|
|
|
|
| LEADER |
01000naa a22002652 4500 |
| 001 |
NLM336244002 |
| 003 |
DE-627 |
| 005 |
20231225231710.0 |
| 007 |
cr uuu---uuuuu |
| 008 |
231225s2022 xx |||||o 00| ||eng c |
| 024 |
7 |
|
|a 10.1111/gcb.16102
|2 doi
|
| 028 |
5 |
2 |
|a pubmed24n1120.xml
|
| 035 |
|
|
|a (DE-627)NLM336244002
|
| 035 |
|
|
|a (NLM)35090074
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a Tian, Weitao
|e verfasserin
|4 aut
|
| 245 |
1 |
0 |
|a Thermal adaptation occurs in the respiration and growth of widely distributed bacteria
|
| 264 |
|
1 |
|c 2022
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a ƒaComputermedien
|b c
|2 rdamedia
|
| 338 |
|
|
|a ƒa Online-Ressource
|b cr
|2 rdacarrier
|
| 500 |
|
|
|a Date Completed 13.04.2022
|
| 500 |
|
|
|a Date Revised 13.04.2022
|
| 500 |
|
|
|a published: Print-Electronic
|
| 500 |
|
|
|a Citation Status MEDLINE
|
| 520 |
|
|
|a © 2022 John Wiley & Sons Ltd.
|
| 520 |
|
|
|a Soil microbial respiration is an important factor in regulating carbon (C) exchange between the soil and atmosphere. Thermal adaptation of soil microorganisms will lead to a weakening of the positive feedback between climate warming and soil respiration. The thermal adaptation of microbial communities and fungal species has been proven. However, studies on the thermal adaptation of bacterial species, the most important decomposers in the soil, are still lacking. Here, we isolated six species of widely distributed dominant bacteria and studied the effects of constant warming and temperature fluctuations on those species. The results showed that constant warming caused a downregulation of respiratory temperature sensitivity (Q10 ) of the bacterial species, accompanied by an elevation of the minimum temperature (Tmin ) required for growth. Similar results were seen with the addition of temperature fluctuations, suggesting that both scenarios caused a significant thermal adaptation among the bacterial species. Fluctuating and increasing temperatures are considered an important component of future warming. Therefore, the inclusion of physiological responses of bacteria to these changes is essential to understand relationships between microbiota and temperature and enhance the prediction of global soil-atmosphere C feedbacks
|
| 650 |
|
4 |
|a Journal Article
|
| 650 |
|
4 |
|a Q10
|
| 650 |
|
4 |
|a Tmin
|
| 650 |
|
4 |
|a bacteria
|
| 650 |
|
4 |
|a temperature fluctuation
|
| 650 |
|
4 |
|a thermal adaptation
|
| 650 |
|
4 |
|a warming
|
| 650 |
|
7 |
|a Soil
|2 NLM
|
| 650 |
|
7 |
|a Carbon
|2 NLM
|
| 650 |
|
7 |
|a 7440-44-0
|2 NLM
|
| 700 |
1 |
|
|a Sun, Huimin
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Zhang, Yan
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Xu, Jianjun
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Yao, Jia
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Li, Jinquan
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Li, Bo
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Nie, Ming
|e verfasserin
|4 aut
|
| 773 |
0 |
8 |
|i Enthalten in
|t Global change biology
|d 1999
|g 28(2022), 8 vom: 28. Apr., Seite 2820-2829
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
|
| 773 |
1 |
8 |
|g volume:28
|g year:2022
|g number:8
|g day:28
|g month:04
|g pages:2820-2829
|
| 856 |
4 |
0 |
|u http://dx.doi.org/10.1111/gcb.16102
|3 Volltext
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_NLM
|
| 912 |
|
|
|a GBV_ILN_350
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 28
|j 2022
|e 8
|b 28
|c 04
|h 2820-2829
|