Arid
DOI10.1016/j.gloplacha.2020.103136
Depositional histories of vegetation and rainfall intensity in Sierra Madre Oriental Mountains (northeast Mexico) since the late Last Glacial
Roy, Priyadarsi D.1; Vera-Vera, Guillermo2; Sanchez-Zavala, Jose L.1; Shanahan, Timothy M.3; Quiroz-Jimenez, Jesus D.4; Curtis, Jason H.5; Giron-Garcia, Patricia1; Lemus-Neri, Victor H.6; Muthusankar, Gowrappan7
通讯作者Roy, Priyadarsi D.
来源期刊GLOBAL AND PLANETARY CHANGE
ISSN0921-8181
EISSN1872-6364
出版年2020
卷号187
英文摘要An evaporite enriched sediment archive from the dry Sandia Basin located in the water-stressed western foothills of the Sierra Madre Oriental Mountains (northeast Mexico) was studied to reconstruct depositional histories of vegetation and rainfall intensity in orbital to millennial-scales over the last similar to 32.5 cal ka. Surrounding vegetation had more C-3 plants during the late last glacial and deglaciation and the expansion of more drought tolerant C-4 plants occurred only after similar to 5 cal ka BP. Classic minerals were sourced from different lithologies within the watershed and their abundances helped to infer runoff dynamics and hence the rainfall intensities. Deposition of more mixed-layer clay represented wetter intervals over the late last glacial and deglaciation. Transportation of elastics from the nearby lithology during these wetter intervals suggested that high-intensity rainfall events were less frequent. Response to the Heinrich stadials (H3, H2 and early H1) was mainly similar (drier) and erosion in the watershed remained less-than-average. Transportation of more quartz-rich sediments from distal lithologies during the late Bolling-Allerod (B/A) interstadial and between similar to 6.2 and 4 cal ka BP with a depositional hiatus between similar to 12.7 and 6.2 cal ka BP represented the intervals of more frequent high-intensity rainfall events, possibly related to short-lived storms. We hypothesize that the Gulf of Mexico sea surface temperature was a principal forcing. Total annual precipitation in this region decreased but the frequency of short-lived storms increased during the warmer Atlantic Multidecadal Oscillation (AMO) states. Warmer conditions also led to deposition of more gypsum. Our observation, however, needs further evaluation under the modern-day greenhouse warming scenario.
英文关键词Geochemistry Stable isotope Paleoclimate Heinrich stadial Atlantic Multidecadal Oscillation North America
类型Article
语种英语
国家Mexico ; USA ; India
收录类别SCI-E
WOS记录号WOS:000526518800002
WOS关键词CARBON-ISOTOPE DISCRIMINATION ; PLEISTOCENE-HOLOCENE TRANSITION ; ATLANTIC WARM POOL ; INTRA-AMERICA SEA ; LATE QUATERNARY ; CHIHUAHUAN DESERT ; CLIMATE-CHANGE ; DELTA-C-13 VALUES ; TROPICAL PACIFIC ; BAJA-CALIFORNIA
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
来源机构Universidad Nacional Autónoma de México
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/314628
作者单位1.Univ Nacl Autonoma Mexico, Inst Geol, Ciudad Univ, Ciudad De Mexico 04510, Mexico;
2.Univ Nacl Autonoma Mexico, Ciencias Tierra, Ciudad Univ, Ciudad De Mexico 04510, Mexico;
3.Univ Texas Austin, Dept Geosci, Austin, TX 78712 USA;
4.Univ Autonoma Estado Hidalgo, Area Acad Ciencias Tierra & Mat, Carretera Pachuca Tulancingo Km 4-5, Pachuca 42184, Hidalgo, Mexico;
5.Univ Florida, Dept Geol Sci, Gainesville, FL 32611 USA;
6.Univ Nacl Autonoma Mexico, USAI, Ciudad Univ, Ciudad De Mexico 04510, Mexico;
7.French Inst Pondicherry, 11 St Louis St, Pondicherry 605001, India
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GB/T 7714
Roy, Priyadarsi D.,Vera-Vera, Guillermo,Sanchez-Zavala, Jose L.,et al. Depositional histories of vegetation and rainfall intensity in Sierra Madre Oriental Mountains (northeast Mexico) since the late Last Glacial[J]. Universidad Nacional Autónoma de México,2020,187.
APA Roy, Priyadarsi D..,Vera-Vera, Guillermo.,Sanchez-Zavala, Jose L..,Shanahan, Timothy M..,Quiroz-Jimenez, Jesus D..,...&Muthusankar, Gowrappan.(2020).Depositional histories of vegetation and rainfall intensity in Sierra Madre Oriental Mountains (northeast Mexico) since the late Last Glacial.GLOBAL AND PLANETARY CHANGE,187.
MLA Roy, Priyadarsi D.,et al."Depositional histories of vegetation and rainfall intensity in Sierra Madre Oriental Mountains (northeast Mexico) since the late Last Glacial".GLOBAL AND PLANETARY CHANGE 187(2020).
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