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地衣石果衣中次生菌丝体生长的实验研究。

Experimental studies of hypothallus growth in the lichen Rhizocarpon geographicum.

作者信息

Armstrong R A, Smith S N

机构信息

Vision Sciences, Aston University, Birmingham, UK.

Pharmaceutical and Biological Sciences, Aston University, Birmingham, UK.

出版信息

New Phytol. 1996 Jan;132(1):123-126. doi: 10.1111/j.1469-8137.1996.tb04517.x.

Abstract

Removal of the areolae of the crustose lichen Rhizocarpon geographicum (L.) DC. resulted in either low or no measurable radial growth of the marginal hypothallus. Radial growth of the hypothallus was also significantly reduced compared with intact thalli when (I) aerolae were removed to within 1 and 2 mm of the hypothallus and (2) a 5 mm wide 'moat' was created between the areolae and the hypothallus. Adding ribitol (0.01 M) to isolated hypothalli at 3-month intervals over 15 months resulted in total radial growth c. 60% that of intact thalli. Adding an arabitol/mannitol mixture (0.05 M arabitol, 0.03 M mannitol) increased radial growth compared with deionized water and ribitol treatments. Adding ribitol (0.7M), arabitol (0.2 M) and mannitol (0.08 M) to the areolae of intact thalli had no significant effects on radial growth of the hypothallus. On a south-facing rock surface, isolated hypothalli grew at a similar rate to intact thalli for 2 months. Growth then declined and the hypothalli disappeared from the rock surface within 6 months. The effects of addition of carbohydrate suggests that the marginal hypothallus has the capacity to utilize exogenous materials. However, in intact thalli in the field, the radial growth of the hypothallus is likely to be a result of transfer of materials from the areolae through hyphal connections.

摘要

去除地衣型壳状地衣地图衣(Rhizocarpon geographicum (L.) DC.)的子囊盘后,边缘下皮层的径向生长要么很低,要么无法测量。当(1)将子囊盘去除至距下皮层1毫米和2毫米以内,以及(2)在子囊盘和下皮层之间形成一条5毫米宽的“护城河”时,与完整的地衣体相比,下皮层的径向生长也显著降低。在15个月内每隔3个月向分离的下皮层添加核糖醇(0.01 M),导致总的径向生长约为完整地衣体的60%。与去离子水和核糖醇处理相比,添加阿拉伯糖醇/甘露醇混合物(0.05 M阿拉伯糖醇,0.03 M甘露醇)可增加径向生长。向完整地衣体的子囊盘添加核糖醇(0.7 M)、阿拉伯糖醇(0.2 M)和甘露醇(0.08 M)对下皮层的径向生长没有显著影响。在朝南的岩石表面,分离的下皮层在2个月内的生长速度与完整地衣体相似。然后生长下降,下皮层在6个月内从岩石表面消失。添加碳水化合物的影响表明边缘下皮层有能力利用外源物质。然而,在野外完整的地衣体中,下皮层的径向生长可能是物质通过菌丝连接从子囊盘转移的结果。

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