330:
302:
111:
337:
309:
636:
The formation was first named as the Santa Rosa
Sandstone by N.H. Darton in July 1919 but the report was not published until 1922. By then the name had already appeared in other publications. A type locality was not formally designated until 1972. In 1987,
842:
Beyl, Alexander; Nesbitt, Sterling; Stocker, Michelle R. (2 January 2020). "An
Otischalkian dinosauromorph assemblage from the Los Esteros Member (Santa Rosa Formation) of New Mexico and its implications for biochronology and lagerpetid body size".
1053:
1134:
329:
301:
1144:
208:
453:
were primarily to the south in the
Tecolotito Member and northeast in the Tres Lagunas Member but are indeterminate in the Los Esteros Member.
20:
645:
and divided the remaining beds into members. W.I. Finch and coinvestigators redesignated the unit as the Santa Rosa
Formation in 1988.
1139:
967:"Vertebrate paleontology and biochronology of the lower Chinle Group (Upper Triassic), Santa Fe County, north-central New Mexico"
994:
898:"Principal reference section for the Santa Rosa formation of Middle and Late Triassic age, Guadalupe County, New Mexico"
201:
510:
966:
409:
401:
272:
189:
142:
642:
418:
405:
152:
821:"Fossil plants from the mudstone member of the Santa Rosa Formation at the principal reference section"
1105:
936:
124:
363:
1075:"Interpretive depositional history of the Santa Rosa Formation at the principal reference section"
1033:
860:
1022:"Stratigraphy of the Anton Chico and Santa Rosa Formations, Triassic of east-central New Mexico"
466:
536:
1113:
1082:
944:
909:
852:
828:
638:
597:
381:
513:
that has yielded a diverse fossil assemblage. Fish fossils include lungfish toothplates of
476:
1109:
940:
550:
438:
1128:
924:
864:
585:
560:
378:
374:
257:
69:
34:
948:
445:
deposit in lakes that formed due to local subsidence from dissolution of underlying
110:
956:
Hager, Dorsey; Robitaille, A.E. (1919). "Oil possibilities in eastern New Mexico".
619:
615:
611:
567:
543:
450:
856:
578:
521:
44:
1054:"Revised Triassic stratigraphy in the Tucumcari basin, east-central New Mexico"
624:
600:
502:
495:
491:
442:
367:
243:
89:
54:
874:"Geologic structure of parts of New Mexico [Sandia and Manzano Mountains"
873:
223:
210:
1117:
591:
555:
531:
526:
515:
485:
393:
175:
94:
1096:
Rich, J.L. (1921). "The stratigraphy of eastern New Mexico; a correction".
604:
573:
434:
397:
179:
84:
79:
64:
59:
49:
1037:
1021:
925:"Composition and similarity of global anomodont-bearing tetrapod faunas"
481:
446:
371:
99:
74:
610:
In east-central New Mexico, the Los
Esteros Member has also yielded a
415:
The formation is divided into (in ascending stratigraphic order) the
1060:. New Mexico Museum of Natural History and Science. pp. 150–170
412:. The total thickness of the formation is 32 meters (105 ft).
1087:
1074:
914:
897:
833:
820:
472:
247:
462:
958:
California
Chamber of Mines and Oil, Mining and Oil Bulletin
641:
and Adrian Hunt removed the lower sandstone beds into the
134:
Tecolotito Member, Los
Esteros Member, Tres Lagunas Member
1002:
New Mexico Bureau of Mines and
Mineral Resources Bulletin
336:
308:
666:
664:
662:
660:
658:
1058:
Dawn of the age of dinosaurs in the
American southwest
974:
New Mexico
Geological Society Field Conference Series
614:
dinosauromorph assemblage that includes specimens of
509:
This member also includes a microvertebrate site in
316:
Santa Rosa Formation, New Mexico (the United States)
286:
278:
268:
263:
253:
239:
200:
195:
185:
171:
166:
158:
148:
138:
130:
120:
28:
742:
461:The Los Esteros Member has yielded fossils of the
115:Santa Rosa Formation along I-25 in Glorieta Pass.
