Paleobiogeoclimatic scenarios of the Late Quaternary inferred from fluvial deposits of the Quadrilátero Ferrífero (Southeastern Brazil)

The Quadrilátero Ferrífero is an important mineral province in Southeastern Brazil and has one of the largest iron ore reserves in the world. Previous work in this region has indicated that the formation of fluvial successions with duricrusts coincided with drier/cooler climatic phases alternating w...

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Published inJournal of South American earth sciences Vol. 67; pp. 71 - 88
Main Authors Barros, Luiz Fernando de Paula, Coe, Heloísa Helena Gomes, Seixas, Amanda Pacheco, Magalhães, Antônio Pereira, Macario, Kita Chaves Damasio
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.04.2016
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Abstract The Quadrilátero Ferrífero is an important mineral province in Southeastern Brazil and has one of the largest iron ore reserves in the world. Previous work in this region has indicated that the formation of fluvial successions with duricrusts coincided with drier/cooler climatic phases alternating with moister/warmer periods during which the formation of fluvial successions without duricrusts occurred. For the construction of this proposal, ages of fluvial sediments obtained through Optically Stimulated Luminescence (OSL) were associated with data from the literature on paleobioclimatic scenarios. Therefore, using these observations as a starting point, this paper aims to investigate evidence of bioclimatic oscillations obtained directly from the fluvial successions and discuss its influence on the geomorphogenis of local river valleys. For this purpose, phytolith, carbon isotope and granulometric analyses were carried out, as well as dating of sediments using OSL and of soil organic matter through radiocarbon. The results show that in the oldest depositional succession (DS1 — about 34ka) the predominant phytoliths are those of bulliform polyedric, elongate, acicular and globular granulate types and δ13C values are typical of C3 plants. On the other hand, despite having a similar phytolith assemblage (abundance of bulliform polyedric, elongate, bulliform cuneiform, acicular, globular psilate and bilobate flat/concave types), the fluvial successions associated with significant conglomeratic duricrusts (DS2 and DS3) present a dominance of δ13C values characteristic of C4 plants. The Bi index indicates water stress in all the successions, and the Ic index suggests decreasing temperatures with depth in DS3. Thus, the three fluvial successions indicate a savanna-like environment, but depositional successions DS2 (∼27ka) and DS3 show drier/cooler climatic conditions when compared to DS1 and to the present-day regime. Both scenarios evolved under conditions of the Last Glacial period, but DS2 and DS3 were formed closer to the Last Glacial Maximum, and therefore under the strong influence of the lower temperatures during this period. These drier/cooler conditions in steep valleys with unprotected hillslopes may have been decisive for the formation of relatively thicker layers of gravel and sand, which later became duricrusts. The results indicate that climate has also played an important role in the regional hydrosedimentological dynamics, given the variations in vegetation influencing the abandonment of fill terraces and formation of nested floodplains. [Display omitted] •Terrace deposits show records of cerrado vegetation despite areas of forest today.•Climatic fluctuations may have influenced the evolution of fluvial systems.•The indicators used suggest a drier/cooler period for successions with duricrusts.•Internal variations indicate fluctuations in climate or local geomorphic conditions.
