DOI: 10.1016/j.catena.2019.104333
论文题名: Multi proxy analysis for reconstructing the late Holocene evolution of a Mediterranean Coastal Lagoon: Environmental variables within foraminiferal assemblages
作者: López-Belzunce M. ; Blázquez A.M. ; Carmona P. ; Ruiz J.M.
刊名: Catena
ISSN: 3418162
出版年: 2020
卷: 187 语种: 英语
英文关键词: Coastal Lagoon evolution
; Foraminifera
; Paleoenvironments
; Western Mediterranean
Scopus关键词: calcium carbonate
; coastal evolution
; coastal lagoon
; flood
; foraminifera
; fossil assemblage
; fossil record
; Holocene
; landscape
; Medieval Warm Period
; paleoenvironment
; progradation
; reconstruction
; Mediterranean Region
; Valencia
; Foraminifera
英文摘要: This study reconstructs the evolution of foraminiferal assemblages and the environmental variables (type of substrate, content in calcium carbonate and content in organic matter) in the Valencia lagoon (western Mediterranean) in response to changes in the late Holocene. In this area of low tidal range, several multiproxy analyses were carried out to determine which environmental variables influence the distribution of the fossil assemblage, and its association with global, regional or local climatic phenomena. The statistical results show that in environments with higher exposure to marine conditions, the calcium carbonate content is the dominant factor, whereas in more restricted environments the type of substrate (grain size) is determinant. The micropaleontological content reveals the evolution from a saline paleoenvironment with a clear marine influence towards the hyposaline or freshwater conditions, recorded at the top. Three phases were identified in the evolution of this area from 2800 cal yr BP to the present. A brackish lagoon with marine connection at the base, followed by a deposit of brackish lagoon (1232 ± 74 cal yr BP − 791 ± 104 cal yr BP), culminating in a brackish marsh (791 ± 104 cal yr BP to present), interpreted as the definitive closure process of the lagoon, favored by the coastal progradation processes related with an extraordinary input of sediments. These findings reflect the climatic variability of the Medieval Climate Optimum (MCO) (1.05 and 0.65 kcal BP) and the migration of the river Turia mouth, which favored the coastal progradation processes. The flood events registered at this phase, may have coincided with changes in the landscape and greater anthropic influence at the end of the LIA, 150 cal yr BP. Coastal processes are mainly responsible for the evolution of this area during phase I, while the influence of fluvial processes is significant towards the top, especially in phase III. © 2019 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/158611
Appears in Collections: 气候变化与战略
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作者单位: Environmental and Marine Sciences Research Institute, Escuela de Doctorado, Catholic University of Valencia, C/Guillem de Castro 94, Valencia, 46003, Spain; Environmental and Marine Sciences Research Institute, Catholic University of Valencia, C/ Guillem de Castro 94, Valencia, 46003, Spain; Department of Geography, University of Valencia, Av. Blasco Ibáñez, 28, Valencia, 46010, Spain
Recommended Citation:
López-Belzunce M.,Blázquez A.M.,Carmona P.,et al. Multi proxy analysis for reconstructing the late Holocene evolution of a Mediterranean Coastal Lagoon: Environmental variables within foraminiferal assemblages[J]. Catena,2020-01-01,187