piacenzian Warm Period 960: 837:The Piacenzian is roughly 792:1996 (as base of Gelasian) 749:Monte San Nicola Section, 27:Latest age of the Pliocene 2528: 2513: 2500:Paleoarchean (3.2–3.6 Ga) 2477: 2437: 2406: 2375: 2362: 2350:Terreneuvian (521–539 Ma) 2322: 2291: 2255: 2224: 2198: 2167: 2154: 2119: 2088: 2062: 2049: 2014: 1988: 1962: 1949: 1833: 1342:. University of Cambridge 1171:Retallack, G. J. (1997). 845:MN 16, overlaps the late 788: 745: 717:Upper boundary definition 716: 708: 658: 651:Lower boundary definition 650: 642: 632: 622: 617: 609: 597: 587: 582: 574: 569: 552: 498:Messinian salinity crisis 123: 118: 37: 32: 2495:Mesoarchean (2.8–3.2 Ga) 2340:Miaolingian (497–509 Ma) 2185:Guadalupian (260–272 Ma) 2037:Paleocene (56.0–66.0 Ma) 2027:Oligocene (23.0–33.9 Ma) 1735:Marine Micropaleontology 1689:10.1017/CBO9780511536045 1393:Allaby, Michael (2013). 1121: 950:Discoaster pentaradiatus 933:magnetostratigraphically 843:European land mammal age 802:is in the international 731:Discoaster pentaradiatus 128: 2490:Neoarchean (2.5–2.8 Ga) 2455:Orosirian (1.8–2.05 Ga) 2450:Statherian (1.6–1.8 Ga) 2393:Cryogenian (635–720 Ma) 2283:Llandovery (433–444 Ma) 2190:Cisuralian (272–299 Ma) 2001:Pliocene (2.59–5.33 Ma) 1626:10.1126/science.aaa1415 1150:1996E&PSL.142..367K 945:calcareous nannofossils 941:Gauss-Matuyama reversal 914:Globorotalia margaritae 826:and is followed by the 662:Punta Piccola Section, 2460:Rhyacian (2.05–2.3 Ga) 2429:Calymmian (1.4–1.6 Ga) 2388:Ediacaran (539–635 Ma) 2335:Furongian (485–497 Ma) 2180:Lopingian (252–260 Ma) 2006:Miocene (5.33–23.0 Ma) 1040:was discovered in the 967:Quaternary glaciations 201:−10 — 191:−12 — 181:−14 — 171:−16 — 161:−18 — 151:−20 — 141:−22 — 131:−24 — 2465:Siderian (2.3–2.5 Ga) 2424:Ectasian (1.2–1.4 Ga) 2345:Series 2 (509–521 Ma) 2032:Eocene (33.9–56.0 Ma) 1217:"ICS Timescale Chart" 981:orbital configuration 918:Pulleniatina primalis 241:−2 — 231:−4 — 221:−6 — 211:−8 — 2505:Eoarchean (3.6–4 Ga) 2398:Tonian (720 Ma–1 Ga) 2278:Wenlock (427–433 Ma) 2268:Pridoli (419–423 Ma) 1599:from Afar, Ethiopia" 1318:"Red Crag Formation" 1224:www.stratigraphy.org 1113:and other hominins. 