ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 11-CH-02II; 11-CH-02III; 11-CH-06I; 11-CH-06III; 11-CH-12I; 11-CH-12II; 11-CH-17I; 11-CH-17II; 12-KO-02; 12-KO-03; 12-KO-04; 12-KO-05; 13-TY-02-VI; 13-TY-02-VII; 14-OM-02-V1; 14-OM-02-V2; 14-OM-11-V3; 14-OM-20-V4; 14-OM-TRANS1; 14-OM-TRANS2; 14-OM-TRANS3; 14-OM-TRANS4; 14-OM-TRANS5; 14-OM-TRANS6; 14-OM-TRANS6-7; 16-KP-01-EN18001; 16-KP-01-EN18002; 16-KP-01-EN18003; 16-KP-01-EN18004; 16-KP-01-EN18005; 16-KP-01-EN18006; 16-KP-01-EN18007; 16-KP-01-EN18008; 16-KP-01-EN18009; 16-KP-01-EN18010; 16-KP-01-EN18011; 16-KP-01-EN18012; 16-KP-01-EN18013; 16-KP-01-EN18014; 16-KP-01-EN18015; 16-KP-01-EN18016; 16-KP-01-EN18017; 16-KP-01-EN18018; 16-KP-01-EN18019; 16-KP-01-EN18020; 16-KP-01-EN18021; 16-KP-01-EN18022; 16-KP-01-EN18023; 16-KP-01-EN18024; 16-KP-01-EN18025; 16-KP-01-EN18026; 16-KP-01-EN18027; 16-KP-04-EN18051; 16-KP-04-EN18052; 16-KP-04-EN18053; 16-KP-04-EN18054; 16-KP-04-EN18055; 16-KP-V01; 16-KP-V02; 16-KP-V03; 16-KP-V04; 16-KP-V05; 16-KP-V06; 16-KP-V07; 16-KP-V08; 16-KP-V09; 16-KP-V10; 16-KP-V11; 16-KP-V12; 16-KP-V13; 16-KP-V14; 16-KP-V15; 16-KP-V16; 16-KP-V17; 16-KP-V18; 16-KP-V19; 16-KP-V20; 16-KP-V21; 16-KP-V22; 16-KP-V23; 16-KP-V24; 16-KP-V25; 16-KP-V26; 16-KP-V27; 16-KP-V28; 16-KP-V29; 16-KP-V30; 16-KP-V31; 16-KP-V32; 16-KP-V33; 16-KP-V34; 16-KP-V35; 16-KP-V36; 16-KP-V37; 16-KP-V38; 16-KP-V39; 16-KP-V40; 16-KP-V41; 16-KP-V42; 16-KP-V43; 16-KP-V44; 16-KP-V45; 16-KP-V46; 16-KP-V47; 16-KP-V48; 16-KP-V49; 16-KP-V50; 16-KP-V51; 16-KP-V52; 16-KP-V53; 16-KP-V54; 16-KP-V55; 16-KP-V56; 16-KP-V57; 16-KP-V58; 18-BIL-00-EN18000; 18-BIL-01-EN18028; 18-BIL-01-EN18029; 18-BIL-02-EN18030; 18-BIL-02-EN18031; 18-BIL-02-EN18032; 18-BIL-02-EN18033; 18-BIL-02-EN18034; 18-BIL-02-EN18035; 18-LD-VP012-Tit-Ary; Area; Area/locality; AWI_Envi; AWI Arctic Land Expedition; B19-T1; B19-T2; Batagay 2019; Campaign; Central Yakutia; Chatanga2011; Chukotka; Chukotka 2018; Comment; DATE/TIME; ELEVATION; EN18061; EN18062; EN18063; EN18064; EN18065; EN18066; EN18067; EN18068; EN18069; EN18070_centre; EN18070_edge; EN18070_end; EN18070_transition; EN18071; EN18072; EN18073; EN18074; EN18075; EN18076; EN18077; EN18078; EN18079; EN18080; EN18081; EN18082; EN18083; EN21201; EN21202; EN21203; EN21204; EN21205; EN21206; EN21207; EN21208; EN21209; EN21210; EN21211; EN21212; EN21213; EN21214; EN21215; EN21216; EN21217; EN21218; EN21219; EN21220; EN21221; EN21222; EN21223; EN21224; EN21225; EN21226; EN21227; EN21228; EN21229; EN21230; EN21231; EN21232; EN21233; EN21234; EN21235; EN21236; EN21237; EN21238; EN21239; EN21240; EN21241; EN21242; EN21243; EN21244; EN21245; EN21246; EN21247; EN21248; EN21249; EN21250; EN21251; EN21252; EN21253; EN21254; EN21255; EN21256; EN21257; EN21258; EN21259; EN21260; EN21261; EN21262; EN21263; EN21264; Event