Titlebook: Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington; Daniel G. Gavin,Linda B. Brubaker Book 2015 Sprin

T-cell

书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington影响因子(影响力)




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington影响因子(影响力)学科排名




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington网络公开度




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington网络公开度学科排名




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington被引频次




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington被引频次学科排名




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington年度引用




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington年度引用学科排名




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington读者反馈




书目名称Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington读者反馈学科排名

addict

样式

Brain-Waves

Late Quaternary Vegetation and Fire History of the Olympic Peninsula how they are linked mechanistically is a major goal of Earth system science. Advances are made when there is intensive development of paleo-records and mechanistic models. The Olympic Peninsula has the potential to be such a location, as the area has received attention from the pioneering years of

显而易见

Brief Review of the Archeological Record in a Context of Environmental Changein the Americas is found in the Pacific Northwest. In this very brief chapter, we examine the correlation of dates of important archeological sites with the well-dated events of the paleoenvironmental record described in Chap. 4. We give special consideration to relative sea-level history, and to th

轻快来事

Insights and Future Research Needsthis region should also provide some new findings. The very steep precipitation gradient, the general lack of human influence on Holocene vegetation (as occurs in Europe), and the important role of an episodic fire regime allow for researchers to infer complex interactions within the scope of changi

同步左右

Late Pleistocene and Holocene Environmental Change on the Olympic Peninsula, Washington

browbeat

Postglacial Climate on the Olympic Peninsulaavoided in this chapter because they are responses to climate change and may lag behind actual climate changes by more than 100 years. In contrast, other proxies of climate, such as the temperature tolerances of beetles or midges or the isotopic composition of carbonates, should respond with much sh

coltish

Late Quaternary Vegetation and Fire History of the Olympic Peninsulatern Washington and southwest British Columbia, is presented through mapped pollen data. This taxon-level analysis provides a view into climatic gradients of the past and suggests modern analogs for periods, such as the late-glacial, that have been difficult to interpret from single sites.

引导