1007:Origin of the genus 955:Discoaster surculus 2560: • 2549: • 2547:Geologic time scale 2309:Middle (458–470 Ma) 2273:Ludlow (423–427 Ma) 2242:Middle (383–393 Ma) 2137:Middle (237–247 Ma) 2106:Middle (164–174 Ma) 1747:1996MarMP..27...27T 1617:2015Sci...347.1355D 1487:(2005), p. 28; Rio 1443:2020NatSR..1011002D 1362:"The Naze citation" 1075: /  1058:Afar Regional State 804:geologic time scale 789:Upper GSSP ratified 773:37.1469Β°N 14.2035Β°E 769: /  746:Upper boundary GSSP 737:Discoaster surculus 709:Lower GSSP ratified 693:37.2889Β°N 13.4933Β°E 689: /  659:Lower boundary GSSP 643:Time span formality 2558:Geology portal 2419:Stenian (1–1.2 Ga) 2314:Early (470–485 Ma) 2247:Early (393–419 Ma) 2142:Early (247–252 Ma) 2111:Early (174–201 Ma) 2080:Early (100–145 Ma) 2075:Late (66.0–100 Ma) 1431:Scientific Reports 1404:978-0-19-96530 6-5 873:Red Crag Formation 725:Extinction of the 633:Stratigraphic unit 623:Chronological unit 610:Time scale(s) used 2575: 2574: 2473: 2472: 2439:Paleoproterozoic 2358: 2357: 2304:Late (444–458 Ma) 2237:Late (359–383 Ma) 2150: 2149: 2132:Late (201–237 Ma) 2101:Late (145–164 Ma) 2045: 2044: 1966:(present–2.58 Ma) 1954:(present–66.0 Ma) 1909: 1908: 1904: 1903: 1785:Neogene timescale 1779:Neogene timescale 796: 795: 583:Usage information 547: 546: 527: 526: 505: 504: 16:(Redirected from 2605: 2569:World portal 2567: 2566: 2556: 2555: 2518: 2482: 2442: 2411: 2408:Mesoproterozoic 2380: 2373: 2372: 2368: 2327: 2296: 2260: 2229: 2203: 2172: 2165: 2164: 2160: 2124: 2093: 2067: 2060: 2059: 2055: 2019: 1993: 1967: 1960: 1959: 1955: 1936: 1929: 1922: 1913: 1912: 1836: 1835: 1820: 1813: 1806: 1797: 1796: 1758: 1729: 1727: 1702: 1675: 1673: 1639: 1638: 1628: 1611:(6228): 1355–9. 1590: 1584: 1583: 1581: 1579: 1567: 1561: 1560: 1558: 1556: 1541: 1535: 1534: 1532: 1530: 1515: 1509: 1498: 1492: 1481: 1475: 1474: 1464: 1454: 1418: 1409: 1408: 1390: 1384: 1383: 1381: 1379: 1373: 1366: 1358: 1352: 1351: 1349: 1347: 1336: 1330: 1329: 1327: 1325: 1314: 1308: 1307: 1305: 1281: 1275: 1274: 1272: 1271: 1266: 1248: 1239: 1228: 1227: 1221: 1213: 1207: 1206: 1204: 1203: 1168: 1162: 1161: 1144:(3–4): 367–380. 1132: 1090: 1089: 1087: 1086: 1085: 1080: 1076: 1073: 1072: 1071: 1068: 1034:Australopithecus 1023:Australopithecus 985:solar insolation 784: 783: 781: 780: 779: 778:37.1469; 14.2035 774: 770: 767: 766: 765: 762: 704: 703: 701: 700: 699: 698:37.2889; 13.4933 694: 690: 687: 686: 685: 682: 553:Formerly part of 522: 512: 507: 500: 492: 487: 460: 452: 443: 434: 425: 416: 407: 398: 389: 379: 370: 360: 345: 323: 304: 279: 268: 242: 237: 232: 227: 222: 217: 212: 207: 202: 197: 192: 187: 182: 177: 172: 167: 162: 157: 152: 147: 142: 137: 132: 126: 114: 44: 30: 29: 21: 2613: 2612: 2608: 2607: 2606: 2604: 2603: 2602: 2598:Geological ages 2578: 2577: 2576: 