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Fig 1.

Experimental Station of Caldeirão, Central Amazon—Brazil.

The base image is LANDSAT 5 image (2011). The Landsat images were downloaded from USGS.

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Fig 1 Expand

Fig 2.

(A) Pretic Anthrosol (Orthodystric, Clayic) (P1); (B) Pretic Anthrosol (Lixic, Orthoeutric, Clayic) (P2); (C) Haplic Xanthic Acrisol (Hyperdystric, Clayic) (P3).

Central Amazon—Brazil.

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Fig 2 Expand

Table 1.

Some morphological and physical properties in (A) Pretic Anthrosol (Orthodystric, Clayic), (B) Pretic Anthrosol (Lixic, Orthoeutric, Clayic) and (C) Haplic Xanthic Acrisol (Hyperdystric, Clayic).

Central Amazon—Brazil.

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Table 1 Expand

Table 2.

Chemical properties in (A) Pretic Anthrosol (Orthodystric, Clayic), (B) Pretic Anthrosol (Lixic, Orthoeutric, Clayic) and (C) Haplic Xanthic Acrisol (Hyperdystric, Clayic).

Central Amazon—Brazil.

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Table 3.

Summary of the micromorphological description of the Pretic Anthrosol (Orthodystric, Clayic).

Central Amazon—Brazil.

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Table 3 Expand

Table 4.

Summary of the micromorphological description of the Pretic Anthrosol (Lixic, Orthoeutric, Clayic).

Central Amazon—Brazil.

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Table 4 Expand

Table 5.

This is the Table 5 Summary of the micromorphological description of the Haplic Xanthic Acrisol (Hyperdystric, Clayic).

Central Amazon—Brazil.

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Table 5 Expand

Fig 3.

Different color of the fine material (melanization) in Pretic Anthrosol (Orthodystric, Clayic) (OIL).

(A) Au1: single fine material dark gray (10YR 4/1); (B) Au2: 60% brownish yellow (10YR 6/8), 30% yellow (10YR 8/8) and 10% dark gray; (C) Au3: 80% brownish yellow and 20% yellow; (D) Au4: 45% brownish yellow, 35% dark gray and 20% yellow; (E) Au5: 50% yellow, 35% dark gray and 15% brownish yellow; (F) Bt1 exclusively yellow. q: quartz; v: voids; c: charcoal.

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Fig 3 Expand

Fig 4.

Microstructure types (PPL).

(A and B) granular microstructure of Au1 horizons; (C) subangular block microstructure of non-anthropic A; (D) different types of microaggregates in pretic horizons. q: quartz; v: voids; a: oval microaggregates with well-sorted quartz; b: oval microaggregates with or without poorly-sorted quartz; c: polyhedral microaggregates.

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Fig 5.

Textural pedofeatures in pretic horizons (A and B—XPL) (C and D—PPL).

(A) typical yellow red microlaminated (m) and non-laminated (nl) clay coatings with strong continuous orientation and extinction bands (Au4); (B) illuvial clay coating on ceramic fragment; (C) non-laminated reddish yellow hypo-coating (detail); (D) fragment of clay coatings (papule) with moderately continuous orientation and diffuse extinction (Au5).

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Fig 5 Expand

Table 6.

Chemical composition by EDS-SEM of nodules and micromass associated to biological channels in (A) Pretic Anthrosol (Orthodystric, Clayic), (B) Pretic Anthrosol (Lixic, Orthoeutric, Clayic) and (C) Haplic Xanthic Acrisol (Hyperdystric, Clayic).

Central Amazon—Brazil.

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Fig 6.

Amorphous pedofeatures (nodules) in Pretic Anthrosol (Lixic, Orthoeutric, Clayic).

(A and B) irregular, orthic and concentric nodules with very small voids, spongy-like (ultraviolet light); (C and D) nodules formed of several smaller entities each separated by adjacent groundmass (disjointed morphology) (OIL).

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Fig 7.

The xanthization process at different stages in the nodules.

(A and B) dark red (PPL) and yellow (OIL) nodules with a strongly impregnative core and a weaker impregnative cortex (dissolution); (C) detail of nodule with internal fabric severed at the boundaries with groundmass and serrated edges (degradation) (OIL); (D) hematite nodule at intermediate degradation stage with yellowish red infillings; (E) highly changed nodule, predominantly yellow with yellowish red edges (OIL); (F) nodule completely changed, yellowish and without reddish material (OIL).

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