根据其组合特征可划分五个孢粉组合带。
According to the composition features, they can be devided into 5 pollen components.
浙江金衢盆地白垩系红层，共发现二个化石孢粉组合。
Two fossil spore-pollen assemblages are found in the Cretaceous red beds of Jin Ju Basin, Chekiang Province.
在南海北部陆架，这一孢粉组合可与WS1-3-1井流沙港组三段孢粉组合对比，时代为早始新世。
On the northern shelf of South China Sea, the latter assemblage can only be compared with the third member of Liushagang Formation in the WS1-3-1 well, Beibu Gulf Basin.
孢粉化石组合的变化显示当时出现暖湿至干热气候条件的演变。
The assemblage variation of spore and pollen indicates a change from warm humid to dry hot climates.
作者首次比较完整地介绍了赤峰盆地早白垩世岩石地层层序及孢粉化石组合序列，并对各地层单元的区域对比关系和地质时代归属进行了简要讨论。
Comparatively it is the first time that the stratigraphic sequence in Chifeng Basin is introduced completely in this paper, and the spore-pollen assemblages have been set up.
[王开发，张玉兰。宁波平原晚第四纪沉积的孢粉、藻类组合及其古地理。地理科学，1985，5（2）：145-151。]。
Wang Kaifa, Zhang Yulan. Palynological assemblages from the late Quaternary sediments of Ningbo Plain in Zhejiang Province and its paleogeography. Scientia Geographica Sinica, 1985,5(2):145-151.
[王开发，张玉兰。宁波平原晚第四纪沉积的孢粉、藻类组合及其古地理。地理科学，1985，5（2）：145-151。]。
Wang Kaifa, Zhang Yulan. Palynological assemblages from the late Quaternary sediments of Ningbo Plain in Zhejiang Province and its paleogeography. Scientia Geographica Sinica, 1985,5(2):145-151.
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