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Alvarez hypothesis

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237:, oscillating movements of water in lakes, bays, or gulfs, that would have reached the site in North Dakota within minutes or hours of the impact. This would have led to the rapid burial of organisms under a thick layer of sediment. Coauthor David Burnham of the University of Kansas was quoted as saying "They’re not crushed, it’s like an avalanche that collapses almost like a liquid, then sets like concrete. They were killed pretty suddenly because of the violence of that water. We have one fish that hit a tree and was broken in half." 268: 1415: 187: 1421: 20: 324:
the scientists themselves. Verbal accusations have been thrown both by and toward many prominent researchers including Gerta Keller and Luis Alvarez, discouraging civil debate and in some cases threatening careers. Walter Alvarez is an active member of the UC Berkeley team researching the connection between Deccan volcanism and the Chicxulub impact.
97:, as being the cause of the extinction. A team of 41 scientists reviewed 20 years of scientific literature and in so doing also ruled out other theories such as massive volcanism. They had determined that a space rock 10–15 km (6–9 mi) in diameter hurtled into earth at Chicxulub. For comparison, the Martian moon 355:
by immense pressure from its usual state into its present form in just minutes; the fact that the peak ring was made of granite was also significant, since granite is not a rock found in sea-floor deposits, it originates much deeper in the Earth and had been ejected to the surface by the immense pressures of impact; that
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A 2016 drilling project into the peak ring of the crater strongly supported the hypothesis, and confirmed various matters that had been unclear until that point. These included the fact that the peak ring comprised granite (a rock found deep within the Earth) rather than typical sea floor rock, which
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from the mid-crust deep within the Earth, to create colossal water movements, and to eject an immense quantity of vaporized rock and sulfates into the atmosphere, where they would have persisted for a long time. This global dispersal of dust and sulfates would have led to a sudden and catastrophic
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samples from the impact itself. The discoveries were widely seen as confirming current theories related to both the crater impact, and its effects. They confirmed that the rock composing the peak ring had been subjected to immense pressures and forces and had been melted by immense heat and shocked
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Debate regarding the cause of the K-Pg extinction has proven to be extremely controversial among researchers, and the resilience of its intensity has earned it the moniker of the "dinosaur wars." Criticism is unusually harsh, targeting not only research findings but the credibility and integrity of
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to more accurately identify the eruptions as occurring both within a span of one million years and around 250,000 years prior to the K-Pg boundary. Keller additionally determined that ocean temperatures rose seven to nine degrees Celsius during the most significant period of the Deccan eruptions.
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spanning ~1.3 million square kilometers that were created by massive volcanic activity during the same time period in which the Chicxulub impact occurred. Prior to Keller's research, the timeframe of the Deccan Traps' eruptions had a significantly large range of error, making it difficult to draw
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strong enough to initiate volcanic eruptions. They determined that the largest period of Deccan volcanic eruptions, or the Wai subgroup, occurred 50,000 to 100,000 years after the Chixculub impact, which is consistent with theoretical predictions modeling the length of time after which eruptions
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Keller has specifically rejected the Alvarez hypothesis, pointing to evidence she gathered from the Chicxulub crater in 2009 revealing that twenty inches of sediment separates the impact from the extinction. The finding suggests that the impact occurred 200,000 to 300,000 years before the K-Pg
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led by Paul Renne and Mark Richards. This theory proposes that the impact itself instigated the most intense period of Deccan eruptions, both of which had devastating effects contributing to the K-Pg extinction. Renne and Richards calculated that the Chixculub impact was capable of producing
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found on the site and were also embedded in the gills of about 50 percent of the fossil fish. They were also able to find traces of iridium. The authors – who include Walter Alvarez – postulate that shock of the impact, equivalent to an earthquake of magnitude 10 or 11, may have led to
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should occur. The group also confirmed that the length of time between the extinction and subsequent biological recovery was consistent with the length of Deccan volcanic activity, proposing that the eruptions paused the recovery of the marine ecosystems destroyed by the impact.
