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Metadados

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/449CFUE
Repositóriosid.inpe.br/mtc-m21c/2021/03.02.16.05   (acesso restrito)
Última Atualização2021:03.02.16.05.34 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2021/03.02.16.05.34
Última Atualização dos Metadados2022:04.03.22.28.11 (UTC) administrator
DOI10.1016/j.geomorph.2021.107648
ISSN0169-555X
Chave de CitaçãoRodriguesCLPYRRSD:2021:EfGlWa
TítuloThe effect of global warming on the establishment of mangroves in coastal Louisiana during the Holocene
Ano2021
MêsMay
Data de Acesso02 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3576 KiB
2. Contextualização
Autor1 Rodrigues, Erika
2 Cohen, Marcelo C. L.
3 Liu, Kam-biu
4 Pessenda, Luiz C. R.
5 Yao, Qiang
6 Ryu, Junghyung
7 Rossetti, Dilce de Fátima
8 Souza, Adriana de
9 Dietz, Marianne
Identificador de Curriculo1
2
3
4
5
6
7 8JMKD3MGP5W/3C9JGTQ
Grupo1
2
3
4
5
6
7 DIOTG-CGCT-INPE-MCTI-GOV-BR
Afiliação1 Universidade Federal do Pará (UFPA)
2 Universidade Federal do Pará (UFPA)
3 Louisiana State University
4 Universidade de São Paulo (USP)
5 Louisiana State University
6 Louisiana State University
7 Instituto Nacional de Pesquisas Espaciais (INPE)
8 Universidade Federal do Pará (UFPA)
9 Louisiana State University
Endereço de e-Mail do Autor1
2 mcohen@ufpa.br
3
4
5
6
7 dilce.rossetti@inpe.br
RevistaGeomorphology
Volume381
Páginase107648
Nota SecundáriaA1_INTERDISCIPLINAR A1_GEOGRAFIA A1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2021-03-02 16:05:34 :: simone -> administrator ::
2021-03-02 16:05:36 :: administrator -> simone :: 2021
2021-03-02 16:06:41 :: simone -> administrator :: 2021
2022-04-03 22:28:11 :: administrator -> simone :: 2021
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chaveanthropocene
Avicennia
isotopes
palynology
port fourchon
ResumoWinter temperature and sea-level position are critical factors affecting the global distribution of mangroves and saltmarshes. The replacement of saltmarshes by mangroves is expected due to global warming, reflecting the long-term natural trends in the Holocene and anthropogenic impacts since the 20th century. We documented the Holocene history of wetlands dynamics in the boreal limits of the American mangroves, located at Bay Champagne, Louisiana (USA), by integrating sedimentological, palynological, geochemical (δ13C and C\N), X-ray fluorescence (XRF) data, and radiocarbon chronology from two sediment cores. The results indicated a freshwater lake environment with herbs and wetland ferns, as well as C3 terrestrial plants, between ~8100 and ~6500 cal yr BP. This environment shifted into a lagoon and saltmarshes having sedimentary organic matter sourced from marine algae between ~6500 and ~1500 cal yr BP. In the final stage, washover sediments were deposited in the lagoon during the last ~1500 cal yr BP. Despite the increased marine influence over the last ~6500 cal yr BP, mangrove pollen were not recorded between ~8100 and ~1500 cal yr BP, suggesting that mangroves were absent in the study area during that time interval. Historical evidence and a comparative analysis of our multi-proxy data with other mangrove studies from the Gulf of Mexico, Caribbean, and eastern South America revealed a gradual mangrove expansion from tropical to subtropical coasts of South and North America during the mid-late Holocene. The mangrove colonies at their current boreal (29° 09′ N) and austral (28° 29′ S) limits were established in the early and mid-20th century, respectively. This mangrove dynamics on a continental scale suggests that the poleward mangrove migration was likely caused by the warming climate during the Holocene. More importantly, the industrial-era warming has likely accelerated the mangrove expansion, but it was not the primary force that drove the mangrove migration into temperate zones.
ÁreaSRE
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4. Condições de acesso e uso
Idiomaen
Arquivo AlvoRodrigues_effect.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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