Climate and landscape reconstruction of the Arroyo Chijuillita Member of the Nacimiento Formation, San Juan Basin, New Mexico: Providing environmental context to early Paleocene mammal evolution

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Climate and landscape reconstruction of the Arroyo Chijuillita Member of the Nacimiento Formation, San Juan Basin, New Mexico: Providing environmental context to early Paleocene mammal evolution

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作者：Adam J. Davis^a ; ^{adam_davis1@baylor.edu" class="auth_mail" title="E-mail the corresponding author} ; Daniel J. Peppe^a ; ^{daniel_peppe@baylor.edu" class="auth_mail" title="E-mail the corresponding author} ; Stacy C. Atchley^a ; ^{stacy_atchley@baylor.edu" class="auth_mail" title="E-mail the corresponding author} ; Thomas E. Williamson^b ; ^{thomas.williamson@state.nm.us" class="auth_mail" title="E-mail the corresponding author} ; Andrew G. Flynn^a ; ^{andrew_flynn@baylor.edu" class="auth_mail" title="E-mail the corresponding author}
关键词：Paleocene ; Paleoclimate ; San Juan Basin ; Paleosol ; Fluvial Sedimentology ; Puercan
刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
出版年：2016
出版时间：1 December 2016
年：2016
卷：463
期：Complete
页码：27-44
全文大小：4753 K

文摘

class="label">•: Early Paleocene sediments in the lower Nacimiento Fm. indicate a stable climate.
class="label">•: Early Paleocene San Juan Basin climate was warm, relatively wet and seasonally dry.
class="label">•: Changes in early Nacimiento sediments is driven by autocyclic channel migration.
class="label">•: Turnover in middle Puercan is likely due to rapid evolution and/or faunal dispersal.