A multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene (2015)
- Authors:
- USP affiliated authors: PESSENDA, LUIZ CARLOS RUIZ - CENA ; GIANNINI, PAULO CESAR FONSECA - IGC ; LORENTE, FLAVIO LIMA - CENA ; BUSO JUNIOR, ANTONIO ALVARO - CENA
- Unidades: CENA; IGC
- DOI: 10.1016/j.catena.2015.02.005
- Subjects: PALEOAMBIENTES; PALEOPALINOLOGIA; PALEOCLIMATOLOGIA; HOLOCENO
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Source:
- Este periódico é de acesso aberto
- Este artigo NÃO é de acesso aberto
-
ABNT
FRANÇA, Marlon Carlos et al. A multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene. Catena, v. 128, p. 155-166, 2015Tradução . . Disponível em: https://doi.org/10.1016/j.catena.2015.02.005. Acesso em: 13 fev. 2026. -
APA
França, M. C., Alves, I. C. C., Castro, D. F., Cohen, M. C. L., Rossetti, D., Pessenda, L. C. R., et al. (2015). A multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene. Catena, 128, 155-166. doi:10.1016/j.catena.2015.02.005 -
NLM
França MC, Alves ICC, Castro DF, Cohen MCL, Rossetti D, Pessenda LCR, Lorente FL, Fontes NA, Buso Júnior AA, Giannini PCF, Francisquini MI. A multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene [Internet]. Catena. 2015 ; 128 155-166.[citado 2026 fev. 13 ] Available from: https://doi.org/10.1016/j.catena.2015.02.005 -
Vancouver
França MC, Alves ICC, Castro DF, Cohen MCL, Rossetti D, Pessenda LCR, Lorente FL, Fontes NA, Buso Júnior AA, Giannini PCF, Francisquini MI. A multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene [Internet]. Catena. 2015 ; 128 155-166.[citado 2026 fev. 13 ] Available from: https://doi.org/10.1016/j.catena.2015.02.005 - Landscape evolution during the late Quaternary at the Doce River mouth, Espírito Santo state, southeastern Brazil
- Mangrove vegetation changes on Holocene terraces of the Doce River, southeastern Brazil
- Interdisciplinary studies of late Quaternary vegetation and marine dynamics and climate inferences on the Northern coast of Espirito Santo State, Southeastern Brazil
- Coastal wetland dynamics on the Delta of the Doce River during the middle to late Holocene, Southeastern Brazil
- Cold and humid Atlantic Rainforest during the last glacial maximum, northern Espírito Santo state, southeastern Brazil
- Millennial to secular time-scale impacts of climate and sea-level changes on mangroves from the Doce River delta, Southeastern Brazil
- Atlas palinológico: laboratório 14C - CENA/USP = Palynological atlas: 14C laboratory - CENA/USP
- Palynofacies and stable C and N isotopes of Holocene sediments from Lake Macuco (Linhares, Espírito Santo, southeastern Brazil): depositional settings and palaeonvironmental evolution
- Análise de palinofácies e interpretação paleoambiental de sedimentos lacustres da costa norte do Espírito Santo
- Genesis and variation spatial of Podzol in depressions of the Barreiras Formation, northeastern Espírito Santo State, Brazil, and its implications for Quaternary climate change
Informações sobre o DOI: 10.1016/j.catena.2015.02.005 (Fonte: oaDOI API)
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