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Correction: Unravelling the mystery of "Madagascar copal": Age, origin and preservation of a Recent resin.

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Abstract

[This corrects the article DOI: 10.1371/journal.pone.0232623.].

Entities:  

Year:  2020        PMID: 32614910      PMCID: PMC7332030          DOI: 10.1371/journal.pone.0235695

Source DB:  PubMed          Journal:  PLoS One        ISSN: 1932-6203            Impact factor:   3.240


Fig 3 appears in black and white rather than in color. Please see the correct Fig 3 here. The publisher apologizes for the error.
Fig 3

FTIR analyses comparing the differences between resin, copal and amber produced by Hymenaea spp. and Canarium madagascariensis.

(A) FTIR analyses of the samples in order to identify the tree-resin producer of “Madagascar copal”, include (see Table 1): Canarium madagascariensis and two samples of “Madagascar copal” (CM01 and CM02), two samples of resin from H. verrucosa branches (RHvA01-R1 and RHvA02-R0). (B) Malagasy H. verrucosa analyses: FTIR analyses that show the comparison between the results of A and other resin, copal and amber produced by Hymenaea ssp. The analyses include samples of Canarium madagascariensis (RMCR-01), “Madagascar copal” (CM01), resin from H. verrucosa branch, (RHvA01-R1), resin from H. verrucosa of the Andranotsara pit Q1, found in A horizon A (CM05-Q1) and in the sub-horizon B1 (CM06-Q1), and resin pieces of H. verrucosa of the Antampolo pit Q2, found in A horizon (CM03-Q2) and in sub-horizon B1 (CM4-Q2). (C) Neotropical Hymenaea spp. resin and amber analyses: resin from “copal of Colombia”, (CCS01), Miocene Mexican amber (AMS01), Miocene Dominican amber (AD-03) and (AD-04), and Miocene Ethiopian amber (EA-01). Diterpenic resin/copal has some characteristic vibrational group frequencies: characteristic is a low intensity of absorption band at 3080 cm-1 that is absent from triterpenoid resin/copal and that corresponds to v (= C-H), intensity absorption band at 2937–2929 cm-1 corresponds to vas(C-H), CH3, CH2 (methylene group), intensity band at 2874–2844 cm-1 corresponds to vs (C-H), CH3, CH2 (methyl group), intensity bands at 1718 cm-1, 1694 cm-1, and 1644 cm-1 correspond to v (C = O), intensity band at 1446 cm-1 corresponds to δas (CH3), intensity band at 1386 cm-1 corresponds to δs (CH3), and intensity band at 888 cm-1 corresponds out of plane δ (CH2) of the exomethylene functionality C8-C20. “Madagascar copal” and “East African Copal” can be differentiated from “Western African Copal” by the linear slope of the spectra in the case of the resin/copal of West Africa and the intensity of 3411–3422 cm-1 that corresponds to v (OH) of the East African copal. It is possible to differentiate between amber and copal by observing the exocyclic methylene bands at 3048, 1642 and 887 cm-1. In the case of copal, the first two bands are not intense, but they are clearly observed, and the band of 887 cm-1 is very intense. In the case of ambers, the bands are absent or of very weak intensity.

FTIR analyses comparing the differences between resin, copal and amber produced by Hymenaea spp. and Canarium madagascariensis.

(A) FTIR analyses of the samples in order to identify the tree-resin producer of “Madagascar copal”, include (see Table 1): Canarium madagascariensis and two samples of “Madagascar copal” (CM01 and CM02), two samples of resin from H. verrucosa branches (RHvA01-R1 and RHvA02-R0). (B) Malagasy H. verrucosa analyses: FTIR analyses that show the comparison between the results of A and other resin, copal and amber produced by Hymenaea ssp. The analyses include samples of Canarium madagascariensis (RMCR-01), “Madagascar copal” (CM01), resin from H. verrucosa branch, (RHvA01-R1), resin from H. verrucosa of the Andranotsara pit Q1, found in A horizon A (CM05-Q1) and in the sub-horizon B1 (CM06-Q1), and resin pieces of H. verrucosa of the Antampolo pit Q2, found in A horizon (CM03-Q2) and in sub-horizon B1 (CM4-Q2). (C) Neotropical Hymenaea spp. resin and amber analyses: resin from “copal of Colombia”, (CCS01), Miocene Mexican amber (AMS01), Miocene Dominican amber (AD-03) and (AD-04), and Miocene Ethiopian amber (EA-01). Diterpenic resin/copal has some characteristic vibrational group frequencies: characteristic is a low intensity of absorption band at 3080 cm-1 that is absent from triterpenoid resin/copal and that corresponds to v (= C-H), intensity absorption band at 2937–2929 cm-1 corresponds to vas(C-H), CH3, CH2 (methylene group), intensity band at 2874–2844 cm-1 corresponds to vs (C-H), CH3, CH2 (methyl group), intensity bands at 1718 cm-1, 1694 cm-1, and 1644 cm-1 correspond to v (C = O), intensity band at 1446 cm-1 corresponds to δas (CH3), intensity band at 1386 cm-1 corresponds to δs (CH3), and intensity band at 888 cm-1 corresponds out of plane δ (CH2) of the exomethylene functionality C8-C20. “Madagascar copal” and “East African Copal” can be differentiated from “Western African Copal” by the linear slope of the spectra in the case of the resin/copal of West Africa and the intensity of 3411–3422 cm-1 that corresponds to v (OH) of the East African copal. It is possible to differentiate between amber and copal by observing the exocyclic methylene bands at 3048, 1642 and 887 cm-1. In the case of copal, the first two bands are not intense, but they are clearly observed, and the band of 887 cm-1 is very intense. In the case of ambers, the bands are absent or of very weak intensity.
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1.  Unravelling the mystery of "Madagascar copal": Age, origin and preservation of a Recent resin.

Authors:  Xavier Delclòs; Enrique Peñalver; Voajanahary Ranaivosoa; Mónica M Solórzano-Kraemer
Journal:  PLoS One       Date:  2020-05-18       Impact factor: 3.240

  1 in total

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