300:
341:
206:
647:
635:
623:
25:
611:
683:
671:
659:
348:
472:
The dalle is thought to have been partially unearthed for the first time in June 1941, during road works on what is now the D 900A. In 1979, before the establishment of the Géologique de Haute-Provence
National Nature Reserve, earthworks began to uncover the slab and unearthed 600 ammonites over 160
476:
Until 1994 only 200 square metres (2,200 sq ft) were visible. After this date, the Géologique de Haute-Provence
National Nature Reserve took the task of clearing an additional 150 square metres (1,600 sq ft) to attain a total area of 350 square metres (3,800 sq ft).
571:
process. The good conservation of the shells give informations over the marine dynamism responsible for the deposit conditions : an hectic environment, like a beach or a coast, were the waves actions were strongly felt, with a tendency to break the shells, leading to fragmentary deposits,
559:. The Dalle à ammonites, as well as other sites in the area, are witnesses of the first step of this process, and of what was life in this ocean before the apparition of the mountains. They bring paleontological context for the understanding of paleoenvironments and period conditions.
595:
analysis, as well as the position of the shells, lead to the conclusion that the Dalle à ammonites was an accumulation facies : a large number of dead animals were carried by weak marine currents, towards their deposit site. Traces of
584:. The majority of the fossils on the slab are still almost complete, which lead to the hypothesis of a milder environment, deeper, and better preserved. Moreover, this deposit was effected over the
761:
394:
781:
756:
732:
480:
The 160 square metres (1,700 sq ft) already unearthed in 1992 of the slab were molded in 1992 by the geological reserve for the city of
766:
42:
340:
262:
89:
108:
61:
791:
305:
786:
68:
46:
484:
in Japan (who desired to buy the original). The mold was realized in 30 parts, which were sent and reassembled in Japan.
585:
255:
75:
57:
35:
729:
771:
634:
622:
445:
The deposit thickness is estimated to be 20 centimetres (7.9 in), deposited over a 100,000-year period.
378:
457:, who prospected the area in the middle of the 19th century, doesn't mention it. Geologists studying the
646:
610:
730:
Livret-Guide d'excursion géologique, congrès de l'Association des paléontologues français, 3–5 Mai 2007
205:
82:
776:
454:
592:
381:) is a remarkable natural site consisting of a rock strata bearing a large number of fossilized
514:
541:
geological facies. It bears the traces of the oceanisation preceding the orogeny beginning.
434:
736:
682:
670:
658:
574:
386:
374:
211:
530:
419:
401:
750:
707:
568:
164:
129:
597:
556:
741:
538:
458:
410:
222:
139:
24:
742:
Ammonites: 1,553 photographies d'ammonites, un projet artistique d'Oscar Molina
580:
549:
498:
415:
184:
149:
277:
264:
429:
425:
385:. This site is located approximately 1.5 kilometres (0.93 mi) south of
189:
506:
502:
481:
462:
422:). Those ammonites can attain a diameter of 70 centimetres (28 in).
405:
382:
328:
179:
174:
159:
154:
144:
601:
534:
510:
466:
439:
194:
169:
390:
453:
As well known as it is, the slab wasn't known until recently :
404:, inclined at 60°, is made of grey limestone. It bears around 1,500
553:
545:
518:
18:
604:
fauna, such as scavenger worms, who thrived in this biotope.
724:
461:
remains near the site only mentions numerous species of
533:. The Dignes-les-Bains area is located in the French
395:
Géologique de Haute-Provence
National Nature Reserve
324:
319:
311:
293:
254:
249:
241:
236:
228:
218:
123:
49:. Unsourced material may be challenged and removed.
762:Tourist attractions in Alpes-de-Haute-Provence
529:The Dalle à ammonites was created during the
8:
782:Fossiliferous stratigraphic units of Europe
567:The fossils aspect helps to understand the
204:
120:
347:
109:Learn how and when to remove this message
548:were erected in several phases, after a
408:, 90% of which belonging to the species
699:
606:
473:square metres (1,700 sq ft).
7:
757:Geography of Alpes-de-Haute-Provence
725:Réserve géologique de Haute Provence
47:adding citations to reliable sources
708:"Analyse de Georges Henri Ducreux"
442:can also be found in the deposit.
14:
588:, and hence at an average depth.