2571: 2561: 2550: 2542: 2524: 2516: 2509: 2480: 2469: 2440: 2433: 2409: 2402: 2378: 2377:Neoproterozoic 2367:(539 Ma–2.5 Ga) 2366: 2365: 2364:Proterozoic Eon 2354: 2325: 2318: 2294: 2287: 2258: 2251: 2227: 2220: 2201: 2194: 2170: 2158: 2157: 2146: 2122: 2115: 2091: 2084: 2065: 2053: 2052: 2041: 2017: 2010: 1991: 1984: 1965: 1953: 1952: 1945: 1940: 1910: 1905: 1900: 1884: 1829: 1824: 1765: 1699: 1648: 1643: 1642: 1591: 1587: 1577: 1575: 1568: 1564: 1554: 1552: 1543: 1542: 1538: 1528: 1526: 1516: 1512: 1499: 1495: 1482: 1478: 1426: 1423:"Atmospheric CO 1419: 1412: 1405: 1391: 1387: 1377: 1375: 1374:on 4 March 2016 1371: 1364: 1360: 1359: 1355: 1345: 1343: 1338: 1337: 1333: 1323: 1321: 1316: 1315: 1311: 1282: 1278: 1269: 1267: 1246: 1240: 1231: 1219: 1215: 1214: 1210: 1201: 1199: 1189:10.2307/3515337 1169: 1165: 1133: 1129: 1124: 1119: 1083: 1081: 1079:11.36Β°N 40.86Β°E 1077: 1074: 1069: 1066: 1064: 1062: 1061: 1012: 963: 885: 777: 775: 771: 768: 763: 760: 758: 756: 755: 754: 753:, Sicily, Italy 697: 695: 691: 688: 683: 680: 678: 676: 675: 674: 664:Porto Empedocle 548: 543: 542: 540: 523: 517:North American 516: 510: 501: 496: 490: 483: 482: 478: 477: 473: 472: 468: 467: 463: 462: 458: 454: 453: 448: 445: 444: 439: 436: 435: 430: 427: 426: 421: 418: 417: 412: 409: 408: 403: 400: 399: 394: 391: 390: 385: 382: 381: 377: 373: 372: 368: 366: 362: 361: 357: 355: 353: 350: 347: 346: 342: 340: 338: 336: 334: 332: 329: 326: 325: 321: 319: 315: 314: 306: 305: 300: 298: 296: 294: 292: 290: 286: 283: 282: 277: 275: 270: 269: 264: 262: 260: 258: 256: 254: 252: 248: 243: 240: 238: 235: 233: 230: 228: 225: 223: 220: 218: 215: 213: 210: 208: 205: 203: 200: 198: 195: 193: 190: 188: 185: 183: 180: 178: 175: 173: 170: 168: 165: 163: 160: 158: 155: 153: 150: 148: 145: 143: 140: 138: 135: 133: 130: 113: 112: 111: 110: 105: 100: 95: 90: 85: 80: 75: 70: 65: 60: 55: 50: 40:3.600 – 2.58 39: 38: 28: 23: 22: 15: 12: 11: 5: 2611: 2601: 2600: 2595: 2590: 2573: 2572: 2529: 2526: 2525: 2522: 2520: 2511: 2510: 2508: 2507: 2502: 2497: 2492: 2486: 2484: 2475: 2474: 2471: 2470: 2468: 2467: 2462: 2457: 2452: 2446: 2444: 2435: 2434: 2432: 2431: 2426: 2421: 2415: 2413: 2404: 2403: 2401: 2400: 2395: 2390: 2384: 2382: 2370: 2360: 2359: 2356: 2355: 2353: 2352: 2347: 2342: 2337: 2331: 2329: 2320: 2319: 2317: 2316: 2311: 2306: 2300: 2298: 2289: 2288: 2286: 2285: 2280: 2275: 2270: 2264: 2262: 2253: 2252: 2250: 2249: 2244: 2239: 2233: 2231: 2222: 2221: 2219: 2218: 2213: 2207: 