label; Forest; Forest type; FTa; FTc; FTe; Genus; Gini coefficient; HAND; Height, maximum; Height, quantile; Individual Trees; Keperveem_2016; Kolyma, Russia; Kytalyk-Pokhodsk_2012, Kolyma2012; LATITUDE; Lena 2018; LONGITUDE; Mean values; Median values; MULT; Multiple investigations; Number of species; Number of trees; Omoloy2014; Plot; Polar Terrestrial Environmental Systems @ AWI; Principal investigator; Quantile (25th); Quantile (75th); Quantile (90th); Quantile (98th); Reference/source; RU-Land_2011_Khatanga; RU-Land_2012_Kytalyk_Kolyma; RU-Land_2013_Taymyr; RU-Land_2014_Omoloy; RU-Land_2016_Keperveem; RU-Land_2018_Chukotka; RU-Land_2018_Lena; RU-Land_2018_Yakutia; RU-Land_2019_Batagay; RU-Land_2021_Yakutia; Sampling by hand; Shannon Diversity Index; Siberia; Site; Taymyr; Taymyr2013; Tree, basal area, at base; Tree, basal area, at breast height; Tree, volume, conical; Tree, volume, smallian; Tree density; Tree height; Trees, basal area; Trees, volume, conical; Trees, volume, smallian; TY04VI; TY04VII; TY07VI; TY07VII; TY09VI; TY09VII; Vegetation survey; VEGSUR; Yakutia  (1)
  • AGE; AWI_Envi; AWI_PerDyn; Calculated, see reference(s); Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; Carbon, total; Depth, composite; DEPTH, sediment/rock; Difference; Karakul Lake, Tadschikistan; KK12-1; Niederreiter Piston corer; Nitrogen, total; Nitrogen/Carbon ratio; NPC; Permafrost Research (Periglacial Dynamics) @ AWI; Polar Terrestrial Environmental Systems @ AWI; see reference(s); Tadschikistan2012; Zone; δ13C; δ13C, organic carbon; δ15N  (1)
  • AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI  (1)
Collection
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Niemeyer, Bastian; Epp, Laura Saskia; Stoof-Leichsenring, Kathleen Rosmarie; Pestryakova, Luidmila A; Herzschuh, Ulrike (2017): A comparison of sedimentary DNA and pollen from lake sediments in recording vegetation composition at the Siberian treeline. Molecular Ecology Resources, 17(6), e46-e62, https://doi.org/10.1111/1755-0998.12689
    Publication Date: 2023-03-07
    Description: Reliable information of past vegetation changes are important to project future changes, especially for areas undergoing rapid transitioning such as the boreal treeline. The application of detailed sedDNA records has the potential to enhance our understanding of vegetation changes gained mainly from pollen studies of lake sediments. This study investigates sedDNA and pollen records from 31 lakes along a gradient of increasing larch forest cover in northern Siberia (Taymyr Peninsula) and compares them with vegetation field surveys within the lake's catchment. With respect to vegetation richness, sedDNA recorded 114 taxa, about half of them to species level, while pollen analyses identified 43 pollen