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Arroyo Formation

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Journal Article
Journal: Geology
Published: 01 May 2001
Geology (2001) 29 (5): 399–402.
... not conducive for arroyo formation along the floors of desert valleys. After a hiatus in arroyo formation, the frequency of arroyo cutting and filling increased dramatically after 4000 14 C yr B.P. The early Holocene arroyos and increased frequency of arroyo incision after 4000 14 C yr B.P. are related...
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First thumbnail for: Late Quaternary <span class="search-highlight">arr...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2013
GSA Bulletin (2013) 125 (7-8): 1114–1124.
... and tectonics; however, how and why they form remain poorly understood. Here, we focus on Arroyo Seco in the central California Coast Ranges, where we test hypotheses for strath planation and subsequent strath terrace formation. Several lines of evidence indicate that strath planation is triggered by braiding...
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First thumbnail for: Sediment supply, base level, braiding, and bedrock...
Second thumbnail for: Sediment supply, base level, braiding, and bedrock...
Third thumbnail for: Sediment supply, base level, braiding, and bedrock...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1969
AAPG Bulletin (1969) 53 (7): 1518–1519.
... American Association of Petroleum Geologists Baltz’ critical review should have been directed more to my late 1967 paper, Biostratigraphy and carbonate facies of the Mississippian Arroyo Peñasco Formation, north-central New Mexico , published as New Mexico Bureau of Mines and Mineral Resources...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1969
AAPG Bulletin (1969) 53 (7): 1508–1518.
.... Publication authorized by Director, U.S. Geological Survey. 2 Geologist, U.S. Geological Survey. © 1969 American Association of Petroleum Geologists. All rights reserved 1969 American Association of Petroleum Geologists In the interim report on the Mississippian Arroyo Peñasco Formation...
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First thumbnail for: Interim Report on Mississippian <span class="searc...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1967
AAPG Bulletin (1967) 51 (3): 417–424.
... of north-central New Mexico, Precambrian crystalline rocks are overlain at many places by the Arroyo Peñasco Formation, a thin sequence of shallow-marine to intertidal clastic and carbonate rocks of late Osage to middle Meramec (Mississippian) age. In 1962 the writers measured and re-collected...
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First thumbnail for: Interim Report on Mississippian <span class="searc...
Second thumbnail for: Interim Report on Mississippian <span class="searc...
Third thumbnail for: Interim Report on Mississippian <span class="searc...
Journal Article
Published: 01 September 1958
Journal of Paleontology (1958) 32 (5): 970–976.
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1935–1944.
... River Canyon of southern Colorado. The formation in which the fossils occur is discontinuous, preserved only as isolated erosional remnants. The most complete section observed, and the best fossil locality, is in Arroyo Penasco in the San Ysidro Quadrangle, Sandoval County, New Mexico. It is proposed...
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First thumbnail for: <span class="search-highlight">ARROYO</span> PEÑAS...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1942
AAPG Bulletin (1942) 26 (1): 80–99.
...Robert L. Bates ABSTRACT Surface exposures in the walls of Rocky Arroyo and adjacent canyons, 12 miles northwest of Carlsbad, New Mexico, reveal an abrupt lateral change in lithology in the Seven Rivers formation. A 275-foot section of gypsum with thin beds of dolomitic limestone merges...
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First thumbnail for: Lateral Gradation in the Seven Rivers <span class=...
Second thumbnail for: Lateral Gradation in the Seven Rivers <span class=...
Third thumbnail for: Lateral Gradation in the Seven Rivers <span class=...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1941
AAPG Bulletin (1941) 25 (5): 935.
...Robert L. Bates The paper embodies results of a study of surface exposures of Rocky Arroyo, 12 miles northwest of Carlsbad, New Mexico. In the walls of this and adjacent canyons is revealed an abrupt lateral change in lithology in the Seven Rivers formation. A 275-foot section of gypsum with thin...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2003
GSA Bulletin (2003) 115 (5): 596–606.
... began to dominate, channel erosion was typically initiated by a shift from relatively warmer and drier to cooler and wetter climates. The timing of erosion events exhibits a remarkable correlation to arroyo formation and paleosol formation of ephemeral streams in the North American southwest...
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First thumbnail for: Late Quaternary fluvial landscape evolution in des...
Second thumbnail for: Late Quaternary fluvial landscape evolution in des...
Third thumbnail for: Late Quaternary fluvial landscape evolution in des...
Journal Article
Published: 01 November 2018
Journal of Paleontology (2018) 92 (6): 1092–1106.
.... However, most of this material has been sourced from the oldest member, the Arroyo Formation, and the understanding of the paleoecosystem of the younger Vale and Choza formations is less well resolved. Here we present a previously undescribed Vale locality, the first vertebrate-bearing locality from...
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First thumbnail for: Faunal overview of the Mud Hill locality from the ...
Second thumbnail for: Faunal overview of the Mud Hill locality from the ...
Third thumbnail for: Faunal overview of the Mud Hill locality from the ...
Journal Article
Published: 01 May 1968
Journal of Paleontology (1968) 42 (3): 827–835.
...David S. Berman Abstract Well preserved tooth plates, vomerine teeth, and lower jaws of the lungfish Gnathorhiza, collected from the Lueders and Arroyo Formations [in Baylor County, north-central Texas], are in close accord with those of other late Paleozoic dipnoans, particularly Sagenodus...
Journal Article
Published: 01 March 2020
Journal of Paleontology (2020) 94 (2): 366–377.
...Bryan M. Gee; Robert R. Reisz Abstract Nanobamus macrorhinus Schoch and Milner, 2014 is a small amphibamiform temnospondyl from the early Permian Arroyo Formation of Texas. It is most readily characterized by an elongate and partially subdivided naris. This condition is superficially reminiscent...
