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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
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Repositóriosid.inpe.br/mtc-m21c/2019/12.10.11.42
Última Atualização2021:02.23.13.52.53 (UTC) simone
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Chave SecundáriaINPE--PRE/
Chave de CitaçãoGonçalvesDiVeLeMuMaLu:2019:MiChBe
TítuloMillennial-Scale Changes in Benthic Foraminifera Stable Carbon Isotope Gradients in the Western Equatorial Atlantic
Ano2019
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho77 KiB
2. Contextualização
Autor1 Gonçalves, Caio Souza
2 Dias, Bruna B.
3 Venancio, Igor Martins
4 Lessa, Douglas Villela de Oliveira
5 Mulitza, Stefan
6 Mackensen, Andreas
7 Luiza, Albuquerque Ana
Grupo1
2
3 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 Universidade Federal Fluminense (UFF)
2 Universidade Federal Fluminense (UFF)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal Fluminense (UFF)
5 University of Bremen
6 Alfred Wegner Institute for Polar and Marine Research
7 Universidade Federal Fluminense (UFF)
Endereço de e-Mail do Autor1
2
3 igor.venancio@inpe.br
Nome do EventoAGU Fall Meeting
Localização do EventoSan Francisco, CA
Data09-13 dec.
Histórico (UTC)2019-12-10 11:42:50 :: simone -> administrator ::
2019-12-10 17:44:19 :: administrator -> simone :: 2019
3. Conteúdo e estrutura
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Transferível1
Tipo do ConteúdoExternal Contribution
ResumoThe stable carbon isotope ratio of benthic foraminifera (δ13C) is a widely applied proxy for ocean circulation and productivity changes, as the δ13C gradient between some species is linked to carbon export and bottom water oxygen concentration. Although there is some consensus about what could drive the variability of the oxygen concentration (such as the ocean circulation or the export of primary productivity), the mechanisms, especially in the Western Equatorial Atlantic (WEA), remain unexplained. To explore potential factors influencing bottom water [O2] over the last glacial period (63 to 29 kyr) in more detail, we analyzed the δ13C difference between three benthic foraminiferal species (Cibicides wuellerstorfi, Uvigerina peregrina, and Globobulimina affinis) from a site in the WEA. Our records demonstrate that the most prominent decreases in oxygen diffusion occurred during the Heinrich Stadials (HS) (especially HS3 and HS4) as a result of a reduced North Atlantic Deep Water (NADW) ventilation and increased fluvial terrigenous input. Our results show decreases in the strength of the bottom-water currents during these events, reflected by decreases in the sortable silt grain-size fraction (SS). Moreover, we show that the highest values of total organic carbon content (TOC) at our site during HS did not result from increased surface primary productivity but rather from continental input via the Parnaíba River. Furthermore, the highest TOC values are inconsistent with the gradient between two benthic foraminifera species (U. peregrina and C. wuellerstorfi), which reflects the low flux of labile organic carbon in the sediment. We suggest that the deposition and accumulation of terrigenous material reduced O2 diffusion into the sediment and, coupled with millennial-scale ventilation, played an important role in influencing the oxygen availability in the WEA during several HS over the last glaciation.
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5. Fontes relacionadas
Repositório Espelhourlib.net/www/2017/11.22.19.04.03
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 7
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
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