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Free-living Plathelminthes constitute an important component of meiobenthic communities in various marine benthic environments, but research focusing on this group is generally scarce. The current study investigated the free-living interstitial flatworms of the shallow sandy sublittoral zone of the southern Baltic coast. Sediment samples were taken at Hel Peninsula at water depths of 1.5 m and 7 m, and the plathelminths were identified alive to the species level. In total, 22 species were identified. The majority of the species belonged to Kalyptorhynchia and Proseriata, but Acoela recently moved from Plathelminthes into their own phyllum and represented by Mecynostomidae, was the most numerous group. The average total plathelminth densities ranged between 6 and 74 ind. 10 cm–2. The vertical distribution of the plathelminth fauna in the sediments was usually limited to the upper 3–4 cm, except for acoels which penetrated deeper into the sediment layers. The role of both sediment water saturation and oxygen availability appeared to be the main factors limiting flatworm occurrence in the sediments investigated in this study.
The purpose of presented study was determination of the impact of selected physicochemical parameters, strongly influencing the soil biological life: water potential (pF), oxygen availability for microorganisms (ODR), redox potential (Eh), content of Mg, Ca and total organic carbon (TOC) on soil DNA concentration. Undisturbed loess soil material was taken to metal cylin-ders (100 cm3) from four depths (0-20; 20-40; 40-60 and 60-80 cm), what make possibility for description of DNA content and its distribution in the whole soil profile. Our results revealed signif-icant (p<0.05) positive relationships between soil DNA content and measured values of ODR (r = 0.94***), Eh (r = 0.52**) and TOC (r = 0.98***), what were confirmed by high values of correla-tion coefficients (r). Whereas, significant negative interrelationships between soil DNA and pF (r = –0.57*) or Mg content (r = –0.79***) were determined. However, in the current experiment condi-tions, we did not found significant correlation between Ca presence and DNA content (p>0.05). Significant (p<0.05) decrease of DNA concentration by 62.8% with an increase of soil depth was noted, what was undoubtedly connected with spatial distribution of microorganisms in the soil profile and its likes for surface layers colonization.
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