Premium
Biogeochemical characteristics and hydroperiod affect carbon dioxide flux rates from exposed high‐elevation pond sediments
Author(s) -
DelVecchia Amanda Gay,
Gougherty Steven,
Taylor Brad W.,
Wissinger Scott A.
Publication year - 2021
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.1002/lno.11663
Subject(s) - biogeochemical cycle , sediment , environmental science , anoxic waters , hydrology (agriculture) , total organic carbon , flux (metallurgy) , temperate climate , ecology , environmental chemistry , geology , chemistry , geomorphology , biology , geotechnical engineering , organic chemistry
While inundated, small ponds (< 1000 m 2 area) account for disproportionately large contributions of CO 2 efflux to the global carbon budget and also store carbon in anoxic sediments. However, pond hydrology is shifting toward increasingly dry conditions in alpine and temperate zones, which might lead to increased exposure of shallow pond sediments. We analyzed sediment CO 2 efflux rates in dried sediments of multiple ponds of varying hydrology and sediment characteristics at montane and subalpine elevations near the Rocky Mountain Biological Laboratory in Colorado. Average CO 2 efflux rates from exposed sediments, 331.5 ± 11.5 mmol m −2 d −1 at the montane sites and 142.8 ± 45.1 mmol m −2 d −1 at the subalpine sites, were 10 times higher than average CO 2 efflux rates from pond water. Principal components analysis to reduce dimensionality of sediment characteristics revealed that random inter‐pond differences rather than exposure timing or hydroperiod drove variation among sediments. In linear mixed effects models of CO 2 flux rates, significant predictors included sediment moisture and temperature, pH, total organic carbon, and organic matter content at all pond hydroperiod classifications and sites. However, the sediment characteristics explaining the most variance differed among sites and hydroperiods and included nitrate concentrations, pH, bulk density, and temperature. We conclude that pond sediments are heterogeneous both within and among ponds in close proximity, and drivers of relatively high CO 2 efflux rates differ among pond hydroperiods and elevations. This work emphasizes that local differences can impact predictions of CO 2 flux from lentic sediments which are becoming increasingly exposed.