Cerrar

No. de sistema: 000059782

LDR _ _ 00000naa^^22^^^^^za^4500
008 _ _ 200122s2019^^^^sz^^^^^fr^^^^z000^0^eng^d
040 _ _ a| ECO
c| ECO
043 _ _ a| n-mx---
044 _ _ a| sz
100 1 _ a| Torrescano Valle, Nuria
e| autora
245 1 0 a| Introduction
b| the holocene and anthropocene environmental history of Mexico
500 _ _ a| Para consultar el capítulo véase el libro con la clasificación EE 577 H6, en SIBE-Campeche, SIBE-Chetumal, SIBE-San Cristóbal
506 _ _ a| Disponible para usuarios de ECOSUR con su clave de acceso
520 _ _ a| The Holocene spans the last 11,700 years of Earth’s history, and the paleoecology and paleoclimate dynamics of Mexico over this interval were complex. This is apparent when considering the region’s ecological and physiographic diversity, as well as human impact since the Late Holocene. The geography of Mexico varies from desert to high mountain systems, indicating conspicuous precipitation and temperature variability on latitudinal and altitudinal scales. More than one-third of Mexico’s territory is classified as arid or subarid. This area receives more than 60% of its total annual precipitation during the warm season through the North American Monsoon (NAM) and tropical storm systems, and significant winter precipitation occurs only in its northwestern margin. The Anthropocene is the latest part of the Holocene and it is marked by an era of substantial human activity. Climate change during this interval is not exclusively driven by natural processes, as humans have been influencing shifts in the global climate. Several climate projections predict that anthropogenic global warming will cause further enhancement in aridity in this drought-prone region by increasing the mean temperature and reducing the average annual rainfall in the near future. Other areas of Mexico are projected to receive less annual precipitation or the same amount but in shorter time periods. Ultimately, the knowledge of Holocene environmental change can provide society with clues for conservation, management, and adaptation of Mexico’s diverse environments.
530 _ _ a| Disponible en línea
533 _ _ a| Reproducción electrónica en formato PDF
538 _ _ a| Adobe Acrobat profesional 6.0 o superior
650 _ 4 a| Paleoecología
650 _ 4 a| Historia ambiental
650 _ 4 a| Cambio climático
650 _ 4 a| Antropoceno
650 _ 4 a| Cuaternario
651 _ 4 a| México
651 _ 4 a| Mesoamérica
700 1 _ a| Islebe, Gerald A.
c| Doctor
e| autor
700 1 _ a| Roy, Priyadarsi Debajyoti
e| autor
773 0 _
t| The holocene and anthropocene environmental history of Mexico: a paleoecological approach on Mesoamerica / editors: Nuria Torrescano Valle, Gerald A. Islebe, Priyadarsi D. Roy
d| Cham, Switzerland : Springer International Publishing, 2019
g| página 1-5
z| 978-3-030-31718-8
900 _ _ a| Solicítelo con su bibliotecario/a
901 _ _ a| Capítulo de libro con arbitraje
902 _ _ a| JSGM / GOG
904 _ _ a| Enero 2020
905 _ _ a| Artecosur
906 _ _ a| Producción Académica ECOSUR
LNG eng
Cerrar
*Solicítelo con su bibliotecario/a
Introduction: the holocene and anthropocene environmental history of Mexico
Torrescano Valle, Nuria (autora)
Islebe, Gerald A. (autor)
Roy, Priyadarsi Debajyoti (autor)
Nota: Para consultar el capítulo véase el libro con la clasificación EE 577 H6, en SIBE-Campeche, SIBE-Chetumal, SIBE-San Cristóbal.
Nota: Disponible en línea
Disponible para usuarios de ECOSUR con su clave de acceso
Contenido en: The holocene and anthropocene environmental history of Mexico: a paleoecological approach on Mesoamerica / editors: Nuria Torrescano Valle, Gerald A. Islebe, Priyadarsi D. Roy. Cham, Switzerland : Springer International Publishing, 2019. página 1-5. ISBN: 978-3-030-31718-8
Bibliotecas:
Campeche , Chetumal , San Cristóbal
No. de sistema: 59782
Tipo: - Capítulo de libro con arbitraje
PDF
  • Consulta (1)




Español

"The Holocene spans the last 11,700 years of Earth’s history, and the paleoecology and paleoclimate dynamics of Mexico over this interval were complex. This is apparent when considering the region’s ecological and physiographic diversity, as well as human impact since the Late Holocene. The geography of Mexico varies from desert to high mountain systems, indicating conspicuous precipitation and temperature variability on latitudinal and altitudinal scales. More than one-third of Mexico’s territory is classified as arid or subarid. This area receives more than 60% of its total annual precipitation during the warm season through the North American Monsoon (NAM) and tropical storm systems, and significant winter precipitation occurs only in its northwestern margin. The Anthropocene is the latest part of the Holocene and it is marked by an era of substantial human activity. Climate change during this interval is not exclusively driven by natural processes, as humans have been influencing shifts in the global climate. Several climate projections predict that anthropogenic global warming will cause further enhancement in aridity in this drought-prone region by increasing the mean temperature and reducing the average annual rainfall in the near future. Other areas of Mexico are projected to receive less annual precipitation or the same amount but in shorter time periods. Ultimately, the knowledge of Holocene environmental change can provide society with clues for conservation, management, and adaptation of Mexico’s diverse environments."

SIBE Campeche
Codigo de barra
Estado
Colección
59782-30
(Disponible)
Artículos de investigación ECOSUR
SIBE Chetumal
Codigo de barra
Estado
Colección
59782-20
(Disponible)
Artículos de investigación ECOSUR
SIBE San Cristóbal
Codigo de barra
Estado
Colección
59782-10
(Disponible)
Artículos de investigación ECOSUR

  • Adobe Acrobat profesional 6.0 o superior