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Previously, in a 1953 publication, geologists Allan O. Kelly and Frank Dachille analyzed global geological evidence suggesting that one or more giant asteroids impacted the Earth, causing an angular shift in its axis, global floods, firestorms, atmospheric occlusion, and the
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in 2015, as well the more recent assertion that a tsunami generated by the impact created the unusual sediment layer. Keller additionally claims that the impact did not cause as much ecological damage as is widely believed, and she determined that many
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Renne, Paul R.; Deino, Alan L.; Hilgen, Frederik J.; Kuiper, Klaudia F.; Mark, Darren F.; Mitchell, William S.; Morgan, Leah E.; Mundil, Roland; Smit, Jan (7 February 2013). "Time Scales of Critical Events Around the Cretaceous-Paleogene Boundary".
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species began to decline well before the impact event occurred. Her 2009 project revealed that the 52 species found in the sediment prior to the impact were present in the sediment following it, suggesting that the impact caused minimal extinction.
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that declared that the extinction of the dinosaurs was caused by Chicxulub was co-authored by 41 scientists, dozens of other scientists challenged both the paper's methods and its conclusions. A leading critic of the Alvarez hypothesis is
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volcanism as a likely cause of a more gradual extinction. Despite the fact that the Alvarez hypothesis has overwhelming support from the scientific community, Keller has continued to advocate for research into alternate theories.
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usually present in the shallow seabed of the region, had been almost entirely removed and must therefore have been almost entirely vaporized and entered the atmosphere, and that the event was immediately followed by a huge
70:. Prior to 2013, it was commonly cited as having happened about 65 million years ago, but Renne and colleagues (2013) gave an updated value of 66 million years. Evidence indicates that the asteroid fell in the 113:
had been shocked, melted, and ejected to the surface in minutes, and evidence of colossal seawater movement directly afterwards from sand deposits. Crucially, the cores also showed a near-complete absence of
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According to a high-resolution study of fossilized fish bones published in 2022, the Cretaceous-Paleogene asteroid which caused mass extinction impacted during the Northern Hemisphere spring.
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has a diameter of 22 km (14 mi), and Mount Everest is just under 9 km (5.6 mi). The collision would have released the same energy as 100,000,000 megatonnes of TNT (4.2
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Richards, Mark A.; Alvarez, Walter; Self, Stephen; Karlstrom, Leif; Renne, Paul R.; Manga, Michael; Sprain, Courtney J.; Smit, Jan; Vanderkluysen, LoĂżc; Gibson, Sally A. (2015-04-30).
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that the authors say provides a "postimpact snapshot" of events after the asteroid collision "including ejecta accretion and faunal mass death". The team found that the
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Schoene, Blair; Samperton, Kyle M.; Eddy, Michael P.; Keller, Gerta; Adatte, Thierry; Bowring, Samuel A.; Khadri, Syed F. R.; Gertsch, Brian (2015-01-09).
1318: 1268: 909: 293:, ozone reduction, acid rain, and a release of harmful gases, she asserts that these conditions were sufficient to have initiated the mass extinction. 793: 275:
The Deccan Traps theory was first proposed in 1978 by geologist Dewey McLean but quickly lost traction. The Deccan Traps are an area of volcanic
372:(a massive movement of sea waters) sufficient to lay down the largest known layer of sand separated by grain size directly above the peak ring. 640: 819: 1374: 284:
strong conclusions regarding their connection to the K-Pg extinction. In a 2014 report, Keller and her colleagues used uranium-lead zircon
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These strongly support the hypothesis that the impactor was large enough to create a 120-mile peak ring, to melt, shock and eject
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extinction, a period far too large for the two to be correlated. This, however, contrasts the range of 33,000 years determined by
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Alvarez, L.W.; Alvarez, W.; Asaro, F.; Michel, H. V. (1980). "Extraterrestrial cause for the Cretaceous–Tertiary extinction".
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The location of the impact was unknown when the Alvarez team developed their hypothesis, but later scientists discovered the
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Renne, Paul R.; Sprain, Courtney J.; Richards, Mark A.; Self, Stephen; Vanderkluysen, LoĂżc; Pande, Kanchan (2015-10-02).