AbstractList The Quadrilátero Ferrífero is an important mineral province in Southeastern Brazil and has one of the largest iron ore reserves in the world. Previous work in this region has indicated that the formation of fluvial successions with duricrusts coincided with drier/cooler climatic phases alternating with moister/warmer periods during which the formation of fluvial successions without duricrusts occurred. For the construction of this proposal, ages of fluvial sediments obtained through Optically Stimulated Luminescence (OSL) were associated with data from the literature on paleobioclimatic scenarios. Therefore, using these observations as a starting point, this paper aims to investigate evidence of bioclimatic oscillations obtained directly from the fluvial successions and discuss its influence on the geomorphogenis of local river valleys. For this purpose, phytolith, carbon isotope and granulometric analyses were carried out, as well as dating of sediments using OSL and of soil organic matter through radiocarbon. The results show that in the oldest depositional succession (DS1 — about 34ka) the predominant phytoliths are those of bulliform polyedric, elongate, acicular and globular granulate types and δ13C values are typical of C3 plants. On the other hand, despite having a similar phytolith assemblage (abundance of bulliform polyedric, elongate, bulliform cuneiform, acicular, globular psilate and bilobate flat/concave types), the fluvial successions associated with significant conglomeratic duricrusts (DS2 and DS3) present a dominance of δ13C values characteristic of C4 plants. The Bi index indicates water stress in all the successions, and the Ic index suggests decreasing temperatures with depth in DS3. Thus, the three fluvial successions indicate a savanna-like environment, but depositional successions DS2 (∼27ka) and DS3 show drier/cooler climatic conditions when compared to DS1 and to the present-day regime. Both scenarios evolved under conditions of the Last Glacial period, but DS2 and DS3 were formed closer to the Last Glacial Maximum, and therefore under the strong influence of the lower temperatures during this period. These drier/cooler conditions in steep valleys with unprotected hillslopes may have been decisive for the formation of relatively thicker layers of gravel and sand, which later became duricrusts. The results indicate that climate has also played an important role in the regional hydrosedimentological dynamics, given the variations in vegetation influencing the abandonment of fill terraces and formation of nested floodplains. [Display omitted] •Terrace deposits show records of cerrado vegetation despite areas of forest today.•Climatic fluctuations may have influenced the evolution of fluvial systems.•The indicators used suggest a drier/cooler period for successions with duricrusts.•Internal variations indicate fluctuations in climate or local geomorphic conditions.
Author Coe, Heloísa Helena Gomes
Barros, Luiz Fernando de Paula
Magalhães, Antônio Pereira
Macario, Kita Chaves Damasio
Seixas, Amanda Pacheco
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  givenname: Luiz Fernando de Paula
  surname: Barros
  fullname: Barros, Luiz Fernando de Paula
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  organization: Departamento de Geografia, Universidade Federal de Minas Gerais, Antônio Carlos, 6627, Pampulha, Belo Horizonte, MG, 31270-901, Brazil
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  givenname: Heloísa Helena Gomes
  surname: Coe
  fullname: Coe, Heloísa Helena Gomes
  email: heloisacoe@yahoo.com
  organization: Departamento de Geografia, Universidade do Estado do Rio de Janeiro, Dr. Francisco Portela, 1470, Patronato, São Gonçalo, RJ, 24435-005, Brazil
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  givenname: Amanda Pacheco
  surname: Seixas
  fullname: Seixas, Amanda Pacheco
  email: amapaseixas@hotmail.com
  organization: Departamento de Geologia, Universidade Federal Fluminense, Passos da Pátria, 156, São Domingos, Niterói, RJ, 24210-240, Brazil
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  surname: Magalhães
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  email: magalhaesufmg@yahoo.com.br
  organization: Departamento de Geografia, Universidade Federal de Minas Gerais, Antônio Carlos, 6627, Pampulha, Belo Horizonte, MG, 31270-901, Brazil
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  givenname: Kita Chaves Damasio
  surname: Macario
  fullname: Macario, Kita Chaves Damasio
  email: kita@mail.if.uff.br
  organization: Instituto de Física, Universidade Federal Fluminense, General Milton Tavares de Souza, sala A1-01, Campus da Praia Vermelha, Gragoatá, Niterói, RJ, 24210-346, Brazil
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SSID ssj0005190
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Snippet The Quadrilátero Ferrífero is an important mineral province in Southeastern Brazil and has one of the largest iron ore reserves in the world. Previous work in...
SourceID crossref
elsevier
SourceType Aggregation Database
Publisher
StartPage 71
SubjectTerms Carbon isotopes
Optically stimulated luminescence
Phytoliths
Radiocarbon
Title Paleobiogeoclimatic scenarios of the Late Quaternary inferred from fluvial deposits of the Quadrilátero Ferrífero (Southeastern Brazil)
URI https://dx.doi.org/10.1016/j.jsames.2016.02.004
Volume 67
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