| 1. Identity statement | |
| Reference Type | Journal Article |
| Site | mtc-m16d.sid.inpe.br |
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identifier | 8JMKD3MGP7W/36JTHQ5 |
| Repository | sid.inpe.br/mtc-m19@80/2009/12.17.13.53 (restricted access) |
| Last Update | 2010:09.20.13.02.55 (UTC) marciana |
| Metadata Repository | sid.inpe.br/mtc-m19@80/2009/12.17.13.53.17 |
| Metadata Last Update | 2021:02.12.13.48.17 (UTC) administrator |
| Secondary Key | INPE--PRE/ |
| DOI | 10.1016/j.palaeo.2009.08.004 |
| ISSN | 0031-0182 |
| Citation Key | MirandaRossRuiz:2009:FaDeC1 |
| Title | Quaternary paleoenvironments and relative sea-level changes in Marajo Island (Northern Brazil): Facies, delta C-13, delta N-15 and C/N  |
| Year | 2009 |
| Month | Nov |
| Access Date | 2024, May 18 |
| Secondary Type | PRE PI |
| Number of Files | 1 |
| Size | 1310 KiB |
| 2. Context | |
| Author | 1 Miranda, Maria Carolina Da Cruz 2 Rossetti, Dilce De Fatima 3 Ruiz Pessenda, Luiz Carlos |
| Resume Identifier | 1 2 8JMKD3MGP5W/3C9JGTQ |
| Group | 1 2 DSR-OBT-INPE-MCT-BR |
| Affiliation | 1 Universidade de São Paulo-USP, Instituto de Geociências, Rua do Lago, 562, 05508-080 São Paulo, SP, Brazil 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Universidade de São Paulo, Laboratório de 14C, Avenida Centenário 303, 13416000 Piracicaba, SP – Brazil |
| Journal | Palaeogeography, Palaeoclimatology, Palaeoecology |
| Volume | 282 |
| Number | 1 |
| Pages | 19-31 |
| Secondary Mark | A1_CIÊNCIAS_BIOLÓGICAS_I A2_ECOLOGIA_E_MEIO_AMBIENTE A2_GEOCIÊNCIAS A1_GEOGRAFIA A1_INTERDISCIPLINAR A2_SAÚDE_COLETIVA |
| History (UTC) | 2010-01-12 10:56:09 :: marciana -> administrator :: 2010-05-11 01:03:01 :: administrator -> marciana :: 2010-09-20 13:02:55 :: marciana -> administrator :: 2012-07-15 03:40:33 :: administrator -> marciana :: 2009 2013-03-05 11:57:06 :: marciana -> administrator :: 2009 2021-02-12 13:48:17 :: administrator -> marciana :: 2009 |
| 3. Content and structure | |
| Is the master or a copy? | is the master |
| Content Stage | completed |
| Transferable | 1 |
| Content Type | External Contribution |
| Version Type | publisher |
| Keywords | Sedimentary facies Carbon and nitrogen isotopes Relative sea level Tectonics Estuary Late Quaternary nitrogen isotope composition georgia salt-marsh organic-matter carbon-isotope stable carbon environmental-changes early diagenesis estuary ratios sediments |
| Abstract | The reconstruction of physical environments of Amazonian areas is of great interest to determine the dynamic evolution of the Amazon drainage basin. However. few studies have emphasized the Quaternary deposits in this region. which is mostly due to the lack of natural exposures imposed by the low topography. This work integrates facies analysis. radiocarbon dating, delta C-13, delta N-15, and C/N of an 124 m-thick core from an area located at the mouth of the Amazon River. northeastern Amazonia. The study records deposits up to 50.795 C-14 yr B P. in age. which formed in a variety of depositional environments including fluvial channel, tidal flat, outer estuarine basin to shallow marine. inner estuarine basin, estuarine channel and lagoon. Facies interpretation was significantly improved with the inclusion of delta C-13, delta N-15, and C/N analyses of organic matter extracted from the sediments The obtained values conform to a transitional. mostly estuarine paleosetting evolved during successive relative sea-level fluctuations. The results suggest fluvial deposition between 40,950 (+/- 590) and 50.795 C-14 yr B P, with a rise in relative sea level that commenced between 35,567 (+/- 649) and 39,079 (+/- 1114) C-14 yr B P. An overall transgression took place until 29,340 (+/- 340) C-14 yr B P., after which the relative sea level dropped, favoring valley rejuvenation and incision. Following this time up to 10,479 (+/- 34) C-14 yr B.P. a rise in relative sea level filled up the valley with estuarine deposits After 10.479(+/- 34) C-14 yr B.P., the estuary was replaced by a lagoon At the end of the Holocene, the coastline prograided approximately 45 km northward, replaci ng the lagoon by a lake system Despite the influence of eustatic fluctuations. regional tectonics played a significant role to create new space where these Late Pleistocene and Holocene sediments accumulated. (C) 2009 Elsevier B V All rights reserved. |
| Area | SRE |
| Arrangement | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Quaternary paleoenvironments and... |
| doc Directory Content | access |
| source Directory Content | there are no files |
| agreement Directory Content | there are no files |
| 4. Conditions of access and use | |
| Language | en |
| Target File | miranda.pdf |
| User Group | administrator marciana |
| Visibility | shown |
| Archiving Policy | denypublisher denyfinaldraft24 |
| Read Permission | deny from all and allow from 150.163 |
| Update Permission | not transferred |
| 5. Allied materials | |
| Mirror Repository | sid.inpe.br/mtc-m19@80/2009/08.21.17.02.53 |
| Next Higher Units | 8JMKD3MGPCW/3ER446E |
| URL (untrusted data) | 10.1016/j.palaeo.2009.08.004 |
| Dissemination | WEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX. |
| Host Collection | sid.inpe.br/mtc-m19@80/2009/08.21.17.02 |
| 6. Notes | |
| Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress electronicmailaddress format isbn label lineage mark nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork |
| 7. Description control | |
| e-Mail (login) | marciana |
| update | |