86:, who first suggested it in 1980. Shortly afterwards, and independently, the same was suggested by Dutch paleontologist 1399: 1359: 1327: 1304: 1283: 311: 167:. There were other earlier speculations on the possibility of an impact event, but without strong confirming evidence. 707: 1681: 148: 31: 209:
has reported that the date of the asteroid event is 66,038,000 years ago, plus or minus 11,000 years, based on
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A more recent theory combining both Deccan volcanism and the impact hypothesis has been developed by teams at
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In March 2010, an international panel of scientists endorsed the asteroid hypothesis, specifically the
213:. He further posits that the mass extinction of dinosaurs occurred within 33,000 years of this date. 1897: 1625: 1460: 87: 586: 1814: 1565: 1435: 1215:"State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact" 1731: 1600: 1530: 1570: 1834: 1711: 1575: 1490: 581: 106: 1855: 1839: 1787: 1505: 1226: 1140: 1050: 1039:"U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction" 861: 746: 573: 519: 467: 410: 180: 71: 8: 1882: 1440: 290: 221: 144: 132: 79: 23: 1230: 1144: 1054: 865: 750: 577: 523: 503:"The Chicxulub Asteroid Impact and Mass Extinction at the Cretaceous-Paleogene Boundary" 471: 414: 1751: 1011:"New, tighter timeline confirms ancient volcanism aligned with dinosaurs' extinction". 905: 887: 769: 734: 688: 634: 607: 543: 502: 483: 434: 271:
The Western Ghats, a province within the Deccan Traps that has been thoroughly studied.
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effect on the climate worldwide, large temperature drops, and devastated the
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10 J), over a billion times the energy of the atomic bombs dropped on
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De Laubenfels, M. W. (1956). "Dinosaur Extinctions: One More Hypothesis".
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Asteroid impact hypothesis as cause of the Cretaceous–Paleogene extinction
1595: 1500: 1414: 369: 267: 140: 1761: 1661: 692: 381: 298: 202: 191: 78:. The hypothesis is named after the father-and-son team of scientists 1726: 1721: 1706: 1152: 479: 351: 343: 147:, discovered that sedimentary layers found all over the world at the 1184:"Did dinosaur-killing asteroid trigger largest lava flows on Earth?" 1129:"Triggering of the largest Deccan eruptions by the Chicxulub impact" 131:
In 1980, a team of researchers led by Nobel prize-winning physicist
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In 2016, a scientific drilling project drilled deep into the
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Target: Earth – The Role of Large Meteors In Earth Science
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Timeline of Cretaceous–Paleogene extinction event research
