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Biber (geology)

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818: 188:
56 to 62, which would place it in the period between 1.6 and 1.8 million years ago, in the latter case it would roughly correspond to MIS 96 to 100, and would therefore have taken place about 2.4 to 2.588 million years ago. The correlation was fraught with problems however due to the fact that the
459:
Kuhlmann, G. (2004), "High resolution stratigraphy and paleoenvironmental changes in the southern North Sea during the Neogene - An integrated study of Late Cenozoic marine deposits from the northern part of the Dutch offshore area. (Thesis Utrecht University)",
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corresponding depositions in the Netherlands were probably not governed by climatic changes. Similar doubts on climatic grounds for the depositions assessed as Biber-related also exist in the Alpine region. It is possible that there were
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Meijer, T.; Cleveringa, P.; Munsterman, D.K.; Verreussel, R.M.C.H. (2006), "The Early Pleistocene Praetiglian and Ludhamian pollen stages in the North Sea Basin and their relationship to the marine isotope record",
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of the western RiĂź-Iller Plateau may also be paralleled with these glacial landforms. The gravels in the Iller-Lech region ascribed to the Biber glaciation are generally heavily weathered and originate from the
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The absolute timing and the connexion with the glacial classification of North Germany and the Netherlands has been problematic. The Biber glacial was thought to correlate either to the
716: 236:(MIS 103 – MIS 64) during Biber. Thus, there have probably been about 20 glacial cycles of varying intensity during Biber. The dominant trigger is believed to be the 41 000 year 544: 686: 142: 400: 520:"Auf den Spuren der Eiszeit im Raum Wangen a. A.: Neue Erkenntnisse auf Grund von bodenkundlichen Untersuchungen im Endmoränengebiet des Rhonegletschers" 269: 197:
of the Alps. The succession and appearance of the gravel bodies makes it possible that during their formation there were several periods of alternating
101:. This corresponded to the Staufenberg Gravel Terrace on the Iller-Lech Plateau, identified in 1974 by Scheunenpflug, and the so-called High Gravels ( 277: 723: 639: 332:
L. Scheunenpflug (1974), "Zur Stratigraphie altpleistozäner Schotter südwestlich bis nordöstlich Augsburg (östliche Iller-Lech-Platte)",
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K.A. Habbe; D. Ellwanger; R. Becker-Haumann (2007), "Stratigraphische Begriffe für das Quartär des süddeutschen Alpenvorlandes",
519: 212:
The 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission firmly places Biber in the
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in the glacial geology of northern Europe. There is continuity between Biber and the glacial cycles of the following
701: 52:
period. Deep sea core samples have identified approximately 20 glacial cycles of varying intensity during Biber.
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Gibbard, P.L.; Cohen, K.M. (2008), "Global stratigraphical correlation table for the last 2.7 Million years",
847: 93:) from gravel landforms of the Stauden Plateau in the area of the Iller-Lech Plateau and in the Aindling 837: 797: 709: 817: 792: 782: 166: 347:
M. Löscher (1976), "Die präwürmzeitliche Schotterablagerungen in der nördlichen Iller-Lech-Platte",
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I. Schaefer (1956), "Sur la division du Quaternaire dans l'avant-pays des Alpes en Allemagne",
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The term Biber glaciation was not part of the traditional four-stage glaciation schema of the
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Geologische Karte von Bayern 1:500000 mit Erläuterungen. 1 Karte + Erläuterungen + 8 Beilagen
205:. The Biber cold period at least corresponds partly with the Swiss cover gravel glaciations ( 474: 485: 392: 233: 185: 622: 445: 149:
in 1953 by Ingo Schaefer, based on the naming system of the traditional Penck schema. Its
8: 658: 237: 489: 760: 501: 158: 775: 584:(in German) (4. ed.), MĂĽnchen: Bayrisches Geologisches Landesamt, pp. 238 ff 138: 36:) is a timespan approximately 2.6–1.8 million years ago in the glacial history of the 842: 807: 765: 627: 505: 281: 731: 750: 654: 617: 607: 493: 440: 396: 221: 194: 770: 320: 198: 70: 29: 755: 170: 134: 321:
German Stratigraphic Commission: Stratigraphische Tabelle von Deutschland 2016
831: 694: 631: 248:
Gravels ascribed to Biber (also called the Highland Gravel or Oldest Gravel (
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Ad-hoc-AG Geologie der Staatlichen Geologischen Dienste (SGD) und der BGR
612: 181: 401:"A Plio-Pleistocene Stack of 57 Globally Distributed Benthic δO Records" 379:
Erläuterungen zur Geologischen Karte von Augsburg und Umgebung, 1:50.000
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Geologica Ultraiectina, Mededelingen van de Faculteit Aardwetenschappen
273: 97:, by grouping together the so-called Middle and Upper Cover Gravels or 49: 377:
I. Schaefer (1957), Bayerisches Geologisches Landesamt MĂĽnchen (ed.),
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complex in the Netherlands. In the former case it would correspond to
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Stratigraphische Tabellen des Bayerischen Geologischen Landesamtes.
