Lateglacial and Holocene palaeoenvironments at Sierra La Madera, northwestern Mexico: Sharp signals of Younger Dryas and North American monsoon
During the last glacial termination, the climate system experienced intense global variations whose causes and impacts are not fully defined, particularly for low latitudes. The northwestern Mexico Sky Islands present a climate‐sensitive ideal setting to record palaeoecological and palaeoclimatic ch...
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| Published in: | Journal of quaternary science Vol. 38; no. 1; pp. 76 - 91 |
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| Abstract | During the last glacial termination, the climate system experienced intense global variations whose causes and impacts are not fully defined, particularly for low latitudes. The northwestern Mexico Sky Islands present a climate‐sensitive ideal setting to record palaeoecological and palaeoclimatic changes due to their physiographic complexity and location in the ecotone between temperate and tropical ecosystems. High‐resolution pollen analysis and a detailed sedimentological study were conducted at the Ciénega Tonibabi tropical thorn scrub site. The 15 540–0 cal a bp nearly continuous record shows that the North Atlantic Ocean did have a cold and humid climatic influence during the glacial stages of the end of the Pleistocene, including a sharp pulse during the Younger Dryas. However, a shift to the Pacific Ocean influence occurred during the Holocene, which led to the development of the El Niño conditions prevailing today. Colder and warmer phases follow one another with higher or lower winter precipitation, including a sharp Bølling–Allerød and development and intensification of the North American monsoon. They are reflected in hydrological changes as well as in the advances, retreats and intermingling of coniferous forests and tropical thorn scrub. |
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| AbstractList | During the last glacial termination, the climate system experienced intense global variations whose causes and impacts are not fully defined, particularly for low latitudes. The northwestern Mexico Sky Islands present a climate‐sensitive ideal setting to record palaeoecological and palaeoclimatic changes due to their physiographic complexity and location in the ecotone between temperate and tropical ecosystems. High‐resolution pollen analysis and a detailed sedimentological study were conducted at the Ciénega Tonibabi tropical thorn scrub site. The 15 540–0 cal a bp nearly continuous record shows that the North Atlantic Ocean did have a cold and humid climatic influence during the glacial stages of the end of the Pleistocene, including a sharp pulse during the Younger Dryas. However, a shift to the Pacific Ocean influence occurred during the Holocene, which led to the development of the El Niño conditions prevailing today. Colder and warmer phases follow one another with higher or lower winter precipitation, including a sharp Bølling–Allerød and development and intensification of the North American monsoon. They are reflected in hydrological changes as well as in the advances, retreats and intermingling of coniferous forests and tropical thorn scrub. During the last glacial termination, the climate system experienced intense global variations whose causes and impacts are not fully defined, particularly for low latitudes. The northwestern Mexico Sky Islands present a climate‐sensitive ideal setting to record palaeoecological and palaeoclimatic changes due to their physiographic complexity and location in the ecotone between temperate and tropical ecosystems. High‐resolution pollen analysis and a detailed sedimentological study were conducted at the Ciénega Tonibabi tropical thorn scrub site. The 15 540–0 cal a bp nearly continuous record shows that the North Atlantic Ocean did have a cold and humid climatic influence during the glacial stages of the end of the Pleistocene, including a sharp pulse during the Younger Dryas. However, a shift to the Pacific Ocean influence occurred during the Holocene, which led to the development of the El Niño conditions prevailing today. Colder and warmer phases follow one another with higher or lower winter precipitation, including a sharp Bølling–Allerød and development and intensification of the North American monsoon. They are reflected in hydrological changes as well as in the advances, retreats and intermingling of coniferous forests and tropical thorn scrub. |
| Author | Flores‐Castro, Kinardo Galaz‐Samaniego, Carlos Alberto Paz‐Moreno, Francisco Abraham Peñalba, M. Cristina Monreal, Rogelio Lizárraga‐Celaya, Carlos Espinoza‐Encinas, Iván Rosario |
| Author_xml | – sequence: 1 givenname: Carlos Alberto orcidid: 0000-0002-6118-7820 surname: Galaz‐Samaniego fullname: Galaz‐Samaniego, Carlos Alberto organization: Universidad de Sonora, Maestría en Ciencias‐Geología, Departamento de Geología, Hermosillo – sequence: 2 givenname: M. Cristina orcidid: 0000-0001-9781-0592 surname: Peñalba fullname: Peñalba, M. Cristina email: cristina.penalba@unison.mx organization: Universidad de Sonora, Departamento de Investigaciones Científicas y Tecnológicas, Hermosillo – sequence: 3 givenname: Francisco Abraham surname: Paz‐Moreno fullname: Paz‐Moreno, Francisco Abraham organization: Universidad de Sonora, Departamento de Geología, Hermosillo – sequence: 4 givenname: Iván Rosario surname: Espinoza‐Encinas fullname: Espinoza‐Encinas, Iván Rosario organization: Universidad de Sonora, Departamento de Geología, Hermosillo – sequence: 5 givenname: Kinardo surname: Flores‐Castro fullname: Flores‐Castro, Kinardo organization: Universidad Autónoma del Estado de Hidalgo, Ciencias de la Tierra y Materiales, Pachuca – sequence: 6 givenname: Rogelio surname: Monreal fullname: Monreal, Rogelio organization: Universidad de Sonora, Departamento de Geología, Hermosillo – sequence: 7 givenname: Carlos surname: Lizárraga‐Celaya fullname: Lizárraga‐Celaya, Carlos organization: Universidad de Sonora, Departamento de Física, Hermosillo |
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| SubjectTerms | Climate Climate system Coniferous forests El Nino Glacial climates Holocene Humid climates Hydrology last glacial termination Monsoons North American monsoon Oceans palaeoclimate Paleoenvironments Pleistocene Pollen Pollen analysis Scrub Tropical forests Winter precipitation Younger Dryas |
| Title | Lateglacial and Holocene palaeoenvironments at Sierra La Madera, northwestern Mexico: Sharp signals of Younger Dryas and North American monsoon |
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