Prokaryotic Microbial Diversity and Community Assembly in Reclaimed Coastal Agricultural Soils.

The results demonstrated that all three factors exhibited highly significant negative correlations with both archaeal and bacterial community similarity ( p < 0.001), indicating a typical distance-decay pattern.

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Homogeneous selection showed an increasing trend with reclamation years during two periods: 5–30 years and 70–530 years ( Figure 5 D).

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In reclaimed soils, Flavobacterium was the most dominant genus, its proportion showing an initial increase followed by a decreasing trend with the reclamation years.

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The soils exhibited a clear trend of desalination and eutrophication, characterized by increasing levels of TOC, TN, and AN, alongside decreasing pH and EC ( Figure 2 ), consistent with previous studies [ 9 , 10 ].

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With increasing reclamation year, soil particles showed a trend towards becoming finer.

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