640:"Das Quartär in der Stratigraphischen Tabelle von Deutschland 2002" 253: 213: 190: 162: 146: 105:) of the Aindling region. The rich crystalline sedimentary facies ( 41: 579: 285: 217: 123: 264:) and southwest of Augsburg as the Stauden Plateau Gravel ( 130: 37: 165:. The Biber glaciation was thought to be followed by the 109:), that Löscher distinguished in 1976 in the area of the 430: 232:
Deep sea core samples have identified approximately 40
48:, which since 2009 is regarded as the first age of the 600:
Eiszeitalter und Gegenwart Quaternary Science Journal
351:(in German), vol. 45, Heidelberg, pp. 1–157 336:(in German), vol. 40, Heidelberg, pp. 87–94 464:(in German), vol. 245, Utrecht, pp. 1–205 161:and the Staufenberg Gravel Terrace in the area of 122:, by contrast, originates from the bedrock of the 260:), as well as northeast as the Hohenried Gravel ( 829: 331: 216:and gives a correspondence to Pre-Tegelen and 717: 517: 268:). Also included are isolated gravels of the 580:Walter Freudenberger; Klaus Schwerd (1996), 458: 426: 424: 376: 361: 724: 710: 366:(in German), vol. 2, pp. 910–914 346: 316: 314: 312: 696:Stratigraphical charts for the Quaternary 621: 611: 573: 444: 421: 410:(in German), vol. 20, archived from 415:(pdf-Datei; archivierte Version; 1,1 MB) 675:– via Deutsche Quartärvereinigung 637: 309: 830: 364:Actes IV Congres INQUA, Rome/Pise 1953 193:influences perhaps in the wake of the 55: 705: 349:Heidelberger Geographische Arbeiten 334:Heidelberger geographische Arbeiten 284:. There may also be gravels in the 13: 569:Encyclopedia of Quaternary Science 14: 859: 732:The cold and warm periods of the 680: 227: 816: 659:10.1127/0078-0421/2005/0041-0385 207:Deckenschotter-Vergletscherungen 562: 537: 511: 446:10.18814/epiiugs/2008/v31i2/011 623:11858/00-1735-0000-0001-B9FE-0 468: 452: 385: 370: 355: 340: 325: 120:Kristallinreiche Liegendfazies 107:Kristallinreiche Liegendfazies 60:In 1953, Schaefer defined the 1: 638:T. Litt; et al. (2006), 591: 478:Journal of Quaternary Science 303: 243: 647:Newsletters in Stratigraphie 256:as the Stauffenberg Gravel ( 7: 291: 266:Schotter der Stauden-Platte 40:. Biber corresponds to the 10: 864: 141:, but was named after the 814: 741: 167:Biber-Danube interglacial 44:age in the international 527:Jahrbuch des Oberaargaus 288:from the Biber ice age. 250:Ă„ltester Deckenschotter 116:Northern Limestone Alps 518:Ueli Reinmann (2004), 298:Timeline of glaciation 252:) occur northwest of 74: 33: 258:Stauffenberg-Schotter 234:marine isotope stages 736:in the Alpine region 613:10.3285/eg.56.1-2.03 393:Lorraine E. Lisiecki 262:Hohenrieder Schotter 848:Geology of the Alps 490:2006JQS....21..307M 238:Milankovitch cycles 159:Iller-Lech Plateaux 56:History of the term 838:Pleistocene events 825: 824: 808:Last Interglacial 282:Landsberg am Lech 855: 820: 726: 719: 712: 703: 702: 676: 674: 673: 667: 661:, archived from 653:(1–3): 385–399, 644: 634: 625: 615: 586: 585: 577: 571: 566: 560: 559: 557: 556: 547:. Archived from 541: 535: 534: 524: 515: 509: 508: 472: 466: 465: 456: 450: 449: 448: 428: 419: 418: 416: 408:Paleoceanography 405: 397:Maureen E. Raymo 389: 383: 382: 374: 368: 367: 359: 353: 352: 344: 338: 337: 329: 323: 318: 95:terrace sequence 69: 62:Biber glaciation 28: 863: 862: 858: 857: 856: 854: 853: 852: 828: 827: 826: 821: 812: 737: 730: 683: 671: 669: 665: 642: 594: 589: 578: 574: 567: 563: 554: 552: 543: 542: 538: 522: 516: 512: 498:10.1002/jqs.956 473: 469: 457: 453: 429: 422: 414: 403: 390: 386: 375: 371: 360: 356: 345: 341: 330: 326: 319: 310: 306: 294: 246: 240:of axial tilt. 230: 199:fluvial erosion 180:complex or the 155:Stauden Plateau 145:river north of 139:Eduard BrĂĽckner 65: 58: 24: 12: 11: 5: 861: 