Мне нужна помощь в переводе нижеприведённого текста (это почти всё). Работа оплачивается.

Если кто-то силён в этих разделах биологии, то, пожалуйста, пришлите мне письмо с описанием своего опыта (или пришлите резюме) на адрес <37pqq55fcpip@mail.ru> (не пугайтесь, это адрес, сгенерированный анонимайзером, но с него почта попадёт прямо мне).
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CARBON IN DEEP ORGANIC-RICH LAKE TEMNOE AND ORGANIC-POOR LAKE SVETLOE OF THE EUROPEAN RUSSIAN SUBARCTIC

To reveal the degree of allochthonous vs. autochthonous control on carbon dynamics in deep boreal lakes, we studied two small (~0.1 km²) and deep (~ 40 m) contrasting seasonally stratified lakes located in the European subarctic zone (NW Russia, Arkhangelsk region) over a 2.5 yr period. The dissolved organic and inorganic carbon (DOC and DIC, respectively) concentrations were equal to 15–30 mg L-1 and 0.5–1.9 mg L-1 for humic lake and 0.8–4.3 mg L-1 and 18–52 mg L-1 for organic-poor lake, respectively. The DOC profile in the organic-poor lake was sensitive to phytoplankton blooms and May and July-August flooding, whereas the humic, organic-rich lake exhibited a highly stable system all over the year in both the epilimnion and hypolimnion, with significant (c.a., 40%) increase in DOC concentration in the hypolimnion relative to the epilimnion. The ratio of dissolved organic carbon to organic nitrogen (Corg/Norg) was significantly lower in the organic-poor lake, reflecting a strong impact of autochthonous Norg production and N diffusion from the sediment to the water column. There was a clear difference in the vertical pattern of the proportion of the low molecular weight (LMW< 1 kDa) organic carbon (OC) between the humic and the clear water lake. Regardless of season, the organic-poor lakes exhibited LMW< 1 kDa of 40–90%, whereas organic-rich lake recorded LMW< 1 kDa of 20 to 30%. This difference was most likely linked to the dominance of peat soil and bog providing allochthonous OC to the organic-rich lake throughout the year, and possible production of LMW autochthonous organic ligands by phytoplankton and photodegradation in the clear water lake. The important role of allochthonous organic matter (OM) in the color properties of the lake water was confirmed by the light absorbance in the visual range and specific ultraviolet absorption measurements. Overall, the deep humic lakes are expected to be less sensitive to external impacts and possible climate change. The evaluation of both number and depth of humic lakes in the boreal zone is crucial for assessing their CO2 emission and carbon storage potential.

А вот заголовок автор гуглем не переводил, и при переводе на русский получилась изрядная глупость: УГЛЕРОДА В ГЛУБОКОЙ ОРГАНИЧЕСКОМ ЯЗЫКЕ ТЕМНО И ОРГАНИЧЕСКОГО ЛЕКА СВЕТЛА ЕВРОПЕЙСКОЙ РОССИЙСКОЙ СУБАРКТИКИ
:)