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No. de sistema: 000058968

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c| ECO
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245 0 0 a| Middle and late Holocene mangrove dynamics of the Yucatan Peninsula, Mexico
520 1 _ a| We present mangrove dynamics, related to precipitation changes derived from migration of the Intertropical Convergence Zone (ITCZ) and the El Niño Southern Oscillation (ENSO) during middle and late Holocene of the northern and southern Yucatan Peninsula. Sea level rise was the major determinant for mangrove establishment during middle Holocene. Following the sea level rate stabilization, changes in precipitation and increasing ENSO activity determined periods of expansion and reduction of mangrove cover. At the onset of late Holocene, mangroves fluctuated abruptly due the coupled effect of the ENSO and latitudinal movement of the ITCZ. Trend correlation analysis revealed significant relationship between the presence of Conocarpus erectus, ENSO and ITCZ. Rhizophora mangle showed a significant relationship with ITCZ based on trend correlation analysis. Expansion of mangrove populations in seasonally flooded wetlands is recorded during the late Holocene.
533 _ _ a| Reproducción electrónica en formato PDF
538 _ _ a| Adobe Acrobat profesional 6.0 o superior
650 _ 4 a| Manglares
650 _ 4 a| Conocarpus erectus
650 _ 4 a| Rhizophora mangle
650 _ 4 a| Polen
650 _ 4 a| Cuaternario
650 _ 4 a| Paleoclimatología
651 _ 4 a| Yucatán (Península) (México)
700 1 _ a| Aragón Moreno, Alejandro Antonio
700 1 _ a| Islebe, Gerald A.
c| Doctor
e| coaut.
700 1 _ a| Torrescano Valle, Nuria
e| coaut.
700 1 _ a| Arellano Verdejo, Javier
e| coaut.
773 0 _
t| Journal of South American Earth Sciences
g| Vol. 85 (August 2018), p. 307-311
x| 0895-9811
856 4 1 u| https://www.sciencedirect.com/science/article/pii/S0895981118300555
z| Artículo electrónico
901 _ _ a| Artículo con arbitraje
902 _ _ a| GOG / MM
904 _ _ a| Agosto 2018
905 _ _ a| Artecosur
905 _ _ a| Artfrosur
905 _ _ a| Biblioelectrónica
LNG eng
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Middle and late Holocene mangrove dynamics of the Yucatan Peninsula, Mexico
Aragón Moreno, Alejandro Antonio (autor)
Islebe, Gerald A. (autor)
Torrescano Valle, Nuria (autor)
Arellano Verdejo, Javier (autor)
Contenido en: Journal of South American Earth Sciences. Vol. 85 (August 2018), p. 307-311. ISSN: 0895-9811
No. de sistema: 58968
Tipo: - Artículo con arbitraje
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Inglés

"We present mangrove dynamics, related to precipitation changes derived from migration of the Intertropical Convergence Zone (ITCZ) and the El Niño Southern Oscillation (ENSO) during middle and late Holocene of the northern and southern Yucatan Peninsula. Sea level rise was the major determinant for mangrove establishment during middle Holocene. Following the sea level rate stabilization, changes in precipitation and increasing ENSO activity determined periods of expansion and reduction of mangrove cover. At the onset of late Holocene, mangroves fluctuated abruptly due the coupled effect of the ENSO and latitudinal movement of the ITCZ. Trend correlation analysis revealed significant relationship between the presence of Conocarpus erectus, ENSO and ITCZ. Rhizophora mangle showed a significant relationship with ITCZ based on trend correlation analysis. Expansion of mangrove populations in seasonally flooded wetlands is recorded during the late Holocene."


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