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Campur Formation

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in an open shelf system. The lower boundary of the Campur Formation is transitional into the underlying
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and limestones occur in the formation. The formation was probably deposited in a fore-
320: 382: 336: 317: 91: 150: 301: 224: 627: 172: 159: 133: 120: 32: 24: 381:. The Campur Formation is laterally equivalent with the upper part of the 597: 538: 522: 467: 359: 344: 309: 305: 214: 99: 81: 28: 348: 313: 340: 393:
The following fossils have been uncovered from the formation:
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List of fossiliferous stratigraphic units in Guatemala
571: 625: 473: 503: 553: 544: 482: 575:EvaluaciĂłn hidrogeolĂłgica de Alta Verapaz 664:Geography of the Alta Verapaz Department 274: 606:Revista Mexicana de Ciencias GeolĂłgicas 626: 583:Universidad de San Carlos de Guatemala 595: 373:. The formation is overlain by the 13: 14: 680: 598:"Cretaceous rudists of Guatemala" 572:Machorro Sagastume, Rudy (2005), 388: 273: 266: 207: 565: 528: 512: 491: 479:Machorro Sagastume, 2005, p.11 457: 326: 1: 509:Machorro Sagastume, 2005, p.9 451: 282:Campur Formation (Guatemala) 151:Approximate paleocoordinates 7: 439: 339:. The formation is rich in 10: 685: 331:The formation consists of 261: 253: 245: 235: 230: 220: 202: 188: 149: 110: 105: 87: 77: 72: 62: 48: 38: 23: 18: 419:Distefanella lombricalis 333:fossiliferous limestones 659:Shallow marine deposits 654:Conglomerate formations 406:Bournonia cardenasensis 399:Accordiella cf. conica 385:of western Guatemala. 426:Senalveolina aubouini 335:with minor levels of 644:Limestone formations 639:Cretaceous Guatemala 634:Geology of Guatemala 596:Scott, R.W. (1995), 649:Dolomite formations 316:dating back to the 169: /  130: /  25:Stratigraphic range 559:Scott, 1995, p.304 550:Scott, 1995, p.303 488:Scott, 1995, p.297 433:Sulcoperculina sp. 298:geologic formation 290: 289: 676: 669:PetĂ©n Department 620: 619: 618: 602: 592: 591: 590: 580: 560: 557: 551: 548: 542: 532: 526: 516: 510: 507: 501: 495: 489: 486: 480: 477: 471: 464:Campur Formation 461: 294:Campur Formation 277: 276: 270: 213: 211: 210: 184: 183: 181: 180: 179: 174: 170: 167: 166: 165: 162: 145: 144: 142: 141: 140: 135: 131: 128: 127: 126: 123: 19:Campur Formation 16: 15: 684: 683: 679: 678: 677: 675: 674: 673: 624: 623: 616: 614: 600: 588: 586: 585:, pp. 1–77 578: 568: 563: 558: 554: 549: 545: 533: 529: 517: 513: 508: 504: 496: 492: 487: 483: 478: 474: 462: 458: 454: 442: 391: 383:Ixcoy Formation 375:Sepur Formation 371:Cobán Formation 329: 318:Late Cretaceous 308:. The subtidal 286: 285: 284: 283: 280: 279: 278: 208: 206: 177: 175: 171: 168: 163: 160: 158: 156: 155: 138: 136: 132: 129: 124: 121: 119: 117: 116: 67:Cobán Formation 57:Sepur Formation 12: 11: 5: 682: 672: 671: 666: 661: 656: 651: 646: 641: 636: 622: 621: 593: 567: 564: 562: 561: 552: 543: 527: 511: 502: 