Diatomeen als Indikatoren für Umwelt- und Klimaänderungen : eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel

The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Baier, Janina - 1971-
Hochschulschrift:	Zugl.: Potsdam, Univ., Diss, 2002

Format:	E-Book
Sprache:	Deutsch

Erschienen:	Potsdam: Geoforschungszentrum ; 2003

Schlagwörter:	Holzmaar / Holozän / Warve / Kieselalgen / Paläolimnologie
Schlagwörter:	Diatoms, Fossil, Germany, Holzmaar, Lake Paleoclimatology, Holocene Paleolimnology, Germany, Holzmaar, Lake
Formangabe:	Hochschulschrift

Systematik:	RB 10360

Umfang:	Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB)

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Baier, Janina: Diatomeen als Indikatoren für Umwelt- und Klimaänderungen - Potsdam : GeoForschungsZentrum, 2003

Reihe:	Scientific technical report / Geoforschungszentrum Potsdam ; 2003,03

Links:	Link aufrufen Volltext Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:kobv:b103-030084

Katalog-ID:	37021854X

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Indexfelder

matchkey_str	baierjanina:2003----:itmeasniaoefuwludl
oclc_num	76627281
hierarchy_sort_str	[2003]
bklnumber	38.21 38.19
publishDate	2003
allfields	03,A41,0885 dnb 968701655 DE-101 urn:nbn:de:kobv:b103-030084 urn (DE-627)37021854X (DE-599)DNB968701655 (OCoLC)76627281 DE-627 ger DE-627 rakwb ger XA-DE 31 sdnb 32 sdnb 16,13 ssgn RB 10360 SEPA rvk (DE-625)rvk/142220:12707 38.21 bkl 38.19 bkl Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel Geoforschungszentrum Potsdam. Von Janina Baier Potsdam Geoforschungszentrum [2003] Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Scientific technical report / Geoforschungszentrum Potsdam 2003,03 Zugl.: Potsdam, Univ., Diss, 2002 The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability. Diatoms, Fossil Germany Holzmaar, Lake Paleoclimatology Holocene Paleolimnology Germany Holzmaar, Lake Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4398290-6 (DE-627)19167446X (DE-576)212026127 Holzmaar gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4189157-0 (DE-627)105259101 (DE-576)210057874 Warve gnd s (DE-588)4030509-0 (DE-627)106269615 (DE-576)208987908 Kieselalgen gnd s (DE-588)4173114-1 (DE-627)105382361 (DE-576)209947950 Paläolimnologie gnd DE-101 Baier, Janina 1971- (DE-588)124993850 (DE-627)369631536 (DE-576)294609334 oth Potsdam uvp Erscheint auch als Druck-Ausgabe Baier, Janina Diatomeen als Indikatoren für Umwelt- und Klimaänderungen Potsdam : GeoForschungsZentrum, 2003 XVI, 181 S. (DE-627)117676571X (DE-576)10676571X GeoForschungsZentrum Potsdam Scientific technical report 2003,03 200303 (DE-627)528840622 (DE-576)281277311 (DE-600)2295786-8 1610-0956 ns http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf Verlag Volltext http://www.gfz-potsdam.de/bib/pub/str0303/0303.pdf Verlag Volltext http://d-nb.info/968701655 Verlag Volltext http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 RB 10360 Stehende Gewässer (Seenkunde, Limnologie) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Mathematische Geografie und Physiogeografie Hydrogeografie Gewässerkunde (Hydrologie) Teilgebiete und Einzelfragen Stehende Gewässer (Seenkunde, Limnologie) (DE-627)1271498529 (DE-625)rvk/142220:12707 (DE-576)201498529 38.21 Paläobotanik SEPA (DE-627)106408216 38.19 Historische Geologie: Sonstiges SEPA (DE-627)106408232 BO 20 01 0084 653258089 x 22-06-04 21 01 0046 659683059 z 13-08-04 22 01 0018 653359993 SUBolrd xu 22-06-04 30 01 0104 71985377X z 14-05-05 40 01 0007 653455518 ksn 23-06-04 60 01 0705 653554125 z 23-06-04 110 01 3110 719853788 xz 14-05-05 285 01 0517 117738504X OLR-EXT z 18-08-10 370 01 4370 822431599 x 08-06-07 20 01 0084 http://d-nb.info/968701655 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 30 01 0104 http://d-nb.info/968701655 40 01 0007 http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf 40 01 0007 Lizenzbedingungen http://creativecommons.org/licenses/by-nc-sa/3.0/de/ 60 01 0705 http://d-nb.info/968701655 110 01 3110 http://d-nb.info/968701655 285 01 0517 Open Access http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 370 01 4370 http://deposit.ddb.de/cgi-bin/dokserv?idn=968701655 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TQ 01040 285 00 DE-517 00 TP 05078 285 00 DE-517 00 TP 5078 285 00 DE-517 00 TQ 1040 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 285 01 0517 OLR-EXT 40 01 0007 2004-06 9
