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Krunica Hruška 《Folia Geobotanica》1985,20(3):225-243
A survey of the nitrophilous fringe communities of the region Marche (Central Italy) allows the individualization of five associations well characterized floristically and ecologically. These are:Urtico-Aegopodietum, Anthriscetum sylvestris, Chaerophylletum aurei, Alliario-Chaerophylletum temuli, andAnthriscetum nemorosae. The first three associations are ranged, from the phytosociological point of view, in the allianceAegopodion podagrariae, while the last two belong to the allianceGalio-Alliarion. 相似文献
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Résumé analytique Dans la région de Yangambi-Stanleyville, les pentes sableuses ou gréseuses sèches ensoleillées (falaises, talus, déblais) sont colonisées par l'association à Dicranopteris linearis (Gleichenietum linearis ass. nov.) se décomposant en une phase initiale à dominance de bryophytes et d'algues et une phase optimale à dominance de ptéridophytes dans laquelle abonde Dicranopteris linearis accompagné d'espèces pionnières des groupements forestiers de terre ferme.
Reçu par la rédaction le 12.XII.1953. 相似文献
Summary In the region of Yangambi-Stanleyville, the sandy dry and sunny slopes (cliff, digging) are colonized by the Dicranopteris linearis association (Gleichenietum linearis ass. nov.) which falls into two phases: an initial with bryophytes and algae and an optimal one with predominance of pteridophytes, chiefly Dicranopteris linearis accompanied by various pioneer forest species.
Reçu par la rédaction le 12.XII.1953. 相似文献
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《Geobios》1988,21(1):49-63
enTwo sections have been analysed: San Onofrequarry and Pliocene deposits from Tarragona E2 hole which is biostratigraphically subdivided according to planktonic foraminifera. A latitudinal floristic differentiation is evidenced for South-Western European Lower Pliocene. The increasing open vegetation in the coastal plain is to be related to high xericity. 相似文献
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《Comptes rendus de l'Académie des sciences. Série III, Sciences de la vie》1999,322(8):651-655
We have found a relationship between the net absorption of carbon at time t divided by the net absorption of carbon in 24 h (AN(t)/AN(24)) and the incubation duration after sunrise, in surface waters of the western Mediterranean sea. This ratio is quite similar whatever the sample location, the sample depth and the 24-h net-absorption level. Considering this result, we have established a correction factor which may be used to convert primary production rates obtained from incubation durations ≤ 24 h to daily rates (24 h dawn-to-dawn). 相似文献
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