4.7 Article

Is a Central Sediment Sample Sufficient? Exploring Spatial and Temporal Microbial Diversity in a Small Lake

期刊

TOXINS
卷 12, 期 9, 页码 -

出版社

MDPI
DOI: 10.3390/toxins12090580

关键词

cyanobacteria; earthquakes; harmful algal blooms; microcystin; sediment; sediment cores

资金

  1. Ministry of Science, Research and the Arts of the Federal State Baden-Wurttemberg, Germany (Water Research Network project `Challenges of Reservoir Management-Meeting Environmental and Social Requirements') [814/15]
  2. Ministry of Business, Innovation and Employment, New Zealand [C05X1707]
  3. Marsden Fund of the Royal Society of New Zealand [CAW1601]
  4. International Max Planck Research School for Organismal Biology
  5. New Zealand Ministry of Business, Innovation & Employment (MBIE) [C05X1707] Funding Source: New Zealand Ministry of Business, Innovation & Employment (MBIE)

向作者/读者索取更多资源

(1) Background: Paleolimnological studies use sediment cores to explore long-term changes in lake ecology, including occurrences of harmful cyanobacterial blooms. Most studies are based on single cores, assuming this is representative of the whole lake, but data on small-scale spatial variability of microbial communities in lake sediment are scarce. (2) Methods: Surface sediments (top 0.5 cm) from 12 sites (n= 36) and two sediment cores were collected in Lake Rotorua (New Zealand). Bacterial community (16S rRNA metabarcoding),Microcystisspecific 16S rRNA, microcystin synthetase gene E (mcyE) and microcystins (MCs) were assessed. Radionuclide measurements (Pb-210,Cs-137) were used to date sediments. (3) Results: Bacterial community, based on relative abundances, differed significantly between surface sediment sites (p< 0.001) but the majority of bacterial amplicon sequence variants (88.8%) were shared. Despite intense MC producingMicrocystisblooms in the past, noMicrocystisspecific 16S rRNA,mcyEand MCs were found in surface sediments but occurred deeper in sediment cores (approximately 1950 ' s).Pb-210 measurements showed a disturbed profile, similar to patterns previously observed, as a result of earthquakes. (4) Conclusions: A single sediment core can capture dominant microbial communities. Toxin producingMicrocystisblooms are a recent phenomenon in Lake Rotorua. We posit that the absence ofMicrocystisfrom the surface sediments is a consequence of the Kaikoura earthquake two years prior to our sampling.

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