Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment”
Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kaufman, Darrell S. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2012 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© Springer Science+Business Media B.V. 2012 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Journal of paleolimnology - Springer Netherlands, 1988, 48(2012), 1 vom: 16. Mai, Seite 1-7 |
|---|---|
| Übergeordnetes Werk: |
volume:48 ; year:2012 ; number:1 ; day:16 ; month:05 ; pages:1-7 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10933-012-9621-6 |
|---|
| Katalog-ID: |
OLC2071092228 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2071092228 | ||
| 003 | DE-627 | ||
| 005 | 20230514111154.0 | ||
| 007 | tu | ||
| 008 | 200819s2012 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s10933-012-9621-6 |2 doi | |
| 035 | |a (DE-627)OLC2071092228 | ||
| 035 | |a (DE-He213)s10933-012-9621-6-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 570 |a 930 |q VZ |
| 084 | |a 14 |a 13 |a 12 |2 ssgn | ||
| 100 | 1 | |a Kaufman, Darrell S. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| 264 | 1 | |c 2012 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Springer Science+Business Media B.V. 2012 | ||
| 520 | |a Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. | ||
| 650 | 4 | |a Paleoenvironment | |
| 650 | 4 | |a Holocene | |
| 650 | 4 | |a Climate change | |
| 650 | 4 | |a Arctic lakes | |
| 650 | 4 | |a Proxy records | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of paleolimnology |d Springer Netherlands, 1988 |g 48(2012), 1 vom: 16. Mai, Seite 1-7 |w (DE-627)131173782 |w (DE-600)1140218-0 |w (DE-576)090827198 |x 0921-2728 |7 nnns |
| 773 | 1 | 8 | |g volume:48 |g year:2012 |g number:1 |g day:16 |g month:05 |g pages:1-7 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s10933-012-9621-6 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OLC-DE-84 | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_154 | ||
| 912 | |a GBV_ILN_2027 | ||
| 912 | |a GBV_ILN_4012 | ||
| 951 | |a AR | ||
| 952 | |d 48 |j 2012 |e 1 |b 16 |c 05 |h 1-7 | ||
| author_variant |
d s k ds dsk |
|---|---|
| matchkey_str |
article:09212728:2012----::nrdcinohjpseilsuhlcnploniomnarcrs |
| hierarchy_sort_str |
2012 |
| publishDate |
2012 |
| allfields |
10.1007/s10933-012-9621-6 doi (DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2012 Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. Paleoenvironment Holocene Climate change Arctic lakes Proxy records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 48(2012), 1 vom: 16. Mai, Seite 1-7 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:48 year:2012 number:1 day:16 month:05 pages:1-7 https://doi.org/10.1007/s10933-012-9621-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 48 2012 1 16 05 1-7 |
| spelling |
10.1007/s10933-012-9621-6 doi (DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2012 Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. Paleoenvironment Holocene Climate change Arctic lakes Proxy records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 48(2012), 1 vom: 16. Mai, Seite 1-7 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:48 year:2012 number:1 day:16 month:05 pages:1-7 https://doi.org/10.1007/s10933-012-9621-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 48 2012 1 16 05 1-7 |
| allfields_unstemmed |
10.1007/s10933-012-9621-6 doi (DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2012 Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. Paleoenvironment Holocene Climate change Arctic lakes Proxy records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 48(2012), 1 vom: 16. Mai, Seite 1-7 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:48 year:2012 number:1 day:16 month:05 pages:1-7 https://doi.org/10.1007/s10933-012-9621-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 48 2012 1 16 05 1-7 |
| allfieldsGer |
10.1007/s10933-012-9621-6 doi (DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2012 Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. Paleoenvironment Holocene Climate change Arctic lakes Proxy records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 48(2012), 1 vom: 16. Mai, Seite 1-7 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:48 year:2012 number:1 day:16 month:05 pages:1-7 https://doi.org/10.1007/s10933-012-9621-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 48 2012 1 16 05 1-7 |
| allfieldsSound |
10.1007/s10933-012-9621-6 doi (DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p DE-627 ger DE-627 rakwb eng 570 930 VZ 14 13 12 ssgn Kaufman, Darrell S. verfasserin aut Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2012 Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. Paleoenvironment Holocene Climate change Arctic lakes Proxy records Enthalten in Journal of paleolimnology Springer Netherlands, 1988 48(2012), 1 vom: 16. Mai, Seite 1-7 (DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 0921-2728 nnns volume:48 year:2012 number:1 day:16 month:05 pages:1-7 https://doi.org/10.1007/s10933-012-9621-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 AR 48 2012 1 16 05 1-7 |
| language |
English |
| source |
Enthalten in Journal of paleolimnology 48(2012), 1 vom: 16. Mai, Seite 1-7 volume:48 year:2012 number:1 day:16 month:05 pages:1-7 |
| sourceStr |
Enthalten in Journal of paleolimnology 48(2012), 1 vom: 16. Mai, Seite 1-7 volume:48 year:2012 number:1 day:16 month:05 pages:1-7 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Paleoenvironment Holocene Climate change Arctic lakes Proxy records |
| dewey-raw |
570 |
| isfreeaccess_bool |
false |
| container_title |
Journal of paleolimnology |
| authorswithroles_txt_mv |
Kaufman, Darrell S. @@aut@@ |
| publishDateDaySort_date |
2012-05-16T00:00:00Z |
| hierarchy_top_id |
131173782 |
| dewey-sort |
3570 |
| id |
OLC2071092228 |
