Titlebook: Vegetation history; B. Huntley,T. Webb Book 1988 Kluwer Academic Publishers 1988 Polle.Vegetation.climate.climate change.environment.flora

concession

書目名稱Vegetation history影響因子(影響力)




書目名稱Vegetation history影響因子(影響力)學(xué)科排名




書目名稱Vegetation history網(wǎng)絡(luò)公開度




書目名稱Vegetation history網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Vegetation history被引頻次




書目名稱Vegetation history被引頻次學(xué)科排名




書目名稱Vegetation history年度引用




書目名稱Vegetation history年度引用學(xué)科排名




書目名稱Vegetation history讀者反饋




書目名稱Vegetation history讀者反饋學(xué)科排名

Verify

Australasiae’s zoogeographical region, Australia (Tivy, 1971). A map of the region incorporating the geological and Wallace’s boundaries appears as Fig. 1. Included here is part of south-east Asia to the west of the defined region which will be considered in discussion of floristic relationships and interchange during the period under discussion.

muffler

先行

Late-tertiary and quaternary palaeoenvironmentsf the atmosphere and lithosphere. The aim of this chapter is to describe the climate system and the controls of its variations, and to examine those timescales of climatic variations that are of relevance to vegetation history.

鈍劍

容易懂得

Ancient permanent plots: Sampling in paleovegetational studiesances in both the techniques and the cumulative findings of paleoecology. As Prentice (1985) has pointed out, pollen analysis is a method of vegetation sampling and description. Notable recent results have provided plant ecologists with telling insights about the modern population distributions of s

Pigeon

Records of vegetation in time and space: the principles of pollen analysisas a record of the response of ecosystems to human impacts in history and prehistory, as a rich source of information about natural vegetation dynamics, and as the only empirical evidence for the behaviour of plant taxa and assemblages when subjected to major climatic and environmental changes. Many

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凹室

連累

Late-tertiary and quaternary palaeoenvironmentsa context for viewing and interpreting many of the vegetational variations recorded by paleoecological data. Climate variations occur at all temporal and spatial scales. At one end of the spectrum they include interannual variations at a particular place that are related to variations in atmospheric