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在向沼泽过渡的潮汐淡水森林湿地中,地下生产力因评估技术、植被类型和养分供应情况而异。

Belowground productivity varies by assessment technique, vegetation type, and nutrient availability in tidal freshwater forested wetlands transitioning to marsh.

机构信息

U.S. Geological Survey, Wetland and Aquatic Research Center, Lafayette, Louisiana, United States of America.

U.S. Geological Survey, Florence Bascom Geoscience Center, Reston, Virginia, United States of America.

出版信息

PLoS One. 2021 Jul 16;16(7):e0253554. doi: 10.1371/journal.pone.0253554. eCollection 2021.

Abstract

Wetlands along upper estuaries are characterized by dynamic transitions between forested and herbaceous communities (marsh) as salinity, hydroperiod, and nutrients change. The importance of belowground net primary productivity (BNPP) associated with fine and coarse root growth also changes but remains the dominant component of overall productivity in these important blue carbon wetlands. Appropriate BNPP assessment techniques to use in various tidal wetlands are not well-defined, and could make a difference in BNPP estimation. We hypothesized that different BNPP techniques applied among tidal wetlands differ in estimation of BNPP and possibly also correlate differently with porewater nutrient concentrations. We compare 6-month and 12-month root ingrowth, serial soil coring techniques utilizing two different calculations, and a mass balance approach (TBCA, Total Belowground Carbon Allocation) among four tidal wetland types along each of two river systems transitioning from freshwater forest to marsh. Median values of BNPP were 266 to 2946 g/m2/year among all techniques used, with lower BNPP estimation from root ingrowth cores and TBCA (266-416 g/m2/year), and higher BNPP estimation from serial coring of standing crop root biomass (using Smalley and Max-Min calculation methods) (2336-2946 g/m2/year). Root turnover (or longevity) to a soil depth of 30 cm was 2.2/year (1.3 years), 2.7/year (1.1 years), 4.5/year (0.9 years), and 1.2/year (2.6 years), respectively, for Upper Forest, Middle Forest, Lower Forest, and Marsh. Marsh had greater root biomass and BNPP, with slower root turnover (greater root longevity) versus forested wetlands. Soil porewater concentrations of NH3 and reactive phosphorus stimulated BNPP in the marsh when assessed with short-deployment BNPP techniques, indicating that pulses of mineralized nutrients may stimulate BNPP to facilitate marsh replacement of forested wetlands. Overall, ingrowth techniques appeared to represent forested wetland BNPP adequately, while serial coring may be necessary to represent herbaceous plant BNPP from rhizomes as marshes replace forested wetlands.

摘要

上游河口的湿地以盐度、水期和养分变化为特征,森林和草本群落(沼泽)之间存在动态过渡。细根和粗根生长相关的地下净初级生产力(BNPP)的重要性也会发生变化,但仍然是这些重要蓝碳湿地整体生产力的主要组成部分。在各种潮汐湿地中使用的适当 BNPP 评估技术尚未明确定义,并且可能会对 BNPP 估算产生影响。我们假设,在潮汐湿地中应用的不同 BNPP 技术在 BNPP 的估算上存在差异,并且可能与孔隙水养分浓度的相关性也不同。我们比较了沿两条河流系统的四个潮汐湿地类型中,6 个月和 12 个月的根内生长、使用两种不同计算方法的连续土壤取样技术以及总地下碳分配(TBCA)之间的差异。使用的所有技术中 BNPP 的中值为 266 至 2946 g/m2/年,根内生长芯和 TBCA(266-416 g/m2/年)的 BNPP 估算值较低,而使用 Smalley 和 Max-Min 计算方法的立茬根生物量连续取样(2336-2946 g/m2/年)的 BNPP 估算值较高。到 30 cm 土壤深度的根周转率(或寿命)分别为 2.2/年(1.3 年)、2.7/年(1.1 年)、4.5/年(0.9 年)和 1.2/年(2.6 年),分别为上林、中林、下林和沼泽。与森林湿地相比,沼泽具有更大的根生物量和 BNPP,以及较慢的根周转率(更长的根寿命)。当使用短期 BNPP 技术评估时,土壤孔隙水中的 NH3 和反应性磷会刺激沼泽中的 BNPP,表明矿化养分的脉冲可能会刺激 BNPP 以促进沼泽取代森林湿地。总体而言,内生长技术似乎可以充分代表森林湿地的 BNPP,而连续取芯技术可能有必要代表根茎草本植物的 BNPP,因为沼泽取代了森林湿地。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bea9/8284669/6e036f9c4818/pone.0253554.g001.jpg

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