There was an error published in Limnology and Oceanography, 2017, 62 (5), pages: 1963–1983.

The equation of the regression line reported in the caption of Fig. 5 was carried over from an earlier version of the manuscript and presents a unit discrepancy in the coefficient and intercept, and an error in the decimal of the intercept.

The unit discrepancy was due to different unit used in the earlier version of the manuscript, in which the regression line was calculated using DOC In in μmol L⁻¹ and DOC uptake in nmol s⁻¹ (cm sponge)⁻². While in the published Fig. 5 DOC uptake is in μmol s⁻¹ (cm sponge)⁻². Therefore, the coefficient and intercept of the regression line should be corrected and divided by 1000.

The corrected equation follows: y = 0.00006x–0.00429, R² = 0.63, p < 0.001.

The final numbers for DOC flux estimates remain unchanged and there are no changes to the results and conclusions of the paper. The authors apologize for any inconvenience this may have caused.

有发表在错误湖沼学和海洋学，2017年，62（5），页：1963年至1983年。

图5的标题中报告的回归线方程式是从较早版本的手稿中继承下来的，它表示系数和截距的单位差异，以及截距的十进制误差。

单位差异是由于在早期版本的手稿中使用了不同的单位，其中回归线是使用mol In ^-1中的DOC In和nmol s ^-1（cm海绵）^-2中的DOC吸收来计算的。而在已发布的图5中，DOC的吸收量为μmols ^-1（cm海绵）^-2。因此，应校正回归线的系数和截距并将其除以1000。

校正后的公式如下：y = 0.00006x–0.00429，R ² = 0.63，p  <0.001。

DOC通量估计的最终数字保持不变，并且论文的结果和结论没有变化。对于由此带来的任何不便，作者深表歉意。