Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.palaeo.2020.109586 |
Late Pleistocene and Late Holocene environment and climate in the campos region of southeastern South America inferred from phytolith, diatom and geochemical data | |
Mourelle, Dominique1; del Puerto, Laura1; Perez, Laura1; Bergamino, Leandro1; Garcia-Rodriguez, Felipe1,2 | |
通讯作者 | Mourelle, Dominique |
来源期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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ISSN | 0031-0182 |
EISSN | 1872-616X |
出版年 | 2020 |
卷号 | 543 |
英文摘要 | A paleolimnological study was undertaken for a sediment core from Laguna Formosa, a subtropical lake in the northern campos inland region of Uruguay. The record encompasses a Late Pleistocene and Late Holocene interval, interrupted by a hiatus. We analyzed (1) opal phytoliths and diatoms to infer the regional environment, climate, and changes in lake trophic state, and (2) total carbon and nitrogen (TC and TN) and stable isotope data (delta C-13 and delta N-15) to infer organic matter sources and composition. Findings indicate that, in Late Pleistocene times, a cool, semi-arid or highly seasonal climate existed, with a dominance of C3 grasslands and riparian hydrophilous shrublands while the shallow freshwater environment was characterized by benthic diatoms and littoral macrophytes. Late Holocene times were initially characterized by a temperate and humid or sub-humid climate, and dominance of grasslands and bunch grasses, while Laguna Formosa was dominated by phytoplankton. The abundance and diversity of littoral hydrophilic vegetation, and riparian forest vegetation, increased progressively over time, as a result of increased rainfall, from ca. 1800 cal yr BP and the onset of a subtropical (temperate and humid) climate by ca. 1300 cal yr BP. Such inferences are in close agreement with an earlier palynological study of Laguna Formosa, and support the paleoclimatic models for the Late Pleistocene and Late Holocene of southeastern South America. |
英文关键词 | Diatoms Opal phytoliths delta C-13 delta N-15 campos region Rio de la Plata grassland |
类型 | Article |
语种 | 英语 |
国家 | Uruguay ; Brazil |
收录类别 | SCI-E |
WOS记录号 | WOS:000518707600003 |
WOS关键词 | SEA-SURFACE TEMPERATURE ; ARAUCARIA FOREST ; SAO-FRANCISCO ; PALEOLIMNOLOGICAL EVIDENCE ; MULTIVARIATE-ANALYSIS ; PAULA REGION ; CARBON FLOW ; FRESH-WATER ; VEGETATION ; DYNAMICS |
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/2XILL650/315277 |
作者单位 | 1.Univ Republ, Ctr Univ Reg Este, Rocha, Uruguay; 2.Univ Fed Rio Grande, Inst Oceanog, Programa Posgrad Oceanol, Rio Grande, Brazil |
推荐引用方式 GB/T 7714 | Mourelle, Dominique,del Puerto, Laura,Perez, Laura,et al. Late Pleistocene and Late Holocene environment and climate in the campos region of southeastern South America inferred from phytolith, diatom and geochemical data[J],2020,543. |
APA | Mourelle, Dominique,del Puerto, Laura,Perez, Laura,Bergamino, Leandro,&Garcia-Rodriguez, Felipe.(2020).Late Pleistocene and Late Holocene environment and climate in the campos region of southeastern South America inferred from phytolith, diatom and geochemical data.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,543. |
MLA | Mourelle, Dominique,et al."Late Pleistocene and Late Holocene environment and climate in the campos region of southeastern South America inferred from phytolith, diatom and geochemical data".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 543(2020). |
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