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1. Identity statement
Reference TypeJournal Article
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Sitemtc-m21c.sid.inpe.br (namespace prefix: upn:3Q3U5H8)
Identifier8JMKD3MGP3W34R/436TQDP
Repositorysid.inpe.br/mtc-m21c/2020/09.02.15.08   (restricted access)
Last Update2020:09.02.15.08.21 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2020/09.02.15.08.21
Metadata Last Update2022:01.04.01.35.21 (UTC) administrator
DOI10.1016/j.scitotenv.2020.140904
ISSN0048-9697
Citation KeyFreitasACCTGVCLBATT:2020:GlTrMi
TitleGlacial-interglacial transitions in microbiomes recorded in deep-sea sediments from the western equatorial Atlantic
Year2020
MonthDec.
Access Date2026, Nov. 08
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2134 KiB
2. Context
Author 1 Freitas, Lucas
 2 Appolinario, Luciana
 3 Calegario, Gabriela
 4 Campeão, Mariana
 5 Tschoeke, Diogo
 6 Garcia, Gizele
 7 Venâncio, Igor Martins
 8 Cosenza, Carlos A. N.
 9 Leomil, Luciana
10 Bernardes, Marcelo
11 Albuquerque, Ana Luiza
12 Thompson, Cristiane
13 Thompson, Fabiano
Group 1
 2
 3
 4
 5
 6
 7 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
Affiliation 1 Universidade Federal do Rio de Janeiro (UFRJ)
 2 Universidade Federal do Rio de Janeiro (UFRJ)
 3 Universidade Federal do Rio de Janeiro (UFRJ)
 4 Universidade Federal do Rio de Janeiro (UFRJ)
 5 Universidade Federal do Rio de Janeiro (UFRJ)
 6 Universidade Federal do Rio de Janeiro (UFRJ)
 7 Instituto Nacional de Pesquisas Espaciais (INPE)
 8 Universidade Federal do Rio de Janeiro (UFRJ)
 9 Universidade Federal do Rio de Janeiro (UFRJ)
10 Universidade Federal Fluminense (UFF)
11 Universidade Federal Fluminense (UFF)
12 Universidade Federal do Rio de Janeiro (UFRJ)
13 Universidade Federal do Rio de Janeiro (UFRJ)
Author e-Mail Address 1
 2
 3
 4
 5
 6
 7 igor.venancio@inpe.br
 8
 9
10
11 ana_albuquerque@id.uff.br
12 thompsoncristiane@gmail.com
13 fabianothompson1@gmail.com
JournalScience of the Total Environment
Volume746
Pagese140904
Secondary MarkA1_ZOOTECNIA_/_RECURSOS_PESQUEIROS A1_SAÚDE_COLETIVA A1_INTERDISCIPLINAR A1_GEOGRAFIA A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_ENGENHARIAS_I A1_ENFERMAGEM A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A1_CIÊNCIA_DE_ALIMENTOS A1_BIODIVERSIDADE A2_QUÍMICA A2_ODONTOLOGIA A2_MEDICINA_III A2_MEDICINA_II A2_MEDICINA_I A2_MATERIAIS A2_FARMÁCIA A2_ENGENHARIAS_II A2_CIÊNCIAS_BIOLÓGICAS_I A2_BIOTECNOLOGIA B1_CIÊNCIAS_BIOLÓGICAS_II B2_ASTRONOMIA_/_FÍSICA
Host Collectionurlib.net/www/2017/11.22.19.04 upn:3Q3U5H8
History (UTC)2020-09-02 15:08:21 :: simone -> administrator ::
2020-09-02 15:08:29 :: administrator -> simone :: 2020
2020-09-02 15:10:02 :: simone -> administrator :: 2020
2020-09-05 14:01:43 :: administrator -> simone :: 2020
2020-12-14 14:56:14 :: simone -> administrator :: 2020
2022-01-04 01:35:21 :: administrator -> simone :: 2020
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsMetagenomics
Sediment core
Bioindicator
Amazon river
Microbiome modulation
AbstractIn the late Quaternary, glacial-interglacial transitions are marked by major environmental changes. Glacial periods in the western equatorial Atlantic (WEA) are characterized by high continental terrigenous input, which increases the proportion of terrestrial organic matter (e.g. lignin, alkanes), nutrients (e.g. iron and sulphur), and lower primary productivity. On the other hand, interglacials are characterized by lower continental contribution and maxima in primary productivity. Microbes can serve as biosensors of past conditions, but scarce information is available on deep-sea sediments in the WEA. The hypothesis put forward in this study is that past changes in climate conditions modulated the taxonomic/functional composition of microbes from deep sediment layers. To address this hypothesis, we collected samples from a marine sediment core located in the WEA, which covered the last 130 kyr. This region is influenced by the presence of the Amazon River plume, which outputs dissolved and particulate nutrients in vast oceanic regions, as well as the Parnaiba river plume. Core GL-1248 was analysed by shotgun metagenomics and geochemical analyses (alkane, lignin, perylene, sulphur). Two clusters (glacial and interglacial-deglacial) were found based on taxonomic and functional profiles of metagenomes. The interglacial period had a higher abundance of genes belonging to several sub-systems (e.g. DNA, RNA metabolism, cell division, chemotaxis, and respiration) that are consistent with a past environment with enhanced primary productivity. On the other hand, the abundance of Alcanivorax, Marinobacter, Kangiella and aromatic compounds that may serve as energy sources for these bacteria were higher in the glacial. The glacial period was enriched in genes for the metabolism of aromatic compounds, lipids, isoprenoids, iron, and Sulphur, consistent with enhanced fluvial input during the last glacial period. In contrast, interglacials have increased contents of more labile materials originating from phytoplankton (e.g. Prochlorococcus). This study provides new insights into the microbiome as climatic archives at geological timescales.
AreaMET
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4. Conditions of access and use
Languageen
Target Filefreitas_glacial.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EUPEJL
Citing Item Listsid.inpe.br/bibdigital/2013/10.06.18.03 - 102
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX; SCOPUS.
6. Notes
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