Internal transformation and damming regulate the longitudinal variation of DOM bioavailability in a large river.

Understanding the spatial patterns of dissolved organic matter (DOM) and factors that influence them is crucial for maintaining river ecosystem functions and riverine health, considering the significant role of DOM in water quality and aquatic ecosystems. Nevertheless, there is limited knowledge regarding the spatial variation of DOM bioavailability and the factors driving them in large river systems. This study involved 39 sampling locations along the main stem of the Changjiang River, spanning its entire length (>5000 km) during a dry season. Spatial patterns of DOM were assessed by measurements of DOC concentrations and eight fluorescence DOM indices, namely fluorescence index (FI-A and FI-B), Trytophan/Tyrosine, Humic A, Humic C, humification indices (HIX-A and HIX-B), and Freshness index (ß/α). The results revealed that the water DOM in the main stem of the Changjiang River primarily originated from terrestrial sources. A decline in DOM bioavailability was observed from the upper to the lower basin, aligning with the carbon processing prediction rather than the river continuum concept (RCC). The pure effect of physicochemical factors (25.30%) was greater than that of geographic factors (9.40%). The internal transformation processes determined the significant longitudinal decreases of DOM bioavailability. While no significant difference in DOM bioavailability was observed between reaches before and after the dams, the construction of dams was found to improve DOM bioavailability at the subsection scale and reduce the spatial autocorrelation of DOM bioavailability across the entire basin.

Exponential decay of between-month spatial dissimilarity congruence of phytoplankton communities in relation to phosphorus in a highland eutrophic lake.

Phytoplankton species composition has long been recognized to be structured by environmental filtering, but our knowledge of patterns of spatial dissimilarity congruence between the phytoplankton community and environmental divers is rather limited. Specifically, a study on whether there are specific temporal properties that could be more related to spatial dissimilarity remains to be seen. We examined the extent to how spatial dissimilarity changed with seasonal succession by measuring ß-diversity in phytoplankton communities in Lake Erhai (from January 2012 to December 2014 at 15 sampling sites) as a function of different period conditions (high-density period and low-density period). We found that congruences of spatial dissimilarity in algal communities over time were neither stable in time nor showed a seasonal pattern. The spatial dissimilarity congruence between the phytoplankton community and dissolved inorganic phosphorus (DIP) concentration followed exponential decay patterns, and this congruence was led by algal cell density. This result implies that species and functions of phytoplankton are specialized, and DIP concentration drastically increases in high-density periods than in low-density periods. This means that DIP enrichment is related to the loss of algal diversity and functions and the increase of algal biomass in eutrophic lakes.