596:. Synapsids are represented by an indeterminate
392:The formation consists mostly of white to brown
766:
534:. Amphibian fossil fragments are probably from
16:Geologic formation in New Mexico, United States
995:"Geology of the Fort Sumner sheet, New Mexico"
896:Finch, W.I.; Lupe, Robert; Ash, S.R. (1988).
441:. The Los Esteros Member is interpreted as a
344:Santa Rosa Formation, New Mexico (New Mexico)
8:
802:
965:Hunt, Adrian P.; Lucas, Spencer G. (1995).
109:
25:
1135:Sandstone formations of the United States
1086:
1026:Arizona-Nevada Academy of Science Journal
913:
832:
730:
682:
670:
433:The sandstone members are interpreted as
718:
654:
426:, which is primarily mudstone; and the
790:
754:
628:, the latter of unusually large size.
1056:. In Lucas, S.G.; Hunt, A.P. (eds.).
7:
778:
694:
422:, which is primarily sandstone; the
706:
845:Journal of Vertebrate Paleontology
14:
1145:Triassic formations of New Mexico
1052:Lucas, S.G.; Hunt, A.P. (1989).
1020:Lucas, S.G.; Hunt, A.P. (1987).
743:Beyl, Nesbitt & Stocker 2020
430:, which is primarily sandstone.
335:
328:
307:
300:
1079:U.S. Geological Survey Bulletin
949:10.1016/j.earscirev.2009.04.001
902:U.S. Geological Survey Bulletin
881:U.S. Geological Survey Bulletin
825:U.S. Geological Survey Bulletin
1:
857:10.1080/02724634.2020.1765788
524:dermopteric, and scales from
319:Show map of the United States
404:. The formation lies on the
1098:American Journal of Science
767:Hager & Robitaille 1919
511:Santa Fe County, New Mexico
1161:
803:Finch, Lupe & Ash 1988
370:that was deposited in the
18:
1140:Triassic geology of Texas
294:
108:
33:
632:History of investigation
1118:10.2475/ajs.s5-2.11.295
408:and is overlain by the
162:32 meters (105 ft)
410:Garita Creek Formation
400:with some interbedded
347:Show map of New Mexico
273:Santa Rosa, New Mexico
143:Garita Creek Formation
993:Kelley, V.C. (1972).
929:Earth-Science Reviews
923:Fröbisch, J. (2009).
872:Darton, N.H. (1922).
731:Hunt & Lucas 1995
683:Lucas & Hunt 1989
671:Lucas & Hunt 1987
643:Anton Chico Formation
406:Anton Chico Formation
153:Anton Chico Formation
437:sheets deposited by
360:Santa Rosa Formation
224:34.9620°N 104.6902°W
29:Santa Rosa Formation
21:Santa Rosa Formation
19:For other uses, see
1110:1921AmJS....2..295R
1081:. 1804-C: C19–C27.
1073:Lupe, R.D. (1988).
941:2009ESRv...95..119F
827:. 1804-C: C19–C27.
548:. Reptiles include
428:Tres Lagunas Member
220: /
35:Stratigraphic range
883:. 726-E: E173–E275
819:Ash, S.R. (1988).
424:Los Esteros Member
229:34.9620; -104.6902
530:, including from
356:
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1016:
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999:
989:
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935:(3–4): 119–157.
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639:Spencer G. Lucas
598:kannemeyeriiform
554:, indeterminate
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1104:(11): 295–298.
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960:: 13–16, 35–42.
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851:(1): e1765788.
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603:and an unnamed
477:Zamites powelli
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439:braided streams
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5:
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1100:. 5th Series.
