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Burnham South, San Juan County, New Mexico, USA
| Mindat.org Locality Page | San Juan County, New Mexico, USA |
|---|---|
| Lat/Long (Decimal) | 36.3,-108.2 |
| Co-ordinates Derivation | based on political unit |
| Given Location | New Mexico, United States |
| Mindat.org Region (for given coordinates) | San Juan County, New Mexico, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| 44 Store (High) | Williamson T. E. (1996) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| 44 Store (Low) | Williamson T. E. (1996) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| Aztec Station (Lower) | Granger W. (1917) | 63.3 - 61.7 Ma Paleocene | |||
| Aztec Station (Upper) | Alroy J. (2002) | 63.3 - 61.7 Ma Paleocene | |||
| Bab's Basin | Taylor L. H. (1981) | Nacimiento | close to the midpoint of a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Blanco Divide | West R. M. (1971) | Nacimiento - upper | 63.3 - 61.7 Ma Paleocene | ||
| Bohannan Draw | Alroy J. (2002) | 63.3 - 61.7 Ma Paleocene | |||
| Cedar Hill | Granger W. (1917) | 63.3 - 61.7 Ma Paleocene | |||
| Chico Springs | Lucas S. G., Alvarado G. E., et al (1997) | Nacimiento | low in a reversed magnetic polarity zone correlated with the Barrel Spring Arroyo = De-na-zin Wash section interpreted as C28r based on the position of the K-T boundary in that section: see Butler et al. 1977, Lucas et al. 1997 | not reported | 63.3 - 61.7 Ma Paleocene |
| Coprolite Point | Williamson T. E., Lucas S. G. (1993) | Nacimiento | high in a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Gallegos Canyon | Schoch R. M. (1986) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| Head of Barrel Spring Arroyo | Williamson T. E., Lucas S. G. (1993) | Nacimiento | within and not close to the bottom of a normal magnetic polarity zone in the Barrel Spring Arroyo = De-na-zin Wash section interpreted as C28n based on the position of the K-T boundary in the section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kimbetoh Arroyo (Middle) | Williamson T. E., Lucas S. G. (1993) | Nacimiento | three UALP localities are separated stratigraphically by five meters: Tomida 1981\nnear the top of the local section in a normal paleomag interval that is is probably chron 27n but could be chron 28n | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (Nine UALP Locs) | Taylor L. H. (1981) | Nacimiento | not far below the middle of a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7642) | Taylor L. H. (1981) | Nacimiento | not far below the middle of a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7655) | Taylor L. H. (1981) | Nacimiento | not far below the middle of a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7656) | Taylor L. H. (1981) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| Kutz Canyon (UALP 7674) | Taylor L. H. (1981) | Nacimiento | not far below the middle of a reversed magnetic polarity zone in the Kutz Canyon section interpreted as C27r based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7881) | Taylor L. H. (1981) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| Kutz Canyon (UALP 7896) | Taylor L. H. (1981) | Nacimiento | near the middle of a normal magnetic polarity zone in the Kutz Canyon section interpreted as C28n based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7897) | Tomida Y. (1981) | Nacimiento | show by Tomida as near the top of a normal zone, but near the middle of a normal magnetic polarity zone in the Kutz Canyon section interpreted as C28n based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UALP 7899) | Taylor L. H. (1981) | Nacimiento | shown as near the base of a reversed zone just above UALP 7897 by Tomida 1981, but near the middle of a normal magnetic polarity zone in the Kutz Canyon section interpreted as C28n based on the position of the K-T boundary in the correlative Barrel Spring Arroyo = De-na-zin Wash section: see Butler et al. 1977, Lucas et al. 1997 | 63.3 - 61.7 Ma Paleocene | |
