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Gauss–Matuyama reversal

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The propagation of charged particles is dependent in the magnetic field intensity and changes in the dipole moment found in the magnetic field. The ionospheric ionization at the poles and equator reduces the energy on cosmic rays by several orders of magnitude. During the reversal, the dipole field
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sediment are used to date the Gauss–Matuyama reversal. This method is a form of geochronology that measures the amount of photons released from a material after being stimulated. This method primarily observes the movement of U, Th, Rb and K as ionizing radiation. The product of stimulating these
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period, and is often used to date sediments. The reversal is thought to have contributed to a hostile environment on Earth due to the lack of protective features of
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was reduced or entirely canceled because the virtual poles were located at low and intermediate latitudes, which would expose these regions to cosmic rays.
476:"Precessional forcing of lacustrine sedimentation in the late Cenozoic Chemeron Basin, Central Kenya Rift, and calibration of the Gauss/Matuyama boundary" 613: 377:"An attempt to determine the absolute geomagnetic field intensity in Southwestern Iceland during the Gauss–Matuyama reversal" 144: 632: 523:"A detailed record of paleomagnetic field change from Searles Lake, California: 2. The Gauss/Matuyama polarity reversal" 50:
from normal polarity (Gauss Chron) to reverse polarity (Matuyama Chron). The reversal is named after German physicist
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The Gauss–Matuyama reversal is a natural phenomenon that is frequently used as a boundary between the
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Jackman, C. H.; Marsh, D. R.; Kinnison, D. E.; Mertens, C. J.; Fleming, E. L. (2015).
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Suc, Jean-Pierre; Bertini, Adele; Leroy, Suzanne A.G.; Suballyova, Danica (1997).
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Goguitchaichvili, Avto; Prévot, Michel; Thompson, John; Roberts, Neil (1999).
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to shield life from ionizing radiation generated by the early Pleistocene
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Glen, Jonathan M. G.; Coe, Robert S.; Liddicoat, Joseph C. (1999-06-10).
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Deino, A; Kingston, J; Glen, J; Edgar, R; Hill, A (2006).
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Earth's geomagnetic reversal 2.58 million years ago
89:The Gauss–Matuyama reversal is marked by a minor 431:Atmospheric Chemistry & Physics Discussions 115:, and leaving the Earth unshielded for ~15 ky. 243:"From Cosmic Explosions to Terrestrial Fires?" 607: 317:Deschamps, Frédéric; Mottez, Fabrice (2020). 135:elements is a reliable date on the sediment. 8: 527:Journal of Geophysical Research: Solid Earth 381:Physics of the Earth and Planetary Interiors 241:Melott, Adrian L.; Thomas, Brian C. (2019). 614: 600: 546: 450: 258: 181: 7: 568: 566: 420: 418: 370: 368: 312: 310: 236: 234: 232: 480:Earth and Planetary Science Letters 111:generated by the early Pleistocene 25: 69:epochs, marking the start of the 570: 152:of 2.51 ± 0.07 million years ago 1: 401:10.1016/s0031-9201(99)00064-3 215:10.1016/s1040-6182(96)00059-6 586:. You can help Knowledge by 123:Methods for dating reversal 52:Johann Carl Friedrich Gauss 654: 565: 500:10.1016/j.epsl.2006.04.009 452:10.5194/acpd-15-33931-2015 54:and Japanese geophysicist 145:Brunhes–Matuyama reversal 38:event approximately 2.58 195:Quaternary International 492:2006E&PSL.247...41D 95:calcareous nannofossils 32:Gauss–Matuyama Reversal 18:Gauss-Matuyama reversal 323:The Journal of Geology 247:The Journal of Geology 44:Earth's magnetic field 161:Electromagnetic field 633:Geomagnetic reversal 548:10.1029/1999jb900048 48:geomagnetic reversal 539:1999JGR...10412883G 533:(B6): 12883–12894. 