Knowledge

Compression fossil

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deposits. When excavated the matrix may be split along the natural grain or cleavage of the rock. A fossil embedded in the sediment may then also split down the middle, with fossil remains sticking to both surfaces, or the counter slab may simply show a negative impression or mould of the fossil.
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is not preserved. These fossils may be studied while still partially entombed in the sedimentary rock matrix where they are preserved, or once lifted out of the matrix by a peel or transfer technique.
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and other three-dimensional plant structures do not preserve as well under compression. Typically, only the basic outline and surface features are preserved in compression fossils; internal
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In order to increase their profit, fossil hunters and dealers occasionally sell slab and counter slab separately. A reptile fossil also found in Liaoning was described and named
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A slab and counter slab, more often called a part and counterpart in paleoentomology and paleobotany, are the matching halves of a compression fossil, a fossil-bearing
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sp. nov. (Equisetales) from the Jurassic San Agustin hot spring deposit, Patagonia: Anatomy, paleoecology, and inferred paleoecophysiology"
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a tale of misguided secrecy and misplaced confidence, of rampant egos clashing, self-aggrandizement, wishful thinking, naΓ―ve assumptions,
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to the plane of the deposited sediment. Since leaves are basically flat, the resulting distortion is minimal.
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came into possession of the counter slab through a fossil hunter. On comparing his fossil with images of
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preserved this way. The reason for this is that physical compression of the rock often leads to
334: 169: 160: 552: 400:"New snakeflies (Insecta: Raphidioptera) from the Lower Cretaceous of the UK, Spain and Brazil" 60: 282: 234:, a link between dinosaurs and birds, from a 125 million-year-old fossil that had come from 250:
led to consternation and embarrassment. Lewis Simons investigated the matter on behalf of
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Comparing slab and counter slab has led to the exposure of a number of fossil forgeries.
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Differences between the impressions on slab and counterslab led astronomer
131: 333:(1st ed.). New York & London: McGraw-Hill Book Company. pp.  305:, unaware they were working with the counter slab of the same specimen. 259: 206: 194: 180: 107: 453: 432: 463: 202: 91: 72: 352:(2nd ed.). Cambridge: Cambridge University Press. pp. 7–22. 103: 32: 83: 95: 67:
preserved as good compression fossils, it is very common to find
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it became evident that it was a composite fake. His note to
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Channing, A.; Zamuner, A.; Edwards, D.; Guido, D. (2011).
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Institute of Vertebrate Paleontology and Paleoanthropology
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Jepson, J.E.; Ansorge, J.; Jarzembowski, E.A. (2011).
