[an error occurred while processing this directive] ������� 2010, 29(1) 1-10 DOI:     ISSN: 1004-5589 CN: 22-1111/P

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PubMed
Article by Yu, T.
Article by Zhou, Z. Z.
Article by Yue, C.
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Ӧ�ù�ѧ��΢���Խ����������Ϸ��^������24��ֲ�ﻨ����̬�����˹۲���о�,�������:�������ʳ���������������,P/Eֵ������С�Ļ��۷ֱ�Ϊ˿��(Yucca smalliana Fern.)�͹�(Osmanthus fragrans(Thunb.)Lour.);������Ļ���Ϊ˿��(Luffa cylindrica (L.) Roem.),��С��Ϊ�㻱(Cladrastis wilsonii Takeda.)�����۵��ȷ�����Ҫ�е�����3��6����������ɢ�������׹���2��4�׼�ɢ�׵�6������,�����������Ҫ������״��ϸ��״������״������״�����ƴ��׵�5�����͡����о�Ϊ���۷ֲ����ṩ�˵���λ��(31°31′��32°37′N,116°40′��117°52′E)�����θ߶�(70��20 m)���꽵ˮ��(900��1 000 mm)��≥10��������(4 500��5 300��)����Ҫ��̬���ӡ�

�ؼ����� ����������   �˹�ֲ��   ������̬   ��ֲ��   ������  
Palynomorphs and ecological factors of autumn bloom ing plants in Jianghua i hilly region
1. School of Life Science, Anhui University, Hefei 230039, China; 2.Key Laboratory of Ecological Engineering and Biotechnology of Anhui Province
Abstract:

The Palynomorphs of 24 autumn blooming p lants from J ianghuai hilly region are described and il2
lustrated by lightmicroscope (LM). The results show that the pollen grains are globose to long globular in shape.
The maximum and minimum P /E values are Yucca sm alliana Fern. and Osm anthus fragrans ( Thunb. ) Lour. The maximum pollen grain is Luffa cylindrica (L. ) Roem. , and the minimum is Clad rastis w ilson ii Takeda. The types of apertures include monosulcate, 3��6 colpate, irregular pantocolpate, tricolporate, 2��4 porate and pantoporate. The ornamentation of exine are sp inulose, finely reticulate, coarsely reticulate, granular and stripe2perforated. The present study p rovides the main ecological factors, including geographical position (31°31′��32°37′N, 116°40′��117°52′E) , altitude (70��20 m) , annual p recip itation (900��1 000 mm ) and annual accumulated temperature of ≥10�� (4 500��5 300 ��) for the distribution area.

Keywords: J ianghuai hilly region   artificial vegetation   pollen morphology   paleovegetation   paleoclimate  
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