Arid
DOI10.1016/j.earscirev.2019.102901
The magnitude and cause of short-term eustatic Cretaceous sea-level change: A synthesis
Ray, David C.; van Buchem, Frans S. P.; Baines, Graham; Davies, Andrew; Greselle, Benjamin; Simmons, Michael D.; Robson, Christopher
通讯作者Ray, David C.
来源期刊EARTH-SCIENCE REVIEWS
ISSN0012-8252
EISSN1872-6828
出版年2019
卷号197
英文摘要No consensus currently exists regarding the magnitude of Cretaceous short-term (less than 3 Ma in duration) eustatic sea-level change. The lack of a consensus limits the ability to predict sedimentary facies and architecture and to assess the potential drivers of eustasy during a period of Earth history considered as significantly warmer than today. Consequently, this review documents, weighs, synthesises, and summarises records of short-term relative sea-level change and evaluates the observed trends in magnitude within the context of potential climatic drivers and their eustatic expression. Although Cretaceous sea-level change is addressed in many publications, estimates of absolute values are relatively limited, often cover short time intervals, and use different methods. Based upon integrated geological and statistical analyses, four broad episodes of magnitude change have been identified. Three of these episodes reflect trends of increasing magnitudes of sea-level change from the Berriasian to early Hauterivian, late Hauterivian to Aptian, and Santonian to Maastrichtian. The fourth episode reflects a decreasing magnitude trend from the Albian to Coniacian. In addition, the maximum magnitude of sea-level change, at an approximate stage level, has been identified and categorised as slight (less than 10 m), modest (10 to 40 m), or significant (41 to 65 m). Significant magnitudes are inferred for the Valanginian, Aptian, Albian, and Maastrichtian; exclusively slight magnitudes are restricted to the Berriasian. Such an assessment casts doubt on the repeated and stratigraphically widespread episodes of very large magnitudes (more than 75 m) advocated by some workers, and instead defines distinct periods and magnitudes of sea-level change that should be globally reflected in sedimentary facies patterns. For example, intervals of sea-level fall of significant magnitude are commonly associated with the increased delivery of sediment into basinal settings, including the marked progradation of shallow-marine sediments, whilst up-systems tract there can be enhanced development of karst and erosional features. Because climatically driven eustasy is the likely cause of short-term sea-level change, an assessment of the characteristic maximum magnitude limits of the principal climatic drivers (thermo-, aquifer-, and glacio-eustasy) has been made. Such a comparison argues for glacio-eustasy as the driver of significant short-term sea-level change. In addition, climate proxy data demonstrates that the Valanginian, Aptian, Albian, and Maastrichtian are intervals of cooling within the Cretaceous, thereby supporting the link between significant magnitudes and glacio-eustasy.
英文关键词Cretaceous sea-level synthesis Eustatic magnitudes Glacio-eustasy Short-term sea-level change
类型Review
语种英语
国家England
收录类别SCI-E
WOS记录号WOS:000497253500015
WOS关键词HIGH-FREQUENCY ; FORAMINIFERAL RESPONSE ; SEQUENCE STRATIGRAPHY ; WESTERN DESERT ; NEW-JERSEY ; ICE ; FLUCTUATIONS ; PLATFORM ; SUCCESSION ; MARGIN
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
EI主题词2019-10-01
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/310248
作者单位Halliburton, 97 Jubilee Ave,Milton Pk, Abingdon OX14 4RW, Oxon, England
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GB/T 7714
Ray, David C.,van Buchem, Frans S. P.,Baines, Graham,et al. The magnitude and cause of short-term eustatic Cretaceous sea-level change: A synthesis[J],2019,197.
APA Ray, David C..,van Buchem, Frans S. P..,Baines, Graham.,Davies, Andrew.,Greselle, Benjamin.,...&Robson, Christopher.(2019).The magnitude and cause of short-term eustatic Cretaceous sea-level change: A synthesis.EARTH-SCIENCE REVIEWS,197.
MLA Ray, David C.,et al."The magnitude and cause of short-term eustatic Cretaceous sea-level change: A synthesis".EARTH-SCIENCE REVIEWS 197(2019).
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