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572:, several new
551:Trilophosaurus
458:
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362:is a geologic
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1088:10.3133/b1804
1084:
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915:10.3133/b1804
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834:10.3133/b1804
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719:Fröbisch 2009
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621:
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586:Hesperosuchus
582:
580:
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571:
569:
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562:
561:Desmatosuchus
557:
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547:
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500:, and seeds (
499:
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456:
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451:Paleocurrents
448:
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431:
429:
425:
421:
420:
413:
411:
407:
403:
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395:
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385:
383:
380:
379:late Triassic
376:
373:
369:
365:
361:
331:
303:
293:
289:
285:
281:
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274:
271:
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258:United States
256:
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66:
61:
56:
51:
46:
36:
32:
27:
22:
1101:
1097:
1078:
1064:17 September
1062:. Retrieved
1057:
1043:17 September
1041:. Retrieved
1032:(1): 21–33.
1029:
1025:
1011:17 September
1009:. Retrieved
1005:
1001:
984:17 September
982:. Retrieved
977:
973:
957:
932:
928:
905:
901:
887:17 September
885:. Retrieved
880:
848:
844:
824:
813:Bibliography
798:
786:
774:
762:
750:
738:
726:
714:
702:
690:
678:
635:
623:
622:, including
620:Lagerpetidae
616:Silesauridae
612:Otischalkian
609:
590:
584:
577:
568:Stagonolepis
566:
559:
549:
544:Apachesaurus
542:
535:
525:
514:
508:
501:
494:
484:
475:
465:
460:
432:
427:
423:
416:
414:
402:conglomerate
391:
359:
357:
287:Year defined
264:Type section
190:Conglomerate
791:Kelley 1972
755:Darton 1922
579:Chatterjeea
522:redfieldiid
449:salt beds.
417:Tecolotito
388:Description
366:exposed in
282:N.H. Dalton
227: /
215:104°41′25″W
202:Coordinates
1129:Categories
649:References
625:Dromomeron
601:dicynodont
563:haplocerus
556:phytosaurs
532:coprolites
503:Samaropsis
496:Dinophyton
492:gymnosperm
469:lasiophora
467:Cynepteria
443:lacustrine
368:New Mexico
244:New Mexico
212:34°57′43″N
980:: 243–246
865:221751762
779:Rich 1921
695:Lupe 1988
592:Parrishia
574:aetosaurs
537:Buttneria
527:Turseodus
516:Arganodus
488:pleoensis
486:Pelourdea
394:sandstone
364:formation
269:Named for
176:Sandstone
167:Lithology
159:Thickness
139:Underlies
131:Sub-units
125:Formation
1038:40024381
707:Ash 1988
605:cynodont
570:wellesii
546:gregorii
539:perfecta
518:dorothea
498:spinusos
435:alluvial
398:mudstone
279:Named by
196:Location
180:mudstone
149:Overlies
1106:Bibcode
937:Bibcode
581:elegans
482:conifer
457:Fossils
447:Permian
377:of the
372:Carnian
254:Country
172:Primary
40:Carnian
1036:
863:
594:mcreai
589:, and
490:, the
480:, the
471:, the
419:Member
382:Period
240:Region
1034:JSTOR
998:(PDF)
970:(PDF)
877:(PDF)
861:S2CID
473:cycad
248:Texas
186:Other
1066:2020
1045:2020
1013:2020
986:2020
906:1804
889:2020
618:and
541:and
520:, a
463:fern
396:and
358:The
290:1919
121:Type
45:PreꞒ
1114:doi
1083:doi
945:doi
910:doi
853:doi
829:doi
506:).
375:Age
1131::
1112:.
1077:.
1030:22
1028:.
1024:.
1006:98
1004:.
1000:.
978:46
976:.
972:.
943:.
933:95
931:.
927:.
908:.
904:.
900:.
879:.
859:.
849:40
847:.
823:.
657:^
607:.
583:,
576:,
565:,
558:,
384:.
246:,
178:,
95:Pg
37::
1120:.
1116::
1108::
1102:2
1091:.
1085::
1068:.
1047:.
1015:.
988:.
951:.
947::
939::
918:.
912::
891:.
867:.
855::
837:.
831::
805:.
793:.
781:.
769:.
757:.
745:.
733:.
721:.
709:.
697:.
685:.
673:.
100:N
90:K
85:J
80:T
75:P
70:C
65:D
60:S
55:O
50:Ꞓ
23:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