| 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">OLC2071092228</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230514111154.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2012 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10933-012-9621-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2071092228</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10933-012-9621-6-p</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">570</subfield><subfield code="a">930</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="a">13</subfield><subfield code="a">12</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kaufman, Darrell S.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment”</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media B.V. 2012</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Paleoenvironment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Holocene</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Arctic lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Proxy records</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of paleolimnology</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">48(2012), 1 vom: 16. Mai, Seite 1-7</subfield><subfield code="w">(DE-627)131173782</subfield><subfield code="w">(DE-600)1140218-0</subfield><subfield code="w">(DE-576)090827198</subfield><subfield code="x">0921-2728</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2012</subfield><subfield code="g">number:1</subfield><subfield code="g">day:16</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:1-7</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10933-012-9621-6</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2012</subfield><subfield code="e">1</subfield><subfield code="b">16</subfield><subfield code="c">05</subfield><subfield code="h">1-7</subfield></datafield></record></collection>
|
| author |
Kaufman, Darrell S. |
| spellingShingle |
Kaufman, Darrell S. ddc 570 ssgn 14 misc Paleoenvironment misc Holocene misc Climate change misc Arctic lakes misc Proxy records Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| authorStr |
Kaufman, Darrell S. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)131173782 |
| format |
Article |
| dewey-ones |
570 - Life sciences; biology 930 - History of ancient world to ca. 499 |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0921-2728 |
| topic_title |
570 930 VZ 14 13 12 ssgn Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” Paleoenvironment Holocene Climate change Arctic lakes Proxy records |
| topic |
ddc 570 ssgn 14 misc Paleoenvironment misc Holocene misc Climate change misc Arctic lakes misc Proxy records |
| topic_unstemmed |
ddc 570 ssgn 14 misc Paleoenvironment misc Holocene misc Climate change misc Arctic lakes misc Proxy records |
| topic_browse |
ddc 570 ssgn 14 misc Paleoenvironment misc Holocene misc Climate change misc Arctic lakes misc Proxy records |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Journal of paleolimnology |
| hierarchy_parent_id |
131173782 |
| dewey-tens |
570 - Life sciences; biology 930 - History of ancient world (to ca. 499) |
| hierarchy_top_title |
Journal of paleolimnology |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)131173782 (DE-600)1140218-0 (DE-576)090827198 |
| title |
Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| ctrlnum |
(DE-627)OLC2071092228 (DE-He213)s10933-012-9621-6-p |
| title_full |
Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| author_sort |
Kaufman, Darrell S. |
| journal |
Journal of paleolimnology |
| journalStr |
Journal of paleolimnology |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science 900 - History & geography |
| recordtype |
marc |
| publishDateSort |
2012 |
| contenttype_str_mv |
txt |
| container_start_page |
1 |
| author_browse |
Kaufman, Darrell S. |
| container_volume |
48 |
| class |
570 930 VZ 14 13 12 ssgn |
| format_se |
Aufsätze |
| author-letter |
Kaufman, Darrell S. |
| doi_str_mv |
10.1007/s10933-012-9621-6 |
| dewey-full |
570 930 |
| title_sort |
introduction to the jopl special issue, “holocene paleoenvironmental records from arctic lake sediment” |
| title_auth |
Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| abstract |
Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. © Springer Science+Business Media B.V. 2012 |
| abstractGer |
Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. © Springer Science+Business Media B.V. 2012 |
| abstract_unstemmed |
Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate. © Springer Science+Business Media B.V. 2012 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_40 GBV_ILN_154 GBV_ILN_2027 GBV_ILN_4012 |
| container_issue |
1 |
| title_short |
Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment” |
| url |
https://doi.org/10.1007/s10933-012-9621-6 |
| remote_bool |
false |
| ppnlink |
131173782 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s10933-012-9621-6 |
| up_date |
2024-07-04T02:55:43.866Z |
| _version_ |
1803615463149666304 |
| 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">OLC2071092228</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230514111154.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2012 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10933-012-9621-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2071092228</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10933-012-9621-6-p</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">570</subfield><subfield code="a">930</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="a">13</subfield><subfield code="a">12</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kaufman, Darrell S.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Introduction to the JoPL special issue, “Holocene paleoenvironmental records from Arctic lake sediment”</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media B.V. 2012</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11.5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Paleoenvironment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Holocene</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate change</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Arctic lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Proxy records</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of paleolimnology</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">48(2012), 1 vom: 16. Mai, Seite 1-7</subfield><subfield code="w">(DE-627)131173782</subfield><subfield code="w">(DE-600)1140218-0</subfield><subfield code="w">(DE-576)090827198</subfield><subfield code="x">0921-2728</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2012</subfield><subfield code="g">number:1</subfield><subfield code="g">day:16</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:1-7</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10933-012-9621-6</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2012</subfield><subfield code="e">1</subfield><subfield code="b">16</subfield><subfield code="c">05</subfield><subfield code="h">1-7</subfield></datafield></record></collection>
|
| score |
7.401458 |