Facultad de Química

Ma. Fernanda Lases Hernández

Departamento: Unidad Sisal
   Perfil: Profesores-Investigadores
 Nombramiento: Profesor de Carrera Asociado

 
 

Publicaciones recientes
 
 

Travis-Taylor, L.*, Medina-Elizalde, M., Karmalkar, A. V., Polanco-Martìnez, J. M., Serrato Marks,, G., Burns, S., Lases-Hernández, F., & McGee, D. (2023). Last glacial hydroclimate variability in the Yucatán Peninsula not just driven by ITCZ shifts. Scientific Reports, 13(1).
DOI:10.1038/s41598-023-40108-6

Bernal, J. P.*, Revolorio, F., Cu-Xi, M., Lases-Hernández, F., Piacsek, P., Lachniet, M. S., Beddows, P. A., Lucia, G., López-Aguiar, K., Capella-Vizcaíno, S., López-Martínez, R., & Vásquez, O. J. (2023). Variability of trace-elements and δ18O in drip water from gruta del rey marcos, guatemala; seasonal and environmental effects, and its implications for paleoclimate reconstructions. Frontiers in Earth Science, 11.
DOI:10.3389/feart.2023.1112957

Medina‐Elizalde, M.*, Perritano, S., DeCesare, M., Polanco‐Martinez, J., Lases‐Hernandez, F., Serrato‐Marks, G. & McGee, D. (2022). Southeastern United States Hydroclimate During Holocene Abrupt Climate Events: Evidence From New Stalagmite Isotopic Records From Alabama. Paleoceanography and Paleoclimatology, 37(2).
DOI:10.1029/2021pa004346

Serrato Marks, G.*, Medina‐Elizalde, M., Burns, S., Weldeab, S., Lases‐Hernandez, F., Cazares, G. & McGee, D. (2021). Evidence for Decreased Precipitation Variability in the Yucatán Peninsula During the Mid‐Holocene. Paleoceanography and Paleoclimatology, 36(5).
DOI:10.1029/2021pa004219

Lases-Hernández, F.*, Medina-Elizalde, M. & Benoit Frappier, A. (2020). Drip water δ18O variability in the northeastern Yucatán Peninsula, Mexico: Implications for tropical cyclone detection and rainfall reconstruction from speleothems. Geochimica et Cosmochimica Acta, 285, 237-256.
DOI:10.1016/j.gca.2020.07.008

Lases-Hernandez, F.*, Medina-Elizalde, M., Burns, S. & DeCesare, M. (2019). Long-term monitoring of drip water and groundwater stable isotopic variability in the Yucatán Peninsula: Implications for recharge and speleothem rainfall reconstruction. Geochimica et Cosmochimica Acta, 246, 41-59.
DOI:10.1016/j.gca.2018.11.028

Medina-Elizalde, M.*, Burns, S. J., Polanco-Martinez, J., Lases-Hernández, F., Bradley, R., Wang, H. C. & Shen, C. C. (2017). Synchronous precipitation reduction in the American Tropics associated with Heinrich 2. Scientific Reports, 7(1).
DOI:10.1038/s41598-017-11742-8

Medina-Elizalde, M.*, Polanco-Martínez, J. M., Lases-Hernández, F., Bradley, R. & Burns, S. (2016). Testing the “tropical storm” hypothesis of Yucatan Peninsula climate variability during the Maya Terminal Classic Period. Quaternary Research, 86(2), 111-119.
DOI:10.1016/j.yqres.2016.05.006

Medina-Elizalde, M.*, Burns, S. J., Polanco-Martínez, J. M., Beach, T., Lases-Hernández, F., Shen, C. C. & Wang, H. C. (2016). High-resolution speleothem record of precipitation from the Yucatan Peninsula spanning the Maya Preclassic Period. Global and Planetary Change, 138, 93-102.
DOI:10.1016/j.gloplacha.2015.10.003

 

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