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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Fluvial aggradation and incision in the Brazilian tropical semi-arid: Climate-controlled landscape evolution of the Sao Francisco River

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Author(s):
Mescolotti, Patricia Colombo [1] ; Pupim, Fabiano do Nascimento [2] ; Bernardes Ladeira, Francisco Sergio [3] ; Sawakuchi, Andre Oliveira [4] ; Catharina, Amanda Santa [5] ; Assine, Mario Luis [1]
Total Authors: 6
Affiliation:
[1] Univ Estadual Paulista Unesp, Inst Geociencias & Ciencias Exatas, Ave 24A, 1515, BR-13506900 Rio Claro - Brazil
[2] Univ Fed Sao Paulo, Dept Ciencias Ambientais, Rua Sao Nicolau 210, BR-09913030 Sao Paulo - Brazil
[3] Univ Estadual Campinas Unicamp, Inst Geociencias, R Carlos Gomes 250, Campinas, SP - Brazil
[4] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo - Brazil
[5] Univ Vale Rio Sinos Unisinos, Itt Fossil, Ave Unisinos 950, BR-93020190 Sao Leopoldo, RS - Brazil
Total Affiliations: 5
Document type: Journal article
Source: QUATERNARY SCIENCE REVIEWS; v. 263, JUL 1 2021.
Web of Science Citations: 0
Abstract

Large rivers are dynamic systems whose evolution depends on both internal and external forcing, particularly tectonics, sea level, and climate. Associating fluvial responses to a specific driver is a complex task that has been debated for a long time. Thus, rivers that flow exclusively under tectonically stable areas and without direct influence of relative sea level changes are suitable targets to understand how large fluvial systems responded to past climate changes. The Sao Francisco River is one of the largest cratonic rivers across South America, and its late Quaternary sedimentary deposits record the fluvial landscape evolution in a thousand-year timescale. The Sao Francisco River flows northward over different climate zones, with its upper course in a semi-humid setting, but with most of its watershed under semi-arid conditions. To understand the controls on sediment erosion, transport, and storage from uplands to lowlands, we investigated a 200-km section of the medium course of the Sao Francisco River in northeast Brazil. Several geomorphological zones were characterized, mapped, and dated by optically stimulated luminescence (OSL). Two zones are represented by degraded terraces with lakes, but no preserved alluvial features: (zone 1) high-level terrace (87.7 +/- 12.7 ka) and (zone 2) low-level terrace (65.5 +/- 5.3 to 39.3 +/- 4.3 ka). Three zones comprise the active confined aggradational plain, with features such as scroll bars and abandoned channels: (zone 3) older meander belt (18.1 +/- 1.6 ka); (zone 4) young meander belt (15.5 +/- 1.5 to 9.5 +/- 1.0 ka), and (zone 5) modern channel belt (0.4 +/- 0.1 to 0.3 +/- 0.1 ka). Zone 6 comprises an eolian dune field composed of parabolic dunes with two phases of active sedimentation (45.1 +/- 5.2 to 25.5 +/- 4.4 ka and 14.3 +/- 2.6 to 5.2 +/- 1.4 ka). Sediment deposition ages allowed the recognition of at least four phases of fluvial aggradation (90 ka; 66 to 39 ka; 18 to 9 ka and 0.3 ka to recent), three phases of incision (85 to 66 ka; 39 to 18 ka and 9 to 1 ka), and two phases of dune field stabilization (25 to 15 ka and 5 ka to recent). Development of the eolian dune fields occurred during drier conditions, when the inland activity of trade winds reworked sediments deposited on the fluvial plain. We interpret the incision events as having been set in motion by an increase of fluvial discharge in the upper catchment area, produced by rainfall intensification due to activity of the South Atlantic Convergence Zone (SACZ). The aggradation and incision phases on the Sao Francisco River during the last 100 ka are therefore likely controlled by multi-millennial precipitation changes, possibly related to precession cycles. The events of high sedimentation rate in the Sao Francisco river mouth are partially correlated with incision phases in its middle course. This suggests that sedimentation in plains of large plateau rivers can be decoupled from the coastal area. (C) 2021 Published by Elsevier Ltd. (AU)

FAPESP's process: 17/50085-3 - PIRE: climate research education in the Americas using tree-ring speleothem examples (PIRE-CREATE)
Grantee:Francisco William da Cruz Junior
Support Opportunities: Research Projects - Thematic Grants