2205: 2200:Carboniferous 2196: 2195: 2193: 2192: 2187: 2182: 2176: 2174: 2162: 2152: 2151: 2148: 2147: 2145: 2144: 2139: 2134: 2128: 2126: 2117: 2116: 2114: 2113: 2108: 2103: 2097: 2095: 2086: 2085: 2083: 2082: 2077: 2071: 2069: 2057: 2047: 2046: 2043: 2042: 2040: 2039: 2034: 2029: 2023: 2021: 2018:(23.0–66.0 Ma) 2012: 2011: 2009: 2008: 2003: 1997: 1995: 1992:(2.58–23.0 Ma) 1986: 1985: 1983: 1982: 1977: 1971: 1969: 1957: 1947: 1946: 1939: 1938: 1931: 1924: 1916: 1907: 1906: 1902: 1901: 1899: 1898: 1893: 1887: 1885: 1883: 1882: 1877: 1872: 1867: 1862: 1857: 1851: 1848: 1847: 1845:Pliocene Epoch 1842: 1834: 1831: 1830: 1827:Neogene Period 1823: 1822: 1815: 1808: 1800: 1794: 1793: 1788: 1782: 1776: 1764: 1763:External links 1761: 1760: 1759: 1741:(1–4): 27–49. 1730: 1703: 1697: 1676: 1647: 1644: 1641: 1640: 1585: 1562: 1551:. 4 March 2015 1536: 1510: 1493: 1476: 1424: 1410: 1403: 1385: 1353: 1331: 1309: 1276: 1229: 1208: 1183:(4): 380–390. 1163: 1126: 1125: 1123: 1120: 1118: 1115: 1011: 1005: 1001:North Carolina 993:South Carolina 962: 959: 884: 881: 794: 793: 790: 786: 785: 747: 743: 742: 741: 740: 723: 718: 714: 713: 710: 706: 705: 660: 656: 655: 652: 648: 647: 644: 640: 639: 634: 630: 629: 624: 620: 619: 615: 614: 613:ICS Time Scale 611: 607: 606: 599: 598:Regional usage 595: 594: 589: 588:Celestial body 585: 584: 580: 579: 576: 575:Name formality 572: 571: 567: 566: 554: 550: 549: 545: 544: 529: 528: 525: 524: 515: 513: 503: 502: 495: 493: 484: 480: 479: 475: 474: 470: 469: 465: 464: 456: 455: 447: 446: 438: 437: 429: 428: 420: 419: 411: 410: 402: 401: 393: 392: 384: 383: 375: 374: 364: 363: 349: 348: 328: 327: 317: 316: 308: 307: 285: 284: 272: 271: 247: 246: 244: 239: 234: 229: 224: 219: 214: 209: 204: 199: 194: 189: 184: 179: 174: 169: 164: 159: 154: 149: 144: 139: 134: 129: 124: 121: 120: 116: 115: 108: 107: 106: 101: 96: 91: 86: 81: 76: 71: 66: 61: 56: 51: 46: 35: 34: 26: 9: 6: 4: 3: 2: 2610: 2599: 2596: 2594: 2591: 2589: 2586: 2585: 2583: 2570: 2565: 2559: 2554: 2548: 2545: 2540: 2536: 2532: 2527: 2521: 2519: 2512: 2506: 2503: 2501: 2498: 2496: 2493: 2491: 2488: 2487: 2485: 2483: 2476: 2466: 2463: 2461: 2458: 2456: 2453: 2451: 2448: 2447: 2445: 2443: 2436: 2430: 2427: 2425: 2422: 2420: 2417: 2416: 2414: 2412: 2405: 2399: 2396: 2394: 2391: 2389: 2386: 2385: 2383: 2381: 2379:(539 Ma–1 Ga) 2374: 2371: 2369: 2361: 2351: 2348: 2346: 2343: 2341: 2338: 2336: 2333: 2332: 2330: 2328: 2321: 2315: 2312: 2310: 2307: 2305: 2302: 2301: 