FIGURES
First thumbnail for: The amphibamiform Nanobamus macrorhinus from the e...
Second thumbnail for: The amphibamiform Nanobamus macrorhinus from the e...
Third thumbnail for: The amphibamiform Nanobamus macrorhinus from the e...
Journal Article
Published: 21 November 1999
Canadian Journal of Earth Sciences (1999) 36 (8): 1257–1266.
... correlations imply that the exact age of the Richards Spur deposits is uncertain, and equivalence to the Arroyo Formation of Texas may be erroneous. Les éléments isolés d'un squelette d'amphibien du genre Seymouria ont été récemment découverts dans la localité de Richards Spur, près de Fort Sill, en...
Journal Article
Published: 01 September 1991
Canadian Journal of Earth Sciences (1991) 28 (9): 1488–1492.
...David W. Dilkes Abstract Restudy of the only indisputable larval temnospondyl from the Lower Permian (Arroyo Formation: Clear Fork Group) of North America has revealed the presence of a narial flange, which supports its assignment to the superfamily Dissorophoidea. Two families of dissorophoids...
Journal Article
Published: 01 June 1982
Canadian Journal of Earth Sciences (1982) 19 (6): 1232–1234.
...R. R. Reisz; M. J. Heaton Abstract Bayloria morei from the Lower Permian (Arroyo Formation, Clear Fork Group: Leonardian) of Baylor County, Texas, formerly thought to be the smallest known pelycosaur, is an immature specimen of the captorhinid reptile Captorhinus aguti . As the latter name has...
Image
Figure 7. Summary of regional paleoecology and paleoclimate interpretations in comparison to periods of alluvial deposition, channel erosion, and soil formation in the Juanaquena study area and to periods of arroyo formation, high-magnitude flooding, and black mat formation in the North American Sonoran Biogeographic Province. (a) Based on paleosol stable C isotopes from southern New Mexico (Buck and Monger, 1999). (b) Stable carbon isotopes from alluvial paleosols in the Juanaquena study area, with standard deviations shown by symbol width. (c) Stable carbon isotope curve taken from Lake Babicora sediments (Huang et al., 2001) after conversion of n-alkane δ13C values to bulk sediment humate δ13C values using−19‰ as the C4 end member. (d) Modified from lake-level fluctuations and sediment geochemistry of Lake Babicora (modified from Ortega-Ramirez et al., 1998). (e) Arroyo formation from Waters and Haynes (2001) in Arizona. (f) Maximum flood magnitudes estimated from slackwater deposits in the North American Southwest (Ely et al., 1993). (g) Black mat formation and high water tables from southern Utah (Quade et al., 1998).
Published: 01 May 2003
Figure 7. Summary of regional paleoecology and paleoclimate interpretations in comparison to periods of alluvial deposition, channel erosion, and soil formation in the Juanaquena study area and to periods of arroyo formation, high-magnitude flooding, and black mat formation in the North American
Image
Antropora guajirensis n. sp. from the Siamaná Formation, Arroyo Uitpa (holotype MUN-STRI-47628): (1) general view; (2) detail of the autozooids with intramural reparative budding, drop shaped interzooidal avicularia, and cap-like ooecium (arrowed); (3) close-up of two autozooids and interzooidal avicularia. Scale bars are (1) 0.25 mm; (2) 0.2 mm; (3) 0.15 mm.
Published: 01 July 2021
Figure 3. Antropora guajirensis n. sp. from the Siamaná Formation, Arroyo Uitpa (holotype MUN-STRI-47628): ( 1 ) general view; ( 2 ) detail of the autozooids with intramural reparative budding, drop shaped interzooidal avicularia, and cap-like ooecium (arrowed); ( 3 ) close-up of two autozooids
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Gymnophorella hadra n. gen. n. sp. from the Siamaná Formation, Arroyo Uitpa (holotype MUN-STRI-47640): (1) detail of the regular autozooids, (2) detail of two autozooids with intramural buds and opesia showing opesiular indentations; (paratype MUN-STRI-47641): (3, 4) general view of the multiserial stage, (5) close-up of autozooids and a kenozooid (arrowed). Scale bars are (1, 4) 0.5 mm; (2, 5) 0.25 mm; (3) 1 mm.
Published: 01 July 2021
Figure 8. Gymnophorella hadra n. gen. n. sp. from the Siamaná Formation, Arroyo Uitpa (holotype MUN-STRI-47640): ( 1 ) detail of the regular autozooids, ( 2 ) detail of two autozooids with intramural buds and opesia showing opesiular indentations; (paratype MUN-STRI-47641): ( 3, 4 ) general
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Calpensia caribensis n. sp. from the Siamaná Formation, Arroyo Ekieps (holotype MUN-STRI-47635): (1) autozooids showing the semicircular opesia and the proximally raised opercular region, (2) close-up of autozooids showing paired opesiules, (3) general view of the colony. Atoichos magnus n. gen. n. sp. from the Siamaná Formation, Arroyo Ekieps (holotype MUN-STRI-47637); asterisks indicate putative avicularia: (4) group of autozooids, (5) oblique view showing the development and shape of the cryptocyst and the distal raised opesial margin (arrowed), (6) zooids showing well-preserved opesia with opesiular indentations and the distal opesial margin (arrowed). Scale bars are (1, 2, 4–6) 0.5 mm; (3) 1 mm.
Published: 01 July 2021
Figure 5. Calpensia caribensis n. sp. from the Siamaná Formation, Arroyo Ekieps (holotype MUN-STRI-47635): ( 1 ) autozooids showing the semicircular opesia and the proximally raised opercular region, ( 2 ) close-up of autozooids showing paired opesiules, ( 3 ) general view of the colony