681:
669:
657:
645:
633:
621:
609:
346:
339:
298:
23:
34:needs additional citations for
1:
767:Geologic formations of France
586:carbonate compensation depth
640:Inclination, from the North
628:Inclination, from the South
808:
355:Dalle à ammonites (France)
306:Provence-Alpes-Côte d'Azur
600:can be attributed to the
411:Coroniceras multicostatum
334:
203:
128:
563:Paleontological analysis
393:road. It is part of the
345:
792:Alpes-de-Haute-Provence
379:Alpes-de-Haute-Provence
787:Paleontology in France
616:Fossil-bearing strata
497:An almost horizontal
210:Dalle à ammonites in
438:seashells and other
278:44.11944°N 6.23417°E
43:improve this article
509:, is located below
371:Dalle aux ammonites
274: /
130:Stratigraphic range
58:"Dalle à ammonites"
735:2009-02-06 at the
525:Geodynamic context
414:, dating from the
16:French fossil site
488:Geological aspect
367:Dalle à ammonites
363:
362:
283:44.11944; 6.23417
124:Dalle à ammonites
119:
118:
111:
93:
799:
712:
711:
704:
685:
673:
661:
649:
637:
625:
613:
552:happened in the
513:bridge over the
455:Alcide d'Orbigny
350:
349:
343:
304:
302:
301:
289:
288:
286:
285:
284:
279:
275:
272:
271:
270:
267:
208:
199:
136:
121:
114:
107:
103:
100:
94:
92:
51:
27:
19:
807:
806:
802:
801:
800:
798:
797:
796:
772:Jurassic Europe
747:
746:
737:Wayback Machine
721:
716:
715:
706:
705:
701:
696:
689:
686:
677:
674:
665:
662:
653:
650:
641:
638:
629:
626:
617:
614:
565:
527:
501:slab, from the
495:
490:
451:
387:Digne-les-Bains
375:Digne-les-Bains
359:
358:
357:
356:
353:
352:
351:
299:
297:
282:
280:
276:
273:
268:
265:
263:
261:
260:
214:
212:Digne-les-Bains
198:
197:
192:
187:
182:
177:
172:
167:
162:
157:
152:
147:
142:
134:
133:
115:
104:
98:
95:
52:
50:
40:
28:
17:
12:
11:
5:
805:
803:
795:
794:
789:
784:
779:
774:
769:
764:
759:
749:
748:
745:
744:
739:
727:
720:
719:External links
717:
714:
713:
698:
697:
695:
692:
691:
690:
687:
680:
678:
675:
668:
666:
663:
656:
654:
651:
644:
642:
639:
632:
630:
627:
620:
618:
615:
608:
564:
561:
531:Alpine orogeny
526:
523:
494:
491:
489:
486:
450:
447:
420:Early Jurassic
361:
360:
354:
344:
338:
337:
336:
335:
332:
331:
326:
322:
321:
317:
316:
313:
309:
308:
295:
291:
290:
258:
252:
251:
247:
246:
245:Grey limestone
243:
239:
238:
234:
233:
230:
226:
225:
220:
216:
215:
209:
201:
200:
193:
188:
183:
178:
173:
168:
163:
158:
153:
148:
143:
138:
137:
126:
125:
117:
116:
31:
29:
22:
15:
13:
10:
9:
6:
4:
3:
2:
804:
793:
790:
788:
785:
783:
780:
778:
775:
773:
770:
768:
765:
763:
760:
758:
755:
754:
752:
743:
740:
738:
734:
731:
728:
726:
723:
722:
718:
709:
703:
700:
693:
684:
679:
672:
667:
660:
655:
648:
643:
636:
631:
624:
619:
612:
607:
605:
603:
599:
594:
589:
587:
583:
582:
577:
576:
570:
569:sedimentation
562:
560:
558:
555:
551:
547:
542:
540:
536:
532:
524:
522:
520:
516:
512:
508:
504:
500:
493:Similar sites
492:
487:
485:
483:
478:
474:
470:
468:
464:
460:
456:
448:
446:
443:
441:
437:
436:
431:
427:
423:
421:
417:
413:
412:
407:
403:
398:
396:
392:
388:
384:
380:
376:
372:
368:
342:
333:
330:
327:
323:
318:
314:
310:
307:
296:
292:
287:
259:
257:
253:
248:
244:
240:
235:
231:
227:
224:
221:
217:
213:
207:
202:
196:
191:
186:
181:
176:
171:
166:
161:
156:
151:
146:
141:
131:
127:
122:
113:
110:
102:
91:
88:
84:
81:
77:
74:
70:
67:
63:
60: –
59:
55:
54:Find sources:
48:
44:
38:
37:
32:This article
30:
26:
21:
20:
702:
598:bioturbation
593:tapophenosis
590:
579:
573:
566:
543:
528:
496:
479:
475:
471:
452:
449:Slab history
444:
433:
424:
409:
399:
370:
366:
364:
320:Type section
105:
96:
86:
79:
72:
65:
53:
41:Please help
36:verification
33:
572:settled as
554:paleo-ocean
459:ichthyosaur
281: /
256:Coordinates
223:Fossil site
777:Sinemurian
751:Categories
694:References
581:lumachella
550:subduction
539:Dauphinois
499:Ammonoidea
465:and other
430:belemnites
426:Nautiloids
416:Sinemurian
135:Sinemurian
99:April 2022
69:newspapers
537:, in the
517:river in
463:ammonites
406:ammonites
383:ammonites
325:Named for
266:44°7′10″N
237:Lithology
229:Thickness
733:Archived
515:Conturby
507:Jurassic
503:Triassic
482:Kamaishi
467:molluscs
440:bivalves
329:Ammonite
269:6°14′3″E
250:Location
688:Details
676:Details
664:Details
652:Détails
602:benthic
535:Prealps
511:Fressac
505:or the
312:Country
242:Primary
83:scholar
575:faluns
557:Tethys
435:Pecten
391:Barles
315:France
303:
294:Region
85:
78:
71:
64:
56:
389:from
373:) at
232:20 cm
90:JSTOR
76:books
591:The
546:Alps
544:The
519:Gard
402:slab
400:The
369:(or
365:The
219:Type
140:PreꞒ
62:news
578:or
45:by
753::
521:.
469:.
432:,
428:,
397:.
190:Pg
132::
710:.
418:(
377:(
195:N
185:K
180:J
175:T
170:P
165:C
160:D
155:S
150:O
145:Ꞓ
112:)
106:(
101:)
97:(
87:·
80:·
73:·
66:·
39:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.