Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas
Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and to...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Shamurailatpam, Monica Sharma [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2021transfer abstract |
|---|
| Umfang: |
7 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids - Xiao, Qiuyun ELSEVIER, 2021, the journal of the International Union for Quaternary Research, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:599 ; year:2021 ; day:20 ; month:10 ; pages:55-61 ; extent:7 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.quaint.2020.11.003 |
|---|
| Katalog-ID: |
ELV054625521 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV054625521 | ||
| 003 | DE-627 | ||
| 005 | 20230626040524.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 210910s2021 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.quaint.2020.11.003 |2 doi | |
| 028 | 5 | 2 | |a /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica |
| 035 | |a (DE-627)ELV054625521 | ||
| 035 | |a (ELSEVIER)S1040-6182(20)30729-1 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 540 |q VZ |
| 084 | |a 6,25 |2 ssgn | ||
| 084 | |a ASIEN |q DE-1a |2 fid | ||
| 084 | |a 35.00 |2 bkl | ||
| 084 | |a 35.04 |2 bkl | ||
| 100 | 1 | |a Shamurailatpam, Monica Sharma |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| 264 | 1 | |c 2021transfer abstract | |
| 300 | |a 7 | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. | ||
| 520 | |a Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. | ||
| 700 | 1 | |a Kumar, Om |4 oth | |
| 700 | 1 | |a Ramanathan, AL. |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Xiao, Qiuyun ELSEVIER |t Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |d 2021 |d the journal of the International Union for Quaternary Research |g Amsterdam [u.a.] |w (DE-627)ELV005958261 |
| 773 | 1 | 8 | |g volume:599 |g year:2021 |g day:20 |g month:10 |g pages:55-61 |g extent:7 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.quaint.2020.11.003 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a FID-ASIEN | ||
| 936 | b | k | |a 35.00 |j Chemie: Allgemeines |q VZ |
| 936 | b | k | |a 35.04 |j Ausbildung |j Beruf |j Organisationen |x Chemie |q VZ |
| 951 | |a AR | ||
| 952 | |d 599 |j 2021 |b 20 |c 1020 |h 55-61 |g 7 | ||
| author_variant |
m s s ms mss |
|---|---|
| matchkey_str |
shamurailatpammonicasharmakumaromramanat:2021----:etnteeiberxetudrtnteihlcnciaeaibltrcrsrm |
| hierarchy_sort_str |
2021transfer abstract |
| bklnumber |
35.00 35.04 |
| publishDate |
2021 |
| allfields |
10.1016/j.quaint.2020.11.003 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica (DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 DE-627 ger DE-627 rakwb eng 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Shamurailatpam, Monica Sharma verfasserin aut Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas 2021transfer abstract 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Kumar, Om oth Ramanathan, AL. oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 https://doi.org/10.1016/j.quaint.2020.11.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 599 2021 20 1020 55-61 7 |
| spelling |
10.1016/j.quaint.2020.11.003 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica (DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 DE-627 ger DE-627 rakwb eng 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Shamurailatpam, Monica Sharma verfasserin aut Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas 2021transfer abstract 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Kumar, Om oth Ramanathan, AL. oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 https://doi.org/10.1016/j.quaint.2020.11.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 599 2021 20 1020 55-61 7 |
| allfields_unstemmed |
10.1016/j.quaint.2020.11.003 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica (DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 DE-627 ger DE-627 rakwb eng 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Shamurailatpam, Monica Sharma verfasserin aut Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas 2021transfer abstract 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Kumar, Om oth Ramanathan, AL. oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 https://doi.org/10.1016/j.quaint.2020.11.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 599 2021 20 1020 55-61 7 |
| allfieldsGer |
10.1016/j.quaint.2020.11.003 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica (DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 DE-627 ger DE-627 rakwb eng 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Shamurailatpam, Monica Sharma verfasserin aut Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas 2021transfer abstract 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Kumar, Om oth Ramanathan, AL. oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 https://doi.org/10.1016/j.quaint.2020.11.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 599 2021 20 1020 55-61 7 |
| allfieldsSound |
10.1016/j.quaint.2020.11.003 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica (DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 DE-627 ger DE-627 rakwb eng 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Shamurailatpam, Monica Sharma verfasserin aut Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas 2021transfer abstract 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. Kumar, Om oth Ramanathan, AL. oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 https://doi.org/10.1016/j.quaint.2020.11.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 599 2021 20 1020 55-61 7 |
| language |
English |
| source |
Enthalten in Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids Amsterdam [u.a.] volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 |
| sourceStr |
Enthalten in Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids Amsterdam [u.a.] volume:599 year:2021 day:20 month:10 pages:55-61 extent:7 |
| format_phy_str_mv |
Article |
| bklname |
Chemie: Allgemeines Ausbildung Beruf Organisationen |
| institution |
findex.gbv.de |
| dewey-raw |
540 |
| isfreeaccess_bool |
false |
| container_title |
Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
| authorswithroles_txt_mv |
Shamurailatpam, Monica Sharma @@aut@@ Kumar, Om @@oth@@ Ramanathan, AL. @@oth@@ |
| publishDateDaySort_date |
2021-01-20T00:00:00Z |
| hierarchy_top_id |
ELV005958261 |
| dewey-sort |
3540 |
| id |