377:. Englewood Cliffs, NJ: Prentice Hall. pp. 7–12. 544: 102:Compression fossils are formed most commonly in 347: 254:. In October 2000, he reported what he termed: 219:, a claim dismissed by most palaeontologists. 134:may sometimes preserve plant fossils as well. 348:Stewart, Wilson N.; Rothwell, Gar W. (1993). 106:where fine sediment is deposited, such as in 373:Taylor, Thomas N.; Taylor, Edith L. (1993). 372: 424: 341: 375:The Biology and Evolution of Fossil Plants 320: 462: 452: 415: 391: 86:that have been compressed in a direction 178:Slab (left) and counter slab (right) of 146:Counter slab (left) and slab (right) of 141: 26: 350:Paleobotany and the Evolution of Plants 14: 545: 326: 270:had been constructed from parts of an 82:are found preserved in fine layers of 228:magazine announced the discovery of 238:of China. Chinese palaeontologist 24: 266:It was eventually determined that 25: 564: 417:10.1111/j.1475-4983.2011.01038.x 168: 159: 63:. While it is uncommon to find 301:in Beijing described and named 522: 504: 490: 479: 330:An Introduction to Paleobotany 295:Beijing Natural History Museum 222:In its November 1999 edition, 13: 1: 314: 209:in 1985 to declare that some 7: 327:Arnold, Chester A. (1947). 303:Hyphalosaurus lingyuanensis 10: 569: 441:American Journal of Botany 311:is now the accepted name. 137: 297:. In the same year the 264: 205:and applied physicist 152: 44: 534:14 September 2012 at 511:The Interpretive Mind 283:Microraptor zhaoianus 280:and a small dinosaur 256: 145: 35:leaves from the Late 30: 516:1 April 2010 at the 78:The best fossils of 61:physical compression 454:10.3732/ajb.1000211 252:National Geographic 248:National Geographic 225:National Geographic 59:that has undergone 435:Equisetum thermale 153: 49:compression fossil 45: 236:Liaoning Province 215:fossils had been 16:(Redirected from 560: 538: 529:Two Guys Fossils 526: 520: 508: 502: 494: 488: 483: 477: 476: 466: 456: 428: 422: 421: 419: 395: 389: 388: 370: 364: 363: 345: 339: 338: 324: 277:Yanornis martini 272:Early Cretaceous 172: 163: 57:sedimentary rock 39:of northeastern 21: 568: 567: 563: 562: 561: 559: 558: 557: 543: 542: 541: 527: 523: 518:Wayback Machine 509: 505: 495: 491: 484: 480: 429: 425: 396: 392: 385: 371: 367: 360: 346: 342: 325: 321: 317: 293:in 1999 by the 291:Sinohydrosaurus 187: 186: 185: 184: 175: 174: 173: 165: 164: 140: 75:of the fossil. 23: 22: 15: 12: 11: 5: 566: 556: 555: 540: 539: 521: 503: 489: 478: 447:(4): 680–697. 423: 410:(2): 385–395. 390: 383: 365: 358: 340: 318: 316: 313: 177: 176: 167: 166: 158: 157: 156: 155: 154: 139: 136: 9: 6: 4: 3: 2: 565: 554: 553:Fossilization 551: 550: 548: 537: 536:archive.today 533: 530: 525: 519: 515: 512: 507: 501: 500:14 March 1985 499: 498:New Scientist 493: 487: 482: 474: 470: 465: 460: 455: 450: 446: 442: 438: 436: 427: 418: 413: 409: 405: 404:Palaeontology 401: 394: 386: 384:0-13-651589-4 380: 376: 369: 361: 359:0-521-38294-7 355: 351: 344: 336: 332: 331: 323: 319: 312: 310: 309: 308:Hyphalosaurus 304: 300: 296: 292: 287: 285: 284: 279: 278: 273: 269: 268:Archaeoraptor 263: 261: 255: 253: 249: 245: 244:Archaeoraptor 241: 237: 233: 232: 231:Archaeoraptor 227: 226: 220: 218: 214: 213: 212:Archaeopteryx 208: 204: 199: 196: 192: 183: 182: 171: 162: 151: 150: 149:Pterodactylus 144: 135: 133: 129: 125: 121: 117: 113: 109: 105: 100: 97: 93: 89: 88:perpendicular 85: 81: 76: 74: 70: 66: 62: 58: 55:preserved in 54: 50: 42: 38: 37:Carboniferous 34: 29: 19: 18:Slab (fossil) 524: 506: 497: 492: 481: 444: 440: 434: 426: 407: 403: 393: 374: 368: 349: 343: 329: 322: 306: 302: 290: 288: 281: 275: 267: 265: 257: 251: 247: 243: 229: 223: 221: 210: 200: 188: 179: 147: 132:volcanic ash 108:river deltas 104:environments 101: 77: 48: 46: 464:11336/95234 260:human error 207:Lee Spetner 195:sedimentary 181:Longipteryx 130:, although 92:Plant stems 315:References 203:Fred Hoyle 193:formed in 73:distortion 118:, and in 33:seed fern 547:Category 532:Archived 514:Archived 473:21613167 114:, along 84:sediment 240:Xu Xing 112:lagoons 96:anatomy 65:animals 31:Fossil 471:  381:  356:  217:forged 191:matrix 116:rivers 80:leaves 69:plants 53:fossil 274:bird 138:Slabs 128:shale 120:ponds 51:is a 486:ProZ 469:PMID 379:ISBN 354:ISBN 337:–40. 126:and 124:clay 41:Ohio 459:hdl 449:doi 412:doi 549:: 467:. 457:. 445:98 443:. 439:. 408:54 406:. 402:. 335:14 286:. 110:, 47:A 475:. 461:: 451:: 433:" 420:. 414:: 387:. 362:. 43:. 20:)

Index

Slab (fossil)

seed fern
Carboniferous
Ohio
fossil
sedimentary rock
physical compression
animals
plants
distortion
leaves
sediment
perpendicular
Plant stems
anatomy
environments
river deltas
lagoons
rivers
ponds
clay
shale
volcanic ash

Pterodactylus


Longipteryx
matrix

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