taxa. Both approaches exceed the 31 taxa revealed by vegetation field surveys of 400 m**2 plots. From north to south, Larix percentages increase, as is consistently recorded by all three methods. Furthermore, tundra sites are separated from forested sites in the plots of the principal component analyses. Comparison of ordination results by Procrustes and Protest analyses yields a significant fit among all compared pairs of records. Despite the overall comparability of sedDNA and pollen analyses certain idiosyncrasies in the compositional signal are observed, such as high percentages of Alnus and Betula in all pollen spectra and high percentages of Salix in all sedDNA spectra. In conclusion, our results from the treeline show that sedDNA analyses perform better than pollen in recording site-specific richness (i.e. presence/absence of certain vegetation taxa in the direct vicinity of the lake) and perform as good as pollen in tracing regional vegetation composition.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-07-10
    Keywords: AGE; AWI_Envi; AWI_PerDyn; Calculated, see reference(s); Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; Carbon, total; Depth, composite; DEPTH, sediment/rock; Difference; Karakul Lake, Tadschikistan; KK12-1; Niederreiter Piston corer; Nitrogen, total; Nitrogen/Carbon ratio; NPC; Permafrost Research (Periglacial Dynamics) @ AWI; Polar Terrestrial Environmental Systems @ AWI; see reference(s); Tadschikistan2012; Zone; δ13C; δ13C, organic carbon; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 1008 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-01-10
    Keywords: 11-CH-02II; 11-CH-02III; 11-CH-06I; 11-CH-06III; 11-CH-12I; 11-CH-12II; 11-CH-17I; 11-CH-17II; 12-KO-02; 12-KO-03; 12-KO-04; 12-KO-05; 13-TY-02-VI; 13-TY-02-VII; 14-OM-02-V1; 14-OM-02-V2; 14-OM-11-V3; 14-OM-20-V4; 14-OM-TRANS1; 14-OM-TRANS2; 14-OM-TRANS3; 14-OM-TRANS4; 14-OM-TRANS5; 14-OM-TRANS6; 14-OM-TRANS6-7; 16-KP-01-EN18001; 16-KP-01-EN18002; 16-KP-01-EN18003; 16-KP-01-EN18004; 16-KP-01-EN18005; 16-KP-01-EN18006; 16-KP-01-EN18007; 16-KP-01-EN18008; 16-KP-01-EN18009; 16-KP-01-EN18010; 16-KP-01-EN18011; 16-KP-01-EN18012; 16-KP-01-EN18013; 16-KP-01-EN18014; 16-KP-01-EN18015; 16-KP-01-EN18016; 16-KP-01-EN18017; 16-KP-01-EN18018; 16-KP-01-EN18019; 16-KP-01-EN18020; 16-KP-01-EN18021; 16-KP-01-EN18022; 16-KP-01-EN18023; 16-KP-01-EN18024; 16-KP-01-EN18025; 16-KP-01-EN18026; 16-KP-01-EN18027; 16-KP-04-EN18051; 16-KP-04-EN18052; 16-KP-04-EN18053; 16-KP-04-EN18054; 16-KP-04-EN18055; 16-KP-V01; 16-KP-V02; 16-KP-V03; 16-KP-V04; 16-KP-V05; 16-KP-V06; 16-KP-V07; 16-KP-V08; 16-KP-V09; 16-KP-V10; 16-KP-V11; 16-KP-V12; 16-KP-V13; 16-KP-V14; 16-KP-V15; 16-KP-V16; 16-KP-V17; 16-KP-V18; 16-KP-V19; 16-KP-V20; 16-KP-V21; 16-KP-V22; 16-KP-V23; 16-KP-V24; 16-KP-V25; 