2299: 2297: 2290: 2284: 2281: 2279: 2276: 2274: 2271: 2269: 2266: 2265: 2263: 2261: 2254: 2248: 2245: 2243: 2240: 2238: 2235: 2234: 2232: 2230: 2223: 2217: 2214: 2212: 2209: 2208: 2206: 2204: 2197: 2191: 2188: 2186: 2183: 2181: 2178: 2177: 2175: 2173: 2166: 2163: 2161: 2156:Paleozoic Era 2153: 2143: 2140: 2138: 2135: 2133: 2130: 2129: 2127: 2125: 2118: 2112: 2109: 2107: 2104: 2102: 2099: 2098: 2096: 2094: 2087: 2081: 2078: 2076: 2073: 2072: 2070: 2068: 2066:(66.0–145 Ma) 2061: 2058: 2056: 2054:(66.0–252 Ma) 2048: 2038: 2035: 2033: 2030: 2028: 2025: 2024: 2022: 2020: 2013: 2007: 2004: 2002: 1999: 1998: 1996: 1994: 1987: 1981: 1978: 1976: 1973: 1972: 1970: 1968: 1961: 1958: 1956: 1948: 1944: 1937: 1932: 1930: 1925: 1923: 1918: 1917: 1914: 1897: 1894: 1892: 1889: 1888: 1886: 1881: 1878: 1876: 1873: 1871: 1868: 1866: 1863: 1861: 1858: 1856: 1853: 1852: 1850: 1849: 1846: 1843: 1841: 1840:Miocene Epoch 1838: 1837: 1832: 1828: 1821: 1816: 1814: 1809: 1807: 1802: 1801: 1798: 1792: 1789: 1786: 1783: 1780: 1777: 1774: 1770: 1767: 1766: 1756: 1752: 1748: 1744: 1740: 1736: 1731: 1726: 1721: 1717: 1713: 1709: 1704: 1700: 1698:0-521-78142-6 1694: 1690: 1686: 1682: 1677: 1672: 1667: 1663: 1659: 1655: 1650: 1649: 1636: 1632: 1627: 1622: 1618: 1614: 1610: 1606: 1605: 1600: 1598: 1589: 1573: 1566: 1550: 1549:New Scientist 1546: 1540: 1525: 1521: 1514: 1507: 1506:0-8493-1632-4 1503: 1497: 1490: 1486: 1480: 1472: 1468: 1463: 1458: 1453: 1448: 1444: 1440: 1436: 1432: 1428: 1417: 1415: 1406: 1400: 1396: 1389: 1370: 1363: 1357: 1341: 1335: 1319: 1313: 1304: 1299: 1295: 1291: 1287: 1280: 1265: 1260: 1256: 1252: 1245: 1238: 1236: 1234: 1225: 1218: 1212: 1198: 1194: 1190: 1186: 1182: 1178: 1174: 1167: 1159: 1155: 1151: 1147: 1143: 1139: 1131: 1127: 1114: 1112: 1108: 1104: 1103: 1098: 1094: 1093:climate shift 1088: 1059: 1055: 1051: 1047: 1043: 1042:Afar Triangle 1039: 1035: 1031: 1030: 1025: 1024: 1019: 1018: 1010: 1004: 1002: 998: 994: 988: 986: 982: 977: 972: 968: 958: 956: 952: 951: 946: 942: 938: 934: 929: 927: 923: 919: 915: 912: 909: 905: 900: 898: 894: 890: 880: 876: 874: 870: 866: 862: 859: 855: 852: 848: 847:Chapadmalalan 844: 840: 835: 833: 830:(part of the 829: 825: 821: 817: 813: 809: 805: 801: 791: 787: 782: 752: 748: 744: 739: 738: 733: 732: 728: 724: 721: 720: 719: 715: 711: 707: 702: 673: 669: 665: 661: 657: 653: 649: 645: 641: 638: 635: 631: 628: 625: 621: 616: 612: 608: 604: 600: 596: 593: 590: 586: 581: 577: 573: 568: 565: 561: 558: 555: 551: 539: 538:, as of 2021. 