ELV054625521 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV054625521</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626040524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">210910s2021 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.quaint.2020.11.003</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV054625521</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S1040-6182(20)30729-1</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">6,25</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">ASIEN</subfield><subfield code="q">DE-1a</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.04</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shamurailatpam, Monica Sharma</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">7</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kumar, Om</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ramanathan, AL.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Xiao, Qiuyun ELSEVIER</subfield><subfield code="t">Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids</subfield><subfield code="d">2021</subfield><subfield code="d">the journal of the International Union for Quaternary Research</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV005958261</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:599</subfield><subfield code="g">year:2021</subfield><subfield code="g">day:20</subfield><subfield code="g">month:10</subfield><subfield code="g">pages:55-61</subfield><subfield code="g">extent:7</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.quaint.2020.11.003</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-ASIEN</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.00</subfield><subfield code="j">Chemie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.04</subfield><subfield code="j">Ausbildung</subfield><subfield code="j">Beruf</subfield><subfield code="j">Organisationen</subfield><subfield code="x">Chemie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">599</subfield><subfield code="j">2021</subfield><subfield code="b">20</subfield><subfield code="c">1020</subfield><subfield code="h">55-61</subfield><subfield code="g">7</subfield></datafield></record></collection>
|
| author |
Shamurailatpam, Monica Sharma |
| spellingShingle |
Shamurailatpam, Monica Sharma ddc 540 ssgn 6,25 fid ASIEN bkl 35.00 bkl 35.04 Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| authorStr |
Shamurailatpam, Monica Sharma |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV005958261 |
| format |
electronic Article |
| dewey-ones |
540 - Chemistry & allied sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| topic |
ddc 540 ssgn 6,25 fid ASIEN bkl 35.00 bkl 35.04 |
| topic_unstemmed |
ddc 540 ssgn 6,25 fid ASIEN bkl 35.00 bkl 35.04 |
| topic_browse |
ddc 540 ssgn 6,25 fid ASIEN bkl 35.00 bkl 35.04 |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
o k ok a r ar |
| hierarchy_parent_title |
Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
| hierarchy_parent_id |
ELV005958261 |
| dewey-tens |
540 - Chemistry |
| hierarchy_top_title |
Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV005958261 |
| title |
Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| ctrlnum |
(DE-627)ELV054625521 (ELSEVIER)S1040-6182(20)30729-1 |
| title_full |
Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| author_sort |
Shamurailatpam, Monica Sharma |
| journal |
Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
| journalStr |
Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2021 |
| contenttype_str_mv |
zzz |
| container_start_page |
55 |
| author_browse |
Shamurailatpam, Monica Sharma |
| container_volume |
599 |
| physical |
7 |
| class |
540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Shamurailatpam, Monica Sharma |
| doi_str_mv |
10.1016/j.quaint.2020.11.003 |
| dewey-full |
540 |
| title_sort |
testing the reliable proxies to understand the mid-holocene climate variability records from chandratal lake, western himalayas |
| title_auth |
Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| abstract |
Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. |
| abstractGer |
Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. |
| abstract_unstemmed |
Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN |
| title_short |
Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas |
| url |
https://doi.org/10.1016/j.quaint.2020.11.003 |
| remote_bool |
true |
| author2 |
Kumar, Om Ramanathan, AL |
| author2Str |
Kumar, Om Ramanathan, AL |
| ppnlink |
ELV005958261 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth |
| doi_str |
10.1016/j.quaint.2020.11.003 |
| up_date |
2024-07-06T22:14:49.885Z |
| _version_ |
1803869581356302336 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV054625521</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626040524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">210910s2021 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.quaint.2020.11.003</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001452.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV054625521</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S1040-6182(20)30729-1</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">6,25</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">ASIEN</subfield><subfield code="q">DE-1a</subfield><subfield code="2">fid</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">35.04</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shamurailatpam, Monica Sharma</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Testing the reliable proxies to understand the mid-Holocene climate variability records from Chandratal lake, Western Himalayas</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">7</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Chandratal lake (32°28′30.65″ N 77°37′1.42″ E) located at the junction of Indian Summer Monsoon and Westerlies in the Northwestern Himalaya give an opportunity to reconstruct climate variability over the last ~6300 cal yr BP. Here, we used multi-proxy (Amino acids, Biogenic silica, grain size and total organic carbon) to link climate change and organic burial during the mid-Holocene period. The proxy records captured the changes in monsoon patterns, linking with Holocene climate optimum (HCO) during the ~6344- 5821 cal BP. The sediment profile begins with a wetter and moist climate mostly from the terrestrial environment inputs, corresponding to the warm Holocene Climate Optimum (HCO) period (~6344 - 5821 cal yr BP). A stable condition of the geochemical proxies during ~5821-3780 cal yr BP reveals a shifting of a moisture source, catchment stability and cold/dry climate in correspondence with reduced precipitation.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kumar, Om</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ramanathan, AL.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Xiao, Qiuyun ELSEVIER</subfield><subfield code="t">Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids</subfield><subfield code="d">2021</subfield><subfield code="d">the journal of the International Union for Quaternary Research</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV005958261</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:599</subfield><subfield code="g">year:2021</subfield><subfield code="g">day:20</subfield><subfield code="g">month:10</subfield><subfield code="g">pages:55-61</subfield><subfield code="g">extent:7</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.quaint.2020.11.003</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-ASIEN</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.00</subfield><subfield code="j">Chemie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.04</subfield><subfield code="j">Ausbildung</subfield><subfield code="j">Beruf</subfield><subfield code="j">Organisationen</subfield><subfield code="x">Chemie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">599</subfield><subfield code="j">2021</subfield><subfield code="b">20</subfield><subfield code="c">1020</subfield><subfield code="h">55-61</subfield><subfield code="g">7</subfield></datafield></record></collection>
|
| score |
7.4007425 |