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(1 April 2019). 1869: 1326: 1312: 678: 624: 451: 198:where erosion has exposed the K–Pg boundary. 982: 898: 655:"Early Ideas About Impacts and Extinctions" 228:that had peppered the area were present in 1319: 1305: 639:: CS1 maint: location missing publisher ( 904: 873: 768: 758: 585: 559: 557: 183:, now considered the likely impact site. 732: 393: 266: 216:In April 2019, a paper was published in 185: 54:and many other living things during the 18: 705: 159:hundreds of times greater than normal. 1870: 1133:Geological Society of America Bulletin 1094: 953:"What Caused the Dinosaur Extinction?" 950: 845: 726: 554: 328:2016 Chicxulub crater drilling project 1300: 1281: 1208: 1206: 1204: 1178: 1176: 1174: 1172: 1170: 1122: 1120: 1118: 1116: 1090: 1088: 1032: 1030: 1028: 1026: 1006: 1004: 978: 976: 974: 972: 946: 944: 942: 940: 938: 936: 934: 932: 338:Cretaceous–Paleogene extinction event 56:Cretaceous–Paleogene extinction event 452:Smit, J; Hertogen, J (22 May 1980). 708:"Dinosaur extinction battle flares" 625:Kelly, A. O.; Dachille, F. (1953). 248:Although a 2010 paper published in 13: 1201: 1167: 1113: 1085: 1023: 1001: 969: 929: 14: 1909: 1282:Fleur, Nicholas St (2016-11-17). 951:Bosker, Bianca (September 2018). 501:Schulte, P.; et al. (2010). 1419: 1413: 1275: 1261: 839: 812: 791: 785: 706:Perlman, D. (8 February 2013). 699: 672: 647: 618: 494: 445: 220:which describes evidence from 1: 1893:Cretaceous–Paleogene boundary 1850:Lunar and Planetary Institute 1682:Cretaceous–Paleogene boundary 596:10.1126/science.208.4448.1095 387: 222:a fossil site in North Dakota 207:Berkeley Geochronology Center 149:Cretaceous–Paleogene boundary 846:Barras, Colin (2022-02-23). 243: 7: 1878:Late Cretaceous extinctions 1742:Planar deformation features 1095:Patton, Paul (2014-10-23). 983:O'Neill, Ian (2009-04-27). 170: 165:extinction of the dinosaurs 10: 1914: 1888:Hypothetical impact events 1845:Impact Field Studies Group 875:10.1038/d41586-022-00511-x 331: 124: 120: 1780: 1649: 1428: 1411: 1352: 1334: 1328:Impact cratering on Earth 1815:William Kenneth Hartmann 1481:Clearwater East and West 1429:Confirmed≥20 km diameter 1732:Ordovician meteor event 1239:10.1126/science.aac7549 1063:10.1126/science.aaa0118 760:10.1073/pnas.1817407116 681:Journal of Paleontology 629:. Carlsbad, California. 532:10.1126/science.1177265 423:10.1126/science.1230492 348:Chicxulub impact crater 1835:Eugene Merle Shoemaker 1712:Late Heavy Bombardment 363:-containing rock that 272: 199: 107:Hiroshima and Nagasaki 39: 1856:Traces of Catastrophe 1840:Earth Impact Database 1788:Ralph Belknap Baldwin 270: 259:, who has focused on 189: 135:, his son, geologist 22: 1139:(11–12): 1507–1520. 1013:Science and Children 908:(23 February 2022). 26:, left, and his son 1231:2015Sci...350...76R 1145:2015GSAB..127.1507R 1055:2015Sci...347..182S 906:Ouellette, Jennifer 866:2022Natur.603...17B 751:2019PNAS..116.8190D 578:1980Sci...208.1095A 572:(4448): 1095–1108. 524:2010Sci...327.1214S 518:(5970): 1214–1218. 472:1980Natur.285..198S 415:2013Sci...339..684R 291:ocean acidification 145:Helen Vaughn Michel 24:Luis Walter Alvarez 1752:Shock metamorphism 1657:Alvarez hypothesis 1288:The New York Times 800:. LABX media group 273: 200: 58:was caused by the 44:Alvarez hypothesis 40: 1865: 1864: 1805:Edward C. T. Chao 1049:(6218): 182–184. 798:the scientist.com 745:(17): 8190–8199. 466:(5762): 198–200. 409:(6120): 684–687. 