山东苔藓植物新记录

报道了山东苔藓植物地理分布新记录科1种，新记录属11个，新记录种48个，新记录变种2个。     

山东省莱州湾地区海水入侵成因分析

七十年代以来，我国北方沿海地区，尤其是环渤海经济区的山东、河北、辽宁等省区的沿海地带逐渐显露出这一态势：由海水入侵引起的生态环境恶化、工农业发展受阻和人畜的饮水短缺及人民健康状况下降等问题突出。本以山东省莱州湾沿岩为例，分析了海水入侵的成因，为进一步研究防治对策和综合经济发展规划有重要意义。     

山东苔藓植物研究(Ⅰ)

本文报导了中国新记录藓类植物5种;山东新记录苔藓植物184种,其中苔类植物50种,藓类植物134种。     

《金瓶梅》鲁南方言俗语例释

以北方官话为基础写成的《金瓶梅》，吸收了大量山东方言和俗语，这已为《金》学界所公认。作为土生土长的鲁南人，我更明显地感到书中还有不少典型的鲁南方言、俗语没有为研究者和《金瓶梅辞典》等书所注意，或者虽有解释但却欠准确，可能培读者准确地理解原文带来不便。故个人不揣浅瓶，列举部分条目，予以例释。     

山东肥城晚石炭世苔藓虫新知

通过对山东肥城矿区晚石炭世苔藓虫的进一步研究,又发现了以往在山东乃至华北未曾报道过的苔藓虫化,属隐口目中的两个科,计有两属六种,其中新种四个,近似种两个,进一步丰富了山东乃至华北石炭纪的苔藓虫化石资料。     

台儿庄大战之后

山东省枣庄市台儿庄大战五十周年国际学术研讨会暨大战纪念馆落成典礼筹委会，先后三次来信，告知大会筹备情况，《致台儿庄大战参战将士及其亲属的信》，并希望提供有关台儿庄大战的历史资料，十分高兴，欣喜，遂即将在各报刊发表的几篇文章寄去，受到筹委会负责人朱崇礼先生的称赞，实在感谢了。     

南四湖自然资源优势与开发问题

南四湖是微山湖、南阳湖、独山湖和昭阳湖的简称，行政区划上属山东省徽山县，其南北长126公里，东西最宽处25公里，最窄处5公里，面积1266平方公里。1960年二级坝建成后，分南四湖为上级湖和下级湖，上级湖包括南船湖、独山湖和昭阳湖，下级湖包括微山湖。     

齐鲁文学精魂与俄罗斯文学血脉的叠合

山东文学和俄罗斯文学在精神意蕴和思想内涵上具有很大的相似性：对道德理想的崇敬,文化守成主义思想,底层关怀和人道主义等。     

Noble gases in corundum megacrysts from the basalts in Changle, Shandong Province, eastern China

This study presents noble gaseous data of the corundum megacrysts from the Cenozoic basalts in Changle, Shandong Province, eastern China. It is known that no noble gaseous data of corundum megacryst have been documented before. The 3He/4He ratios (1.13-7.37 Ra) of the corundums from Changle vary from atmosphere to MORB values; the 20Ne/22Ne (9.67-10.75) and 21Ne/22Ne (0.0280-0.0372) data define two linear trends on Ne three-isotope diagram, respectively, along the MFL and the correlation line between atmosphere and MORB; the 38Ar/36Ar (0.177-0.194) ratios, the 40Ar/36Ar (280.9 -404.2) ratios and the 128-136Xe/132Xe ration with obvious 129Xe excess are generally higher than at-mospheric component, but the 40Ar/36Ar ratios are much closer to atomospheric ratio. The isotopic compositions of noble gases (particularly for He and Ar) of the corundums are similar to those of py-roxene, anorthoclase megacrysts, and mantle-derived xenoliths from this area, and those of man-tle-derived xenoliths from several areas in eastern China. Therefore, the noble gases trapped in the corundums probably are from mantle source, representing a ‘mixed fluid' produced by the interaction between the lithospheric mantle and fluids releasing from the convective plate. Both the noble gas isotopic compositions and the oxygen isotopic compositions of the solid corundums are not the characteristics of crustal source. These suggest that the corundums crystallized from mantle-derived magmas with minimal crustal contamination.