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Titlebook: Lake Kinneret; C. Serruya Book 1978 Dr W. Junk bv Publishers The Hague 1978 Fauna.algae.benthic.energy balance.environment.phytoplankton.p

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發(fā)表于 2025-3-21 18:31:24 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Lake Kinneret
編輯C. Serruya
視頻videohttp://file.papertrans.cn/581/580494/580494.mp4
叢書(shū)名稱Monographiae Biologicae
圖書(shū)封面Titlebook: Lake Kinneret;  C. Serruya Book 1978 Dr W. Junk bv Publishers The Hague 1978 Fauna.algae.benthic.energy balance.environment.phytoplankton.p
描述Fauna and flora oflakes are an integrative result of regional past history and present environmental factors. In the Lake Kinneret area where Prehistoric Man witnessed the last tectonic readj ustments of the Rift Valley, geological events do not belong only to the remote past but still strongly affect the lacustrine environment. It is therefore necessary to give a detailed picture of the regional background and limnological features of the lake (Parts I and II) before describing its planktic and benthic com- munities (Parts III and IV) and the Vertebrate fauna of the lake and its surroundings (Part V). The trophic relationships between communities are beyond the scope of a Monograph and have consequently not been studied in detail but only mentioned occasionally. It is intentional that Man and his penetration into the Kinneret area have been treated on a purely zoological basis. It underlines the fact that Man, as any other living organism, is part of the ecosystem and ruled by its laws and that his activities have an automatic feed back on his environment. However, in contrast with other living organisms, Man is able to ‘utilize‘ the lakes and their watersheds for his benefit if,
出版日期Book 1978
關(guān)鍵詞Fauna; algae; benthic; energy balance; environment; phytoplankton; plankton; porifera; temperature; zooplankt
版次1
doihttps://doi.org/10.1007/978-94-009-9954-1
isbn_softcover978-94-009-9956-5
isbn_ebook978-94-009-9954-1Series ISSN 0077-0639 Series E-ISSN 2215-1729
issn_series 0077-0639
copyrightDr W. Junk bv Publishers The Hague 1978
The information of publication is updating

書(shū)目名稱Lake Kinneret影響因子(影響力)




書(shū)目名稱Lake Kinneret影響因子(影響力)學(xué)科排名




書(shū)目名稱Lake Kinneret網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Lake Kinneret網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Lake Kinneret被引頻次




書(shū)目名稱Lake Kinneret被引頻次學(xué)科排名




書(shū)目名稱Lake Kinneret年度引用




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地板
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GeologyThe geological history of Israel was determined by the position of the area between the Precambrian Arabo—Nubian crystalline massif in the south and the pre-Mediterranean Sea in the north and west.
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發(fā)表于 2025-3-22 10:36:40 | 只看該作者
HydrologyThe Jordan Valley is the inland drainage with the lowest base level in the world (400 m below sea level at the Dead Sea). Lake Hula and Lake Kinneret represent intermediary base levels. Lake Kinneret drains a catchment area of 2,730 km. from an altitude of 2,800 m (Mount Hermon) down to a base level of 209 m below MSL.
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發(fā)表于 2025-3-22 16:05:23 | 只看該作者
The Physical environmentThe first observations concerning light penetration date back to Barrois who, in April 1873, noted that the transparency of Kinneret water was considerably limited by numerous particles of algal origin.
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BacteriaThe ecology of bacteria in natural waters is a recent field of study. After the pioneer work of Waksman, ZoBell and Wood in marine environment and of Kuznetsov in lakes, the study of the role of bacteria in chemical transformations in seas and lakes became a popular subject.
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發(fā)表于 2025-3-23 02:42:25 | 只看該作者
The benthic faunaNo systematic work has been done on the Protozoa. The following data come from a preliminary survey carried out in the littoral zone.
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發(fā)表于 2025-3-23 07:42:41 | 只看該作者
Vertical distribution of benthic faunaThe zonation of the benthic fauna has been described by Por (1968). This author distinguished five main faunal zones (Fig. 121).
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