443:2015ACPD...1533931J 437:(23): 33931–33966. 393:1999PEPI..115...53G 335:2020JG....128..389D 269:2019JG....127..475M 207:1997QuInt..40...37S 128:Luminescence dating 105:Discoaster surculus 156:Jaramillo reversal 109:ionizing radiation 85:Biological effects 595: 594: 56:Motonori Matuyama 16:(Redirected from 645: 616: 609: 602: 574: 567: 561: 560: 550: 518: 512: 511: 471: 465: 464: 454: 422: 413: 412: 372: 363: 362: 314: 305: 304: 262: 238: 227: 226: 186: 21: 653: 652: 648: 647: 646: 644: 643: 642: 623: 622: 621: 620: 564: 520: 519: 515: 473: 472: 468: 424: 423: 416: 374: 373: 366: 316: 315: 308: 240: 239: 230: 188: 187: 183: 179: 171:Electric charge 166:Field (physics) 141: 125: 91:mass extinction 87: 75:magnetic fields 28: 23: 22: 15: 12: 11: 5: 651: 649: 641: 640: 635: 625: 624: 619: 618: 611: 604: 596: 593: 592: 575: 563: 562: 513: 486:(1–2): 41–60. 466: 414: 364: 343:10.1086/709750 329:(4): 389–391. 306: 277:10.1086/703418 253:(4): 475–481. 228: 180: 178: 175: 174: 173: 168: 163: 158: 153: 150:Eltanin impact 147: 140: 137: 124: 121: 86: 83: 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 650: 639: 638:Geology stubs 636: 634: 631: 630: 628: 617: 612: 610: 605: 603: 598: 597: 591: 589: 585: 582:article is a 581: 576: 573: 569: 558: 554: 549: 544: 540: 536: 532: 528: 524: 517: 514: 509: 505: 501: 497: 493: 489: 485: 481: 477: 470: 467: 462: 458: 453: 448: 444: 440: 436: 432: 428: 421: 419: 415: 410: 406: 402: 398: 394: 390: 386: 382: 378: 371: 369: 365: 360: 356: 352: 348: 344: 340: 336: 332: 328: 324: 320: 313: 311: 307: 302: 298: 294: 290: 286: 282: 278: 274: 270: 266: 261: 256: 252: 248: 244: 237: 235: 233: 229: 224: 220: 216: 212: 208: 204: 200: 196: 192: 185: 182: 176: 172: 169: 167: 164: 162: 159: 157: 154: 151: 148: 146: 143: 142: 138: 136: 133: 129: 122: 120: 116: 114: 110: 106: 102: 101:pentaradiatus 100: 96: 92: 84: 82: 80: 76: 72: 68: 64: 59: 57: 53: 49: 45: 41: 37: 33: 19: 588:expanding it 577: 530: 526: 516: 483: 479: 469: 434: 430: 387:(1): 53–66. 384: 380: 326: 322: 250: 246: 198: 194: 184: 126: 117: 104: 97: 88: 60: 46:underwent a 31: 29: 67:Pleistocene 627:Categories 285:1808/31444 260:1903.01501 177:References 132:lacustrine 99:Discoaster 71:Quaternary 557:0148-0227 508:0012-821X 461:1680-7367 409:0031-9201 359:225043201 351:0022-1376 293:0022-1376 223:1040-6182 201:: 37–42. 113:supernova 79:supernova 42:when the 301:67877046 139:See also 63:Pliocene 36:geologic 580:geology 535:Bibcode 488:Bibcode 439:Bibcode 389:Bibcode 331:Bibcode 265:Bibcode 203:Bibcode 555:  506:  459:  407:  357:  349:  299:  291:  221:  34:was a 578:This 355:S2CID 297:S2CID 255:arXiv 584:stub 553:ISSN 504:ISSN 457:ISSN 405:ISSN 347:ISSN 289:ISSN 219:ISSN 103:and 65:and 30:The 543:doi 531:104 496:doi 484:247 447:doi 397:doi 385:115 339:doi 327:128 281:hdl 273:doi 251:127 211:doi 130:of 93:of 629:: 551:. 541:. 529:. 525:. 502:. 494:. 482:. 478:. 455:. 445:. 435:15 433:. 429:. 417:^ 403:. 395:. 383:. 379:. 367:^ 353:. 345:. 337:. 325:. 321:. 309:^ 295:. 287:. 279:. 271:. 263:. 249:. 245:. 231:^ 217:. 209:. 199:40 197:. 193:. 81:. 58:. 40:Ma 615:e 608:t 601:v 590:. 559:. 545:: 537:: 510:. 498:: 490:: 463:. 449:: 441:: 411:. 399:: 391:: 361:. 341:: 333:: 303:. 283:: 275:: 267:: 257:: 225:. 213:: 205:: 20:)

Index

Gauss-Matuyama reversal
geologic
Ma
Earth's magnetic field
geomagnetic reversal
Johann Carl Friedrich Gauss
Motonori Matuyama
Pliocene
Pleistocene
Quaternary
magnetic fields
supernova
mass extinction
calcareous nannofossils
Discoaster
ionizing radiation
supernova
Luminescence dating
lacustrine
Brunhes–Matuyama reversal
Eltanin impact
Jaramillo reversal
Electromagnetic field
Field (physics)
Electric charge
"Towards the lowering of the Pliocene/Pleistocene boundary to the Gauss-Matuyama reversal"
Bibcode
1997QuInt..40...37S
doi
10.1016/s1040-6182(96)00059-6

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