• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

隐花植物地被层的一氧化碳通量:I. 对再饱和的响应。

CO fluxes of cryptogamic crusts: I. Response to resaturation.

作者信息

Jeffries D L, Link S O, Klopatek J M

机构信息

Division of Science and Mathematics, University of the Ozarks, Clarksville, Arkansas 72830.

Pacific Northwest Laboratory, Richland, Washington 99352.

出版信息

New Phytol. 1993 Sep;125(1):163-173. doi: 10.1111/j.1469-8137.1993.tb03874.x.

DOI:10.1111/j.1469-8137.1993.tb03874.x
PMID:33874607
Abstract

The relationship between carbon dioxide exchange of Microcoleus- and Scytonema-dominated cryptogamic crusts and resaturation time was measured in the laboratory with a modified discrete sampling technique and infrared gas analysis. Maximum net photosynthetic rate of Microcoleus was 187 nmol CO m s and of Scytonema was 111 nmol CO m s for rehydration to 100% soil saturation. Both crust types demonstrated a slow rise in resaturation respiration and took 2 days to become fully active after the (first rehydration to 100% soil saturation after long-term dryness, and only one day to become active after the second rehydration cycle.

摘要

在实验室中,采用改良的离散采样技术和红外气体分析法,测量了以微鞘藻属和席藻属为主的隐花植物结皮的二氧化碳交换与再饱和时间之间的关系。微鞘藻属的最大净光合速率为187 nmol CO₂ m⁻² s⁻¹,席藻属的最大净光合速率为111 nmol CO₂ m⁻² s⁻¹,复水至土壤饱和度100%时达到此速率。两种结皮类型的再饱和呼吸均呈缓慢上升趋势,在长期干燥后首次复水至土壤饱和度100%后,需要2天才能完全恢复活性,而在第二次复水循环后仅需1天就能恢复活性。

相似文献

1
CO fluxes of cryptogamic crusts: I. Response to resaturation.隐花植物地被层的一氧化碳通量:I. 对再饱和的响应。
New Phytol. 1993 Sep;125(1):163-173. doi: 10.1111/j.1469-8137.1993.tb03874.x.
2
CO fluxes of cryptogamic crusts: II. Response to dehydration.隐花植物地被层的一氧化碳通量:II. 对脱水的响应。
New Phytol. 1993 Oct;125(2):391-396. doi: 10.1111/j.1469-8137.1993.tb03891.x.
3
Response of desert biological soil crusts to alterations in precipitation frequency.沙漠生物土壤结皮对降水频率变化的响应。
Oecologia. 2004 Oct;141(2):306-16. doi: 10.1007/s00442-003-1438-6. Epub 2003 Dec 19.
4
Greenhouse gas fluxes at different growth stages of biological soil crusts in eastern Hobq desert, China.中国毛乌素沙地东部生物土壤结皮不同生长阶段的温室气体通量
Ying Yong Sheng Tai Xue Bao. 2019 Mar;30(3):857-866. doi: 10.13287/j.1001-9332.201903.004.
5
[Development and succession of biological soil crusts and the changes of microbial biomasses].生物土壤结皮的发育与演替及微生物生物量的变化
Huan Jing Ke Xue. 2014 Apr;35(4):1479-85.
6
[Greenhouse gases fluxes of biological soil crusts and soil ecosystem in the artificial sand-fixing vegetation region in Shapotou area].[沙坡头地区人工固沙植被区生物土壤结皮与土壤生态系统温室气体通量]
Ying Yong Sheng Tai Xue Bao. 2014 Jan;25(1):61-8.
7
Precipitation pulse size effects on Sonoran Desert soil microbial crusts.降水脉冲大小对索诺兰沙漠土壤微生物结皮的影响。
Oecologia. 2004 Oct;141(2):317-24. doi: 10.1007/s00442-003-1461-7. Epub 2003 Dec 11.
8
In-situ soil greenhouse gas fluxes under different cryptogamic covers in maritime Antarctica.在南极海洋地区不同隐花植物覆盖下的原位土壤温室气体通量。
Sci Total Environ. 2021 May 20;770:144557. doi: 10.1016/j.scitotenv.2020.144557. Epub 2021 Jan 17.
9
[Response of the artificial cyanobacterial crusts to low temperature and light stress and the micro-structure changes under laboratory conditions].[人工蓝藻结皮对低温和光照胁迫的响应及实验室条件下的微观结构变化]
Huan Jing Ke Xue. 2012 Aug;33(8):2793-803.
10
CO exchange of the endolithic lichen Verrucaria baldensis from karst habitats in northern Italy.来自意大利北部喀斯特栖息地的石内生地衣巴氏疣衣的一氧化碳交换。
Oecologia. 1997 Aug;111(4):515-522. doi: 10.1007/s004420050265.

引用本文的文献

1
Soil moisture dynamics under two rainfall frequency treatments drive early spring CO gas exchange of lichen-dominated biocrusts in central Spain.西班牙中部两种降雨频率处理下的土壤水分动态驱动地衣主导的生物结皮早春CO气体交换。
PeerJ. 2018 Nov 16;6:e5904. doi: 10.7717/peerj.5904. eCollection 2018.
2
Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water.从利用非降雨水的生物结皮碳交换看气候变化。
Sci Rep. 2017 May 31;7(1):2573. doi: 10.1038/s41598-017-02812-y.
3
Response of biological soil crust diazotrophs to season, altered summer precipitation, and year-round increased temperature in an arid grassland of the colorado plateau, USA.
生物土壤结皮固氮生物对季节、夏季降水变化和全年增温的响应,美国科罗拉多高原干旱草原。
Front Microbiol. 2012 Oct 11;3:358. doi: 10.3389/fmicb.2012.00358. eCollection 2012.
4
Impact of grazing intensity on seasonal variations in soil organic carbon and soil CO2 efflux in two semiarid grasslands in southern Botswana.放牧强度对博茨瓦纳南部两个半干旱草地土壤有机碳和土壤 CO2 排放季节变化的影响。
Philos Trans R Soc Lond B Biol Sci. 2012 Nov 19;367(1606):3076-86. doi: 10.1098/rstb.2012.0102.
5
Activation of methanogenesis in arid biological soil crusts despite the presence of oxygen.尽管存在氧气,干旱生物土壤结皮中仍能进行甲烷生成的激活。
PLoS One. 2011;6(5):e20453. doi: 10.1371/journal.pone.0020453. Epub 2011 May 31.