Bioavailability and molecular composition of dissolved organic matter from a diffuse hydrothermal system

被引:40
作者
Rossel, Pamela E. [1 ,2 ]
Stubbins, Aron [3 ]
Hach, Philipp F. [4 ]
Dittmar, Thorsten [2 ]
机构
[1] Alfred Wegener Inst Helmholtz Ctr Polar & Marine, HGF MPG Grp Deep Sea Ecol & Technol, D-27515 Bremerhaven, Germany
[2] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm ICBM, Res Grp Marine Geochem ICBM MPI Bridging Grp, D-26129 Oldenburg, Germany
[3] Univ Georgia, Skidaway Inst Oceanog, Dept Marine Sci, Savannah, GA 31411 USA
[4] Max Planck Inst Microbiol Bremen, Biogeochem Grp, D-28359 Bremen, Germany
关键词
Diffusive hydrothermal systems; Dissolved organic matter; Chromophoric dissolved organic matter; Organic matter degradation; Labile; Recalcitrant; Fourier-transform ion cyclotron resonance mass spectrometry; MID-ATLANTIC RIDGE; CHEMICAL-COMPOSITION; FLUIDS; MASS; CARBON; PHOTOPRODUCTION; ABSORBENCY; BACTERIA; SEAWATER; BASALT;
D O I
10.1016/j.marchem.2015.07.002
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Fluids from the diffusive hydrothermal vent Woody located at the Menez Gwen hydrothermal field were collected directly from a fissure using a Kiel pumping system (KIPS). The fluids were incubated in a biodegradation experiment with the resident microbial community at in situ temperature (55 degrees C). In addition to the initial fluid (T-0), sub-samples were collected at three time points: 12.5 h (T-1), 38 h (T-2) and 180 h (T-final). Whole water samples were characterized by spectrophotometry and for dissolved organic carbon (DOC) and total dissolved nitrogen (TDN) concentrations. Solid-phase extracted dissolved organic matter (SPE-DOM) was molecularly characterized using a 15 Tesla Fourier-transform ion cyclotron resonance mass spectrometer (FT-ICR-MS). Based on Mg2+ concentrations, vent fluids were diluted ca. 1:99% with seawater. SPE-DOC concentrations remained constantly low (30 mu M) over the course of incubation, while DOC and TDN (1180 mu M and 16 mu M, respectively, at T-0) decreased sharply (to 80 mu M and 9 mu M, respectively, at T-final). This biolabile DOC is likely composed of volatiles and short-chain hydrocarbons, and the reason behind their extraordinarily high concentration remains unknown. Molecular characterization of SPE-DOM in fluids and seawater identified over 3000 molecular formulae, which were separated into different groups according to their reactivity. The half-life of the more reactive groups ranged between 6-7 h, 18-21 h and 5-106 days, and represented 7.3, 2.0 and 7.5% of the total formulae present in T-0, while the majority (83%) did not exhibit any significant trend during the experiment. Despite the small molecular changes in SPE-DOM, a decrease in the number of formulae and average molecular mass was observed, the latter consistent with an increase in the spectral slope over the wavelength range 275-295 nm (S275-295) during the experiment. An increase in aromatic molecular formulae during the incubation was also corroborated by a concurrent increase in the absorption coefficient at 254 nm normalized to DOC concentrations (SUVA(254)), an optical indicator of aromatic content. Thus both FT-ICR-MS and optical properties over the course of the incubation corroborated a decrease in molecular mass and increase in aromaticity. This study is the first to report the optical and molecular transformations of bio-labile DOM from diffusive hydrothermal systems. (C) 2015 Elsevier B.V. All rights reserved.
引用
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页码:257 / 266
页数:10
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