851: 850: 845: 840: 823: 822: 815: 813: 811: 810: 805: 800: 798:Haslach/Mindel 795: 790: 785: 779: 778: 773: 768: 763: 758: 753: 748: 742: 739: 738: 729: 728: 721: 714: 706: 700: 699: 692: 682: 681:External links 679: 678: 677: 635: 606:(1/2): 66–83, 593: 590: 588: 587: 572: 561: 536: 510: 484:(3): 307–310, 467: 451: 439:(2): 243–247, 420: 384: 369: 354: 339: 324: 307: 305: 302: 301: 300: 293: 290: 245: 242: 229: 228:Glacial cycles 226: 171:Danube glacial 135:Albrecht Penck 99:Deckenschotter 75:Biber-Kaltzeit 57: 54: 9: 6: 4: 3: 2: 860: 849: 846: 844: 841: 839: 836: 835: 833: 819: 809: 806: 804: 801: 799: 796: 794: 791: 789: 786: 784: 781: 780: 777: 774: 772: 769: 767: 764: 762: 759: 757: 754: 752: 749: 747: 744: 743: 740: 735: 727: 722: 720: 715: 713: 708: 707: 704: 698: 697: 693: 690: 689: 685: 684: 668:on 2015-09-23 664: 660: 656: 652: 649:(in German), 648: 641: 636: 633: 629: 624: 619: 614: 609: 605: 602:(in German), 601: 596: 595: 583: 576: 570: 565: 551:on 2019-09-16 550: 546: 540: 532: 529:(in German), 528: 521: 514: 507: 503: 499: 495: 491: 487: 483: 480:(in German), 479: 471: 463: 455: 447: 442: 438: 435:(in German), 434: 427: 425: 417:on 2011-06-16 413: 409: 402: 398: 394: 388: 380: 373: 365: 358: 350: 343: 335: 328: 322: 317: 315: 313: 308: 299: 296: 295: 289: 287: 283: 279: 275: 271: 267: 263: 259: 255: 251: 241: 239: 235: 225: 223: 219: 215: 210: 208: 204: 200: 196: 195:uplift phases 192: 187: 183: 179: 174: 172: 168: 164: 160: 156: 152: 148: 144: 140: 136: 132: 127: 125: 121: 117: 112: 111:Rhine Glacier 108: 104: 103:Hochschottern 100: 96: 92: 91:Biber-Eiszeit 88: 87:Biber Ice Age 84: 83:Biber-Glazial 80: 79:Biber Glacial 76: 72: 68: 63: 53: 51: 47: 46:geochronology 43: 39: 35: 34:Biber-Komplex 31: 27: 22: 21:Biber Complex 18: 793:Gunz/Haslach 783:Biber/Danube 745: 695: 687: 670:, retrieved 663:the original 650: 646: 603: 599: 581: 575: 564: 553:. Retrieved 549:the original 539: 530: 526: 513: 481: 477: 470: 461: 454: 436: 432: 412:the original 407: 387: 378: 372: 363: 357: 348: 342: 333: 327: 278:Stoffersberg 265: 261: 257: 249: 247: 231: 211: 206: 203:accumulation 175: 154: 128: 119: 118:. Löscher's 106: 102: 98: 90: 86: 82: 78: 61: 59: 20: 16: 15: 803:Mindel/Riss 788:Danube/Gunz 545:"Climatica" 381:(in German) 182:Pre-Tiglian 151:type region 832:Categories 734:Quaternary 672:2015-07-24 592:Literature 555:2019-03-20 304:References 274:Mindelheim 244:Occurrence 50:Quaternary 632:0424-7116 533:: 135–152 506:128908646 270:Hochfirst 178:Eburonian 143:Biberbach 67:‹See Tfd› 26:‹See Tfd› 843:Ice ages 433:Episodes 399:(2005), 292:See also 276:and the 254:Augsburg 214:Gelasian 191:tectonic 169:and the 163:Aindling 147:Augsburg 42:Gelasian 761:Haslach 486:Bibcode 286:Sundgau 218:Tegelen 157:in the 153:is the 124:molasse 85:), or 19:or the 766:Mindel 751:Danube 630:  504:  224:stage 222:Danube 126:zone. 71:German 30:German 746:Biber 666:(PDF) 643:(PDF) 523:(PDF) 502:S2CID 404:(PDF) 280:near 272:near 17:Biber 776:WĂĽrm 771:Riss 756:Gunz 628:ISSN 201:and 137:and 131:Alps 38:Alps 655:doi 618:hdl 608:doi 494:doi 441:doi 209:). 186:MIS 133:by 77:), 834:: 651:41 645:, 626:, 616:, 604:56 531:47 525:, 500:, 492:, 482:21 437:31 423:^ 406:, 395:; 311:^ 173:. 73:: 32:: 725:e 718:t 711:v 657:: 620:: 610:: 558:. 496:: 488:: 443:: 89:( 81:( 64:( 23:(

Index

‹See Tfd›
German
Alps
Gelasian
geochronology
Quaternary
‹See Tfd›
German
terrace sequence
Rhine Glacier
Northern Limestone Alps
molasse
Alps
Albrecht Penck
Eduard BrĂĽckner
Biberbach
Augsburg
type region
Iller-Lech Plateaux
Aindling
Biber-Danube interglacial
Danube glacial
Eburonian
Pre-Tiglian
MIS
tectonic
uplift phases
fluvial erosion
accumulation
Gelasian

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