Arid
DOI10.1016/j.palaeo.2013.07.022
Stable carbon isotope evidence for the abundance of C-4 plants in the middle Miocene of southern California
Feranec, Robert S.1; Pagnac, Darrin2
通讯作者Feranec, Robert S.
来源期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
EISSN1872-616X
出版年2013
卷号388页码:42-47
英文摘要

The abrupt spread of grasslands using C-4 photosynthesis, sometimes referred to as the rapid increase in C-4 ecosystems (RICE), occurred in the late Miocene in North America. While fossil plant specimens from the Miocene Dove Spring Formation of California as well as data from phylogenetic studies and molecular clocks show that C-4 grasses evolved prior to the RICE, most isotopic data from paleosols and mammal tooth enamel suggest that its abundance on the landscape was minimal. However, a few recent studies from the Great Plains suggest that C-4 grasslands may have been more prominent prior to the RICE event. Here we examine stable carbon isotope values from ungulate tooth enamel from the Barstow Formation of southern California, which is geographically and temporally close to the Dove Spring Formation, and records a diverse and abundant paleofauna of medial Miocene age. Tooth enamel delta C-13 values were examined in seven ungulate genera including the hypsodont equids; Acritohippus sp. and Scaphohippus sp.; the camelids, Aepycamelus sp., Hesperocamelus sp., and Procamelus sp.; the antilocaprid, Merycodus sp.; and the proboscidean, Gomphotherium sp. More positive delta C-13 values observed within the equids, camelids, and antilocaprids are suggestive of C-4 grasses being included in the diets of these taxa. The equids exhibited the most positive mean delta C-13 values, which indicate a higher component of dietary C-4 grasses (up to 18%) when compared to the other sampled ungulate taxa. The tooth enamel isotope values presented in this study show the presence of C-4 grasses as a significant component of ungulate diets millions of years before the RICE. The abundance of C-4 plants earlier in the Miocene may imply a more significant role in the major ungulate diversification events than previously suspected. The few pre-RICE localities showing evidence of C-4 abundance suggests that these grasslands were geographically restricted which limits, but may not exclude, the possibility that a world-wide mechanism controlled its spread. (C) 2013 Elsevier B.V. All rights reserved.


英文关键词C-4 grasses Barstow Formation Carbon isotopes Equidae Ungulates Miocene
类型Article
语种英语
国家USA
收录类别SCI-E
WOS记录号WOS:000326773800004
WOS关键词GRASS-DOMINATED ECOSYSTEMS ; ATMOSPHERIC CO2 ; NORTH-AMERICA ; GREAT-PLAINS ; BARSTOW FORMATION ; PRIMARY PRODUCTIVITY ; MOJAVE DESERT ; C4 PLANT ; EVOLUTION ; PHOTOSYNTHESIS
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS研究方向Physical Geography ; Geology ; Paleontology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/179149
作者单位1.New York State Museum & Sci Serv, Cultural Educ Ctr 3140, Albany, NY 12230 USA;
2.South Dakota Sch Mines & Technol, Dept Geol & Geol Engn, Rapid City, SD 57701 USA
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GB/T 7714
Feranec, Robert S.,Pagnac, Darrin. Stable carbon isotope evidence for the abundance of C-4 plants in the middle Miocene of southern California[J],2013,388:42-47.
APA Feranec, Robert S.,&Pagnac, Darrin.(2013).Stable carbon isotope evidence for the abundance of C-4 plants in the middle Miocene of southern California.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,388,42-47.
MLA Feranec, Robert S.,et al."Stable carbon isotope evidence for the abundance of C-4 plants in the middle Miocene of southern California".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 388(2013):42-47.
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