537: 530: 520: 514: 509: 508: 499: 494: 489: 488: 461: 451: 442: 433: 424: 415: 406: 397: 388: 380: 371: 359: 344: 324: 313: 312: 303: 302: 281: 280: 267: 266: 127: 122: 117: 104: 99: 94: 89: 84: 79: 74: 69: 64: 59: 54: 49: 43: 36: 31: 19: 18:Late Pliocene 2543: 2479:Archean Eon 2441:(1.6–2.5 Ga) 2326:(485–539 Ma) 2295:(444–485 Ma) 2259:(419–444 Ma) 2228:(359–419 Ma) 2202:(299–359 Ma) 2171:(252–299 Ma) 2159:(252–539 Ma) 2123:(201–252 Ma) 2092:(145–201 Ma) 2051:Mesozoic Era 1951:Cenozoic Era 1895: 1870:Serravallian 1772: 1738: 1734: 1718:(2): 82–87. 1715: 1711: 1680: 1664:(2): 88–93. 1661: 1657: 1608: 1602: 1596: 1588: 1576:. Retrieved 1565: 1553:. Retrieved 1539: 1527:. Retrieved 1513: 1496: 1488: 1484: 1479: 1437:(1): 11002. 1434: 1430: 1394: 1388: 1376:. Retrieved 1369:the original 1356: 1344:. Retrieved 1334: 1322:. Retrieved 1312: 1296:(2): 82–87. 1293: 1289: 1279: 1268:. Retrieved 1257:(2): 88–93. 1254: 1250: 1223: 1211: 1200:. Retrieved 1180: 1176: 1166: 1141: 1137: 1130: 1110: 1101: 1084:11.36; 40.86 1056:rivers, in 1048:between the 1038:Homo habilis 1037: 1033: 1029:Homo habilis 1027: 1021: 1015: 1013: 1008: 989: 964: 954: 948: 930: 917: 913: 901: 886: 877: 836: 799: 797: 735: 729: 712:January 1997 533: 449: 414:Serravallian 309: 287: 273: 249: 2515:Hadean Eon 2293:Ordovician 2064:Cretaceous 1964:Quaternary 1860:Burdigalian 1574:. bbc.co.uk 1082: / 1046:Ledi-Geraru 999:and inland 997:Outer Banks 869:New Zealand 832:Pleistocene 776: / 727:Haptophytes 696: / 396:Burdigalian 2588:Piacenzian 2582:Categories 2517:(4–4.6 Ga) 2481:(2.5–4 Ga) 2410:(1–1.6 Ga) 2016:Paleogene 1896:Piacenzian 1855:Aquitanian 1769:Piacenzian 1646:Literature 1483:Gradstein 1270:2024-06-12 1202:2008-02-11 1117:References 937:chronozone 908:planktonic 904:extinction 883:Definition 849:and early 810:or latest 806:the upper 800:Piacenzian 764:14Β°12β€²13β€³E 761:37Β°08β€²49β€³N 684:13Β°29β€²36β€³E 681:37Β°17β€²20β€³N 618:Definition 450:Piacenzian 387:Aquitanian 119:Chronology 33:Piacenzian 2544:See also: 2324:Cambrian 2257:Silurian 2226:Devonian 2121:Triassic 2090:Jurassic 1880:Messinian 1875:Tortonian 971:ice sheet 928:, Italy. 