Paleoenvironmental reconstruction of a Late Quaternary lagoon system in southern Brazil (Jaguaruna region, Santa Catarina state) based on multi-proxy analysis

被引:26
|
作者
Carvalho do Amaral, Paula Garcia [1 ,2 ]
Fonseca Giannini, Paulo Cesar [1 ]
Sylvestre, Florence [2 ]
Ruiz Pessenda, Luiz Carlos [3 ]
机构
[1] Univ Sao Paulo, Inst Geociencias, Dept Geol Sedimentar & Ambiental, BR-01498 Sao Paulo, Brazil
[2] Aix Marseille Univ, CEREGE, CNRS, IRD, F-13545 Aix En Provence 4, France
[3] Univ Sao Paulo, CENA, Lab Carbono 14, Piracicaba, SP, Brazil
基金
巴西圣保罗研究基金会;
关键词
Late Quaternary; lagoon system; sedimentary dynamics; geochemistry; diatom analysis; pollen analysis; SEA-LEVEL VARIATIONS; HYDROLOGICAL CHANGES; LATE PLEISTOCENE; LATE-HOLOCENE; COAST; VARIABILITY; RAINFALL; CLIMATE;
D O I
10.1002/jqs.1531
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
This paper provides a paleoenvironmental reconstruction of a Late Quaternary lagoon system in the Jaguaruna region of Santa Catarina state, southern Brazil. Integrated results of bulk sedimentary organic matter characterization (delta C-13, delta N-15 and C/N), microfossil (pollen and diatom) and grain-size analysis from three shallow cores (similar to 2.5m depth) allowed us to propose an evolving paleogeographic scenario in this coastal region for the last ca. 5500 cal a BP. The lagoonal system in this area was more extensive during the mid-Holocene than today, with a gradual and continuous lagoon-sea disconnection until the present. We add to the debate regarding relative sea-level (RSL) variations for the Brazilian coast during the Holocene and discuss the importance of sedimentary dynamics for interpreting changes in coastal ecosystems. The multi-proxy analysis suggests that changes in coastal ecosystems could be directly related to local sedimentary processes, which are not necessarily linked to RSL fluctuations and/or to climatic variations. Copyright (c) 2011 John Wiley & Sons, Ltd.
引用
收藏
页码:181 / 191
页数:11
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