| Kutz Canyon (UNM B-1096) | Schoch R. M., Lucas S. G. (1981) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| NMMNH 681 | Williamson T. E. (1996) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| O'Neill Pantolambda Site | Lucas S. G., O'Neill F. M. (1981) | Nacimiento | 63.3 - 61.7 Ma Paleocene | ||
| Upper Tsosie Wash | Eberle J. J., Lillegraven J. A. (1998) | Nacimiento | two UALP localities are separated stratigraphically by seven meters; LACM 5406 apparently at a very similar level, but may be from Kimbetoh Arroyo: see Williamson and Lucas 1993\nnear the top of the local section in a normal paleomag interval that is probably chron 27n but could be chron 28n, because there are anomalies such as normal polarization at the Ojo Alamo-Nacimiento contact and only one, very short reversed zone between that point and the fauna | 63.3 - 61.7 Ma Paleocene | |
| 2 miles above Ojo Alamo | Williamson T., Carr T. (2007) | Nacimiento | not reported | 66 - 63.3 Ma Paleocene | |
| Alamo Wash | Alroy J. (2002) | Nacimiento | 66 - 63.3 Ma Paleocene | ||
| Barrel Spring Arroyo (Ectoconus Zone) | Alroy J. (2002) | Nacimiento | low in a normal magnetic polarity zone in the Barrel Spring Arroyo = De-na-zin Wash section interpreted as C29n based on the position of the K-T boundary in the section: see Butler et al. 1977, Lucas et al. 1997 | 66 - 63.3 Ma Paleocene | |
| East Flank Kimbeto Wash (Puercan) | Williamson T. E. (1996) | Nacimiento | 66 - 63.3 Ma Paleocene | ||
| Mammalon Hill | Simpson G. G. (1936) | Nacimiento | underlies Middle ("Upper") Kimbetoh from an interval about 8 to 16 m above the Ojo Alamo-Nacimiento contact that is entirely of normal polarity and therefore almost certainly represents chron C29n: Lindsay et al. 1981; this interval is just below the middle of the normal zone | not reported | 66 - 63.3 Ma Paleocene |
| UCMP V-70181 | Greenwald N. S. (1988) | Nacimiento | said to be Puercan | 66 - 63.3 Ma Paleocene | |
| West Flank Kimbeto Wash (NMMNH L-5203) | Williamson T. E., Brusatte S. L. (2013) | Nacimiento | not reported | 66 - 63.3 Ma Paleocene | |
| West Flank Kimbeto Wash (NMMNH L-9181) | Williamson T. E., Brusatte S. L., et al (2016) | Nacimiento | Fossil Horizon A and within the Hemithlaeus kowalevskianus – Taeniolabis taoensis Biozone (H-T Zone) | mudstone | 66 - 63.3 Ma Paleocene |
| West Flank Kimbeto Wash (Puercan) | Williamson T. E. (1996) | Nacimiento | not reported | 66 - 63.3 Ma Paleocene | |
| West Fork of Gallegos Canyon | Lucas S. G. (1984) | Nacimiento | 66 - 63.3 Ma Paleocene | ||
| Fossil Forest Quarry 1 | Rigby, Jr. J. K., Wolberg D. L. (1987) | not reported | 70.6 - 66 Ma Late/Upper Cretaceous | ||
| Jon Powell Microsite | Flynn L. J. (1986) | Ojo Alamo - Naashoibito | not reported | 70.6 - 66 Ma Late/Upper Cretaceous | |
| Southern Slope of South Mesa | Flynn L. J. (1986) | Ojo Alamo - Naashoibito | not reported | 70.6 - 66 Ma Late/Upper Cretaceous | |
| Burnham South | Flynn L. J. (1986) | Fruitland | 83.5 - 70.6 Ma Late/Upper Cretaceous | ||
| Fossil Forest Quarry 1 (NMMNH L-4276) | Williamson T. E., Brusatte S. L. (2014) | Fruitland - Fossil Forest | not reported | 83.5 - 70.6 Ma Late/Upper Cretaceous | |
| Jacobs Bone Bed | Alroy J. (2002) | 83.5 - 70.6 Ma Late/Upper Cretaceous | |||
| Lower Hunter Wash | Alroy J. (2002) | Kirtland - Hunter Wash | not reported | 83.5 - 70.6 Ma Late/Upper Cretaceous |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
