SciELO - Scientific Electronic Library Online

 
vol.29 issue3A Cenomanian aipichthyoid fish (Teleostei, Acanthomorpha) from America, Zoqueichthys carolinae gen. and sp. nov. from El Chango quarry (Cintalapa Member, Sierra Madre Formation), Chiapas, MexicoEnviromental change and vegetation responses during the last 17,000 years in central Mexico: The lake Zirahuén record author indexsubject indexsearch form
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

Related links

  • Have no similar articlesSimilars in SciELO

Share


Revista mexicana de ciencias geológicas

On-line version ISSN 2007-2902Print version ISSN 1026-8774

Abstract

GUTIERREZ-AYALA, Luz Verónica; TORRESCANO-VALLE, Nuria  and  ISLEBE, Gerald Alexander. Late Holocene paleoecological reconstruction of the Los Petenes reserve, Yucatán Peninsula, México. Rev. mex. cienc. geol [online]. 2012, vol.29, n.3, pp.749-763. ISSN 2007-2902.

Changes in climate and ecological dynamics of the Biosphere Reserve of Los Petenes, located in northwestern Yucatan Peninsula, were identified through high-resolution pollen analysis of a core of 2.2 m depth. The reconstruction of the history of vegetation, hydrology and climate that occurred during the last 4000 years was based on fossil pollen analysis, total organic carbon (TOC) and calcium carbonate (CaCO3). The results show changes in the stratigraphy and the percentage of mangrove elements, wich are interpreted as rapid increases in sea level during the middle to late Holocene transition (4095 - 3100 cal BP). From 3000 cal year BP, considerably decreases of mangroves and changes in COT, suggest a strong hydrological variability. Increase of the tropicalforest and disturbance elements shows changes in the distribution of vegetation. The landscape is dominate by tropical forest and secondary vegetation. The accumulation of gastropods and foraminifera, reveals marine transgressions, and periods of deacresed precipitation and sea level. High percentages in the carbonate signal (12, 20 and 40%), mangrove elements and fungal spores decrease, disturbance elements and Cyperaceae increase, indicating around 600 cal dC, the decrease in precipitation and climatic deterioration is significant. The changes, coincide with changes in other circumcaribbean signals, associated with the Medieval Warming and the minimum of solar activity, recorded during the Little Ice Age. The paleoenvironmental record provides information about the environmental history of RBLP, establishing bases for understanding ecological processes and the implications they may have for conservation.

Keywords : climate variability; Late Holocene; Los Petenes; Yucatan Peninsula; fossil pollen; sea level.

        · abstract in Spanish     · text in Spanish     · Spanish ( pdf )

 

Creative Commons License All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License