865:Reuverian 841:with the 570:Etymology 432:Messinian 423:Tortonian 2593:Pliocene 2169:Permian 1990:Neogene 1891:Zanclean 1865:Langhian 1775:database 1712:Episodes 1658:Episodes 1635:25739409 1529:22 March 1471:32647351 1378:5 August 1346:5 August 1324:5 August 1290:Episodes 1251:Episodes 939:(at the 897:Piacenza 895:city of 828:Gelasian 824:Zanclean 816:Pliocene 601:Global ( 557:Tertiary 459:Gelasian 441:Zanclean 405:Langhian 378:Chattian 1773:GeoWhen 1771:at the 1743:Bibcode 1613:Bibcode 1604:Science 1578:7 March 1555:7 March 1462:7347535 1439:Bibcode 1197:3515337 1177:PALAIOS 1146:Bibcode 1107:savanna 1102:Science 1097:savanna 1070:40Β°52β€²E 1067:11Β°22β€²N 961:Climate 906:of the 893:Italian 858:Blancan 814:of the 521:expands 519:prairie 511:← 491:← 236:– 226:– 216:– 206:– 196:– 186:– 176:– 166:– 156:– 146:– 136:– 109:↓ 2523:  1695:  1633:  1504:  1491:(1998) 1489:et al. 1485:et al. 1469:  1459:  1401:  1195:  1060:(near 926:Sicily 920:. The 911:forams 851:Uquian 839:coeval 668:Sicily 646:Formal 578:Formal 564:System 560:Period 481:  476:  471:  466:  1372:(PDF) 1365:(PDF) 1247:(PDF) 1220:(PDF) 1193:JSTOR 1122:Notes 1054:Awash 1050:Mille 889:Swiss 808:stage 672:Italy 637:Stage 592:Earth 1693:ISBN 1631:PMID 1597:Homo 1580:2015 1557:2015 1531:2015 1502:ISBN 1467:PMID 1399:ISBN 1380:2016 1348:2016 1326:2016 1111:Homo 1052:and 1036:and 1017:Homo 1009:Homo 953:and 922:GSSP 916:and 798:The 751:Gela 734:and 48:Preκž’ 1751:doi 1720:doi 1685:doi 1666:doi 1621:doi 1609:347 1524:BBC 1457:PMC 1447:doi 1298:doi 1259:doi 1185:doi 1154:doi 1142:142 834:). 812:age 627:Age 603:ICS 536:ICS 2584:: 2539:Ga 2535:Ma 2531:ka 1749:. 1739:27 1737:. 1716:21 1714:. 1710:. 1691:. 1662:21 1660:. 1656:. 1629:. 1619:. 1607:. 1601:. 1547:. 1522:. 1465:. 1455:. 1445:. 1435:10 1433:. 1429:. 1413:^ 1294:21 1292:. 1288:. 1255:21 1253:. 1249:. 1232:^ 1222:. 1191:. 1181:12 1179:. 1175:. 1152:. 1140:. 987:. 957:. 947:: 899:. 820:Ma 670:, 666:, 358:o. 98:Pg 42:Ma 1935:e 1928:t 1921:v 1819:e 1812:t 1805:v 1757:. 1753:: 1745:: 1728:. 1722:: 1701:. 1687:: 1674:. 1668:: 1637:. 1623:: 1615:: 1582:. 1559:. 1533:. 1508:. 1473:. 1449:: 1441:: 1425:2 1407:. 1382:. 1350:. 1328:. 1306:. 1300:: 1273:. 1261:: 1226:. 1205:. 1187:: 1160:. 1156:: 1148:: 605:) 562:/ 369:C 367:P 356:i 354:l 352:P 343:e 341:n 339:e 337:c 335:o 333:i 331:M 322:C 320:O 311:Q 301:e 299:n 297:e 295:g 293:o 291:e 289:N 278:g 276:P 265:c 263:i 261:o 259:z 257:o 255:n 253:e 251:C 103:N 93:K 88:J 83:T 78:P 73:C 68:D 63:S 58:O 53:κž’ 20:)

Index

Late Pliocene
Ma
Preκž’
κž’
O
S
D
C
P
T
J
K
Pg
N
C
e
n
o
z
o
i
c

P
g

N
e
o
g
e
n
e

Q
O
C

M
i
o
c
e
n
e

P
l
i
o.

P
C

Chattian
Aquitanian
Burdigalian
Langhian
Serravallian
Tortonian
Messinian
Zanclean

Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.

↑