181:Yucatán Peninsula 72:Yucatán Peninsula 50:of the non-avian 1905: 1898:1980s in science 1830:Peter H. Schultz 1793:Daniel Barringer 1702:Impact structure 1423: 1417: 1321: 1314: 1307: 1298: 1297: 1292: 1291: 1279: 1273: 1272: 1265: 1259: 1258: 1210: 1199: 1198: 1196: 1195: 1180: 1165: 1164: 1153:10.1130/b31167.1 1124: 1111: 1110: 1108: 1107: 1092: 1083: 1082: 1034: 1021: 1020: 1008: 999: 998: 996: 995: 980: 967: 966: 964: 963: 948: 927: 926: 924: 922: 902: 896: 895: 877: 843: 837: 836: 834: 833: 816: 810: 809: 807: 805: 789: 783: 782: 772: 762: 730: 724: 723: 721: 720: 703: 697: 696: 676: 670: 669: 667: 666: 657:. 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Dietz 1798:Barringer Medal 1776: 1687:Cryptoexplosion 1645: 1576:Puchezh-Katunki 1556:Nördlinger Ries 1424: 1418: 1409: 1375:Asia and Russia 1348: 1330: 1325: 1295: 1280: 1276: 1267: 1266: 1262: 1225:(6256): 76–78. 1211: 1202: 1193: 1191: 1182: 1181: 1168: 1125: 1114: 1105: 1103: 1093: 1086: 1035: 1024: 1010: 1009: 1002: 993: 991: 981: 970: 961: 959: 949: 930: 920: 918: 903: 899: 844: 840: 831: 829: 818: 817: 813: 803: 801: 790: 786: 731: 727: 718: 716: 704: 700: 677: 673: 664: 662: 653: 652: 648: 632: 631: 623: 619: 587:10.1.1.126.8496 562: 555: 505: 499: 495: 450: 446: 398: 394: 390: 340: 332:Main articles: 330: 246: 173: 139:, and chemists 129: 123: 102: 48:mass extinction 17: 12: 11: 5: 1911: 1901: 1900: 1895: 1890: 1885: 1880: 1863: 1862: 1860: 1859: 1852: 1847: 1842: 1837: 1832: 1827: 1822: 1817: 1812: 1807: 1802: 1801: 1800: 1790: 1784: 1782: 1778: 1777: 1775: 1774: 1769: 1764: 1759: 1757:Shocked quartz 1754: 1749: 1744: 1739: 1734: 1729: 1724: 1719: 1717:Lechatelierite 1714: 1709: 1704: 1699: 1694: 1692:Ejecta blanket 1689: 1684: 1679: 1677:Complex crater 1674: 1669: 1664: 1659: 1653: 1651: 1647: 1646: 1644: 1643: 1638: 1633: 1628: 1623: 1618: 1613: 1608: 1603: 1598: 1593: 1588: 1583: 1578: 1573: 1568: 1563: 1558: 1553: 1548: 1543: 1538: 1533: 1528: 1523: 1518: 1513: 1508: 1503: 1498: 1493: 1488: 1483: 1478: 1473: 1471:Chesapeake Bay 1468: 1463: 1458: 1453: 1448: 1443: 1438: 1432: 1430: 1426: 1425: 1412: 1410: 1408: 1407: 1402: 1397: 1392: 1387: 1382: 1377: 1372: 1367: 1362: 1356: 1354: 1350: 1349: 1347: 1346: 1341: 1335: 1332: 1331: 1324: 1323: 1316: 1309: 1301: 1294: 1293: 1274: 1260: 1200: 1166: 1112: 1101:Universe Today 1084: 1022: 1000: 989:Universe Today 968: 928: 897: 838: 811: 792:Hou, Chia-Yi. 784: 725: 698: 687:(1): 207–218. 671: 646: 617: 553: 493: 444: 391: 389: 386: 329: 326: 245: 242: 190:Badlands near 172: 169: 137:Walter Alvarez 125:Main article: 122: 119: 84:Walter Alvarez 15: 9: 6: 4: 3: 2: 1910: 1899: 1896: 1894: 1891: 1889: 1886: 1884: 1881: 1879: 1876: 1875: 1873: 1858: 1857: 1853: 1851: 1848: 1846: 1843: 1841: 1838: 1836: 1833: 1831: 1828: 1826: 1823: 1821: 1820:H. 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Index


Luis Walter Alvarez
Walter
K–T Boundary
Gubbio
mass extinction
dinosaurs
Cretaceous–Paleogene extinction event
impact
asteroid
Earth
Yucatán Peninsula
Mexico
Luis
Walter Alvarez
Jan Smit
Chicxulub impact
Phobos
Hiroshima and Nagasaki
gypsum
Timeline of Cretaceous–Paleogene extinction event research
Luis Alvarez
Walter Alvarez
Frank Asaro
Helen Vaughn Michel
Cretaceous–Paleogene boundary
concentration
iridium
extinction of the dinosaurs
Chicxulub Crater

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