490: 481: 472: 455: 453: 450: 449: 448: 441: 438: 437: 436: 429: 422: 415: 402: 390: 389:Fossil content 387: 328: 325: 288: 287: 281: 272: 271: 265: 264: 263: 262: 259: 258: 255: 251: 250: 247: 243: 242: 237: 233: 232: 228: 227: 222: 218: 217: 204: 200: 199: 190: 186: 185: 153: 147: 146: 114: 108: 107: 103: 102: 89: 85: 84: 79: 75: 74: 70: 69: 64: 60: 59: 50: 46: 45: 40: 36: 35: 21: 20: 9: 6: 4: 3: 2: 681: 670: 667: 665: 662: 660: 657: 655: 652: 650: 647: 645: 642: 640: 637: 635: 632: 631: 629: 612: 608: 607: 599: 594: 584: 577: 576: 570: 569: 556: 547: 540: 536: 531: 524: 520: 515: 506: 499: 494: 485: 476: 469: 465: 460: 456: 447: 444: 443: 435: 434: 430: 428: 427: 423: 421: 420: 416: 414: 413: 408: 407: 403: 401: 400: 396: 395: 394: 386: 384: 380: 376: 372: 368: 365: 361: 357: 356:conglomerates 354: 350: 346: 342: 338: 334: 324: 322: 319: 315: 311: 307: 303: 299: 295: 269: 260: 256: 252: 248: 244: 241: 238: 234: 229: 226: 223: 219: 216: 205: 201: 198: 194: 191: 187: 182: 173:24.2°N 80.1°W 154: 152: 148: 143: 134:16.0°N 90.5°W 115: 113: 109: 104: 101: 97: 93: 90: 86: 83: 80: 76: 71: 68: 65: 61: 58: 54: 51: 47: 44: 41: 37: 34: 33:Maastrichtian 30: 26: 22: 17: 615:, retrieved 610: 604: 587:, retrieved 574: 566:Bibliography 555: 546: 530: 514: 505: 498:Cuenca PetĂ©n 493: 484: 475: 459: 431: 424: 417: 410: 404: 397: 392: 330: 304:of northern 293: 291: 254:Year defined 231:Type section 193:Alta Verapaz 96:conglomerate 539:Fossilworks 523:Fossilworks 468:Fossilworks 412:B. excavata 379:PetĂ©n Group 367:environment 327:Description 302:PetĂ©n Basin 296:(Kca) is a 225:PetĂ©n Basin 178:24.2; -80.1 176: / 139:16.0; -90.5 137: / 112:Coordinates 53:PetĂ©n Group 628:Categories 617:2019-02-05 589:2019-02-05 535:Rubelsanto 452:References 360:siltstones 312:preserves 613:: 294–306 345:miliolids 337:dolomites 310:limestone 306:Guatemala 236:Named for 215:Guatemala 100:siltstone 82:Limestone 73:Lithology 49:Underlies 43:Formation 519:El Ceibo 440:See also 349:Breccias 246:Named by 106:Location 92:Dolomite 63:Overlies 29:Turonian 377:of the 341:rudists 314:fossils 300:of the 203:Country 164:80°06′W 161:24°12′N 125:90°30′W 122:16°00′N 78:Primary 353:clayey 321:period 249:Vinson 240:Campur 221:Extent 212:  189:Region 601:(PDF) 579:(PDF) 500:- MEM 197:PetĂ©n 88:Other 541:.org 525:.org 470:.org 364:reef 351:and 343:and 292:The 257:1962 39:Type 537:at 521:at 466:at 630:: 611:12 609:, 603:, 581:, 409:, 358:, 347:. 323:. 195:, 98:, 94:, 55:: 27:: 31:-

Index

Stratigraphic range
Turonian
Maastrichtian
Formation
Petén Group
Sepur Formation
Cobán Formation
Limestone
Dolomite
conglomerate
siltstone
Coordinates
16°00′N 90°30′W / 16.0°N 90.5°W / 16.0; -90.5
Approximate paleocoordinates
24°12′N 80°06′W / 24.2°N 80.1°W / 24.2; -80.1
Alta Verapaz
Petén
Guatemala
Petén Basin
Campur
Campur Formation is located in Guatemala
geologic formation
Petén Basin
Guatemala
limestone
fossils
Late Cretaceous
period
fossiliferous limestones
dolomites

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