Erratum: The rise and fall of methanotrophy following a deepwater oil-well blowout
Erratum: The rise and fall of methanotrophy following a deepwater oil-well blowout
复制标题
勘误表:深水油井井喷后甲烷氧化菌的兴衰
DOI:
10.1038/ngeo2447
复制
发表时间:
2015
影响因子:
18.3
通讯作者:
Chanton, J. P.
中科院分区:
文献类型:
--
作者:
Crespo-Medina, M.;Meile, C. D.;Hunter, K. S.;Diercks, A-R.;Asper, V. L.;Orphan, V. J.;Tavormina, P. L.;Nigro, L. M.;Battles, J. J.;Chanton, J. P.
The special circumstances of the Deepwater Horizon oil-well blowout required adaptation of standard operating procedures. As a result, methane oxidation rate assays on 248 of the 1,128 samples we took in our study were not initiated within 12–24 hours of sample collection (Supplementary Table 1), because some cruises lacked a radioisotope isolation van and samples had to be shipped to the University of Georgia for processing after the cruise ended. Specifically, on the RV Pelican, RV Walton Smith, RV Arctic Sunrise, and the RV Nancy Foster cruises, samples were stored for up to 29 days before initiation of rate assays. Sample storage times for these cruises are given in Supplementary Table 1.To evaluate potential issues arising from storage and shipping, we measured the concentration of dissolved oxygen and nutrients on the ship and after storage, and bottles were visually inspected for gas bubbles, and visible changes (for example, turbidity, aggregations) in microbial biomass. On board the ship, samples were stored without a headspace in a gas-tight bottle in a refrigerator set at 4 C. The temperature of the refrigerator was checked at least every four hours to assure stability. We prepared samples for shipment to Athens (Georgia, USA) by placing them on a layer of Styrofoam peanuts (∼ 2.5 cm thick), which overlaid a layer of blue ice packs. Similarly, blue ice packs lined the sides of each cooler and were separated from the sample bottles by cardboard. A piece of cardboard was placed on top of the samples, and an ice pack was then placed on top of the cardboard. No warming occurred during shipment and samples remained at deep-sea temperatures (3–4 C) until arrival in Athens.