16-KP-V26; 16-KP-V27; 16-KP-V28; 16-KP-V29; 16-KP-V30; 16-KP-V31; 16-KP-V32; 16-KP-V33; 16-KP-V34; 16-KP-V35; 16-KP-V36; 16-KP-V37; 16-KP-V38; 16-KP-V39; 16-KP-V40; 16-KP-V41; 16-KP-V42; 16-KP-V43; 16-KP-V44; 16-KP-V45; 16-KP-V46; 16-KP-V47; 16-KP-V48; 16-KP-V49; 16-KP-V50; 16-KP-V51; 16-KP-V52; 16-KP-V53; 16-KP-V54; 16-KP-V55; 16-KP-V56; 16-KP-V57; 16-KP-V58; 18-BIL-00-EN18000; 18-BIL-01-EN18028; 18-BIL-01-EN18029; 18-BIL-02-EN18030; 18-BIL-02-EN18031; 18-BIL-02-EN18032; 18-BIL-02-EN18033; 18-BIL-02-EN18034; 18-BIL-02-EN18035; 18-LD-VP012-Tit-Ary; Area; Area/locality; AWI_Envi; AWI Arctic Land Expedition; B19-T1; B19-T2; Batagay 2019; Campaign; Central Yakutia; Chatanga2011; Chukotka; Chukotka 2018; Comment; DATE/TIME; ELEVATION; EN18061; EN18062; EN18063; EN18064; EN18065; EN18066; EN18067; EN18068; EN18069; EN18070_centre; EN18070_edge; EN18070_end; EN18070_transition; EN18071; EN18072; EN18073; EN18074; EN18075; EN18076; EN18077; EN18078; EN18079; EN18080; EN18081; EN18082; EN18083; EN21201; EN21202; EN21203; EN21204; EN21205; EN21206; EN21207; EN21208; EN21209; EN21210; EN21211; EN21212; EN21213; EN21214; EN21215; EN21216; EN21217; EN21218; EN21219; EN21220; EN21221; EN21222; EN21223; EN21224; EN21225; EN21226; EN21227; EN21228; EN21229; EN21230; EN21231; EN21232; EN21233; EN21234; EN21235; EN21236; EN21237; EN21238; EN21239; EN21240; EN21241; EN21242; EN21243; EN21244; EN21245; EN21246; EN21247; EN21248; EN21249; EN21250; EN21251; EN21252; EN21253; EN21254; EN21255; EN21256; EN21257; EN21258; EN21259; EN21260; EN21261; EN21262; EN21263; EN21264; Event label; Forest; Forest type; FTa; FTc; FTe; Genus; Gini coefficient; HAND; Height, maximum; Height, quantile; Individual Trees; Keperveem_2016; Kolyma, Russia; Kytalyk-Pokhodsk_2012, Kolyma2012; LATITUDE; Lena 2018; LONGITUDE; Mean values; Median values; MULT; Multiple investigations; Number of species; Number of trees; Omoloy2014; Plot; Polar Terrestrial Environmental Systems @ AWI; Principal investigator; Quantile (25th); Quantile (75th); Quantile (90th); Quantile (98th); Reference/source; RU-Land_2011_Khatanga; RU-Land_2012_Kytalyk_Kolyma; RU-Land_2013_Taymyr; RU-Land_2014_Omoloy; RU-Land_2016_Keperveem; RU-Land_2018_Chukotka; RU-Land_2018_Lena; RU-Land_2018_Yakutia; RU-Land_2019_Batagay; RU-Land_2021_Yakutia; Sampling by hand; Shannon Diversity Index; Siberia; Site; Taymyr; Taymyr2013; Tree, basal area, at base; Tree, basal area, at breast height; Tree, volume, conical; Tree, volume, smallian; Tree density; Tree height; Trees, basal area; Trees, volume, conical; Trees, volume, smallian; TY04VI; TY04VII; TY07VI; TY07VII; TY09VI; TY09VII; Vegetation survey; VEGSUR; Yakutia
    Type: Dataset
    Format: text/tab-separated-values, 7323 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...