spelling	03,A41,0885 dnb 968701655 DE-101 urn:nbn:de:kobv:b103-030084 urn (DE-627)37021854X (DE-599)DNB968701655 (OCoLC)76627281 DE-627 ger DE-627 rakwb ger XA-DE 31 sdnb 32 sdnb 16,13 ssgn RB 10360 SEPA rvk (DE-625)rvk/142220:12707 38.21 bkl 38.19 bkl Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel Geoforschungszentrum Potsdam. Von Janina Baier Potsdam Geoforschungszentrum [2003] Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Scientific technical report / Geoforschungszentrum Potsdam 2003,03 Zugl.: Potsdam, Univ., Diss, 2002 The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability. Diatoms, Fossil Germany Holzmaar, Lake Paleoclimatology Holocene Paleolimnology Germany Holzmaar, Lake Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4398290-6 (DE-627)19167446X (DE-576)212026127 Holzmaar gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4189157-0 (DE-627)105259101 (DE-576)210057874 Warve gnd s (DE-588)4030509-0 (DE-627)106269615 (DE-576)208987908 Kieselalgen gnd s (DE-588)4173114-1 (DE-627)105382361 (DE-576)209947950 Paläolimnologie gnd DE-101 Baier, Janina 1971- (DE-588)124993850 (DE-627)369631536 (DE-576)294609334 oth Potsdam uvp Erscheint auch als Druck-Ausgabe Baier, Janina Diatomeen als Indikatoren für Umwelt- und Klimaänderungen Potsdam : GeoForschungsZentrum, 2003 XVI, 181 S. (DE-627)117676571X (DE-576)10676571X GeoForschungsZentrum Potsdam Scientific technical report 2003,03 200303 (DE-627)528840622 (DE-576)281277311 (DE-600)2295786-8 1610-0956 ns http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf Verlag Volltext http://www.gfz-potsdam.de/bib/pub/str0303/0303.pdf Verlag Volltext http://d-nb.info/968701655 Verlag Volltext http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 RB 10360 Stehende Gewässer (Seenkunde, Limnologie) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Mathematische Geografie und Physiogeografie Hydrogeografie Gewässerkunde (Hydrologie) Teilgebiete und Einzelfragen Stehende Gewässer (Seenkunde, Limnologie) (DE-627)1271498529 (DE-625)rvk/142220:12707 (DE-576)201498529 38.21 Paläobotanik SEPA (DE-627)106408216 38.19 Historische Geologie: Sonstiges SEPA (DE-627)106408232 BO 20 01 0084 653258089 x 22-06-04 21 01 0046 659683059 z 13-08-04 22 01 0018 653359993 SUBolrd xu 22-06-04 30 01 0104 71985377X z 14-05-05 40 01 0007 653455518 ksn 23-06-04 60 01 0705 653554125 z 23-06-04 110 01 3110 719853788 xz 14-05-05 285 01 0517 117738504X OLR-EXT z 18-08-10 370 01 4370 822431599 x 08-06-07 20 01 0084 http://d-nb.info/968701655 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 30 01 0104 http://d-nb.info/968701655 40 01 0007 http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf 40 01 0007 Lizenzbedingungen http://creativecommons.org/licenses/by-nc-sa/3.0/de/ 60 01 0705 http://d-nb.info/968701655 110 01 3110 http://d-nb.info/968701655 285 01 0517 Open Access http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 370 01 4370 http://deposit.ddb.de/cgi-bin/dokserv?idn=968701655 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TQ 01040 285 00 DE-517 00 TP 05078 285 00 DE-517 00 TP 5078 285 00 DE-517 00 TQ 1040 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 285 01 0517 OLR-EXT 40 01 0007 2004-06 9
allfields_unstemmed	03,A41,0885 dnb 968701655 DE-101 urn:nbn:de:kobv:b103-030084 urn (DE-627)37021854X (DE-599)DNB968701655 (OCoLC)76627281 DE-627 ger DE-627 rakwb ger XA-DE 31 sdnb 32 sdnb 16,13 ssgn RB 10360 SEPA rvk (DE-625)rvk/142220:12707 38.21 bkl 38.19 bkl Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel Geoforschungszentrum Potsdam. Von Janina Baier Potsdam Geoforschungszentrum [2003] Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Scientific technical report / Geoforschungszentrum Potsdam 2003,03 Zugl.: Potsdam, Univ., Diss, 2002 The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability. Diatoms, Fossil Germany Holzmaar, Lake Paleoclimatology Holocene Paleolimnology Germany Holzmaar, Lake Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4398290-6 (DE-627)19167446X (DE-576)212026127 Holzmaar gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4189157-0 (DE-627)105259101 (DE-576)210057874 Warve gnd s (DE-588)4030509-0 (DE-627)106269615 (DE-576)208987908 Kieselalgen gnd s (DE-588)4173114-1 (DE-627)105382361 (DE-576)209947950 Paläolimnologie gnd DE-101 Baier, Janina 1971- (DE-588)124993850 (DE-627)369631536 (DE-576)294609334 oth Potsdam uvp Erscheint auch als Druck-Ausgabe Baier, Janina Diatomeen als Indikatoren für Umwelt- und Klimaänderungen Potsdam : GeoForschungsZentrum, 2003 XVI, 181 S. (DE-627)117676571X (DE-576)10676571X GeoForschungsZentrum Potsdam Scientific technical report 2003,03 200303 (DE-627)528840622 (DE-576)281277311 (DE-600)2295786-8 1610-0956 ns http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf Verlag Volltext http://www.gfz-potsdam.de/bib/pub/str0303/0303.pdf Verlag Volltext http://d-nb.info/968701655 Verlag Volltext http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 RB 10360 Stehende Gewässer (Seenkunde, Limnologie) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Mathematische Geografie und Physiogeografie Hydrogeografie Gewässerkunde (Hydrologie) Teilgebiete und Einzelfragen Stehende Gewässer (Seenkunde, Limnologie) (DE-627)1271498529 (DE-625)rvk/142220:12707 (DE-576)201498529 38.21 Paläobotanik SEPA (DE-627)106408216 38.19 Historische Geologie: Sonstiges SEPA (DE-627)106408232 BO 20 01 0084 653258089 x 22-06-04 21 01 0046 659683059 z 13-08-04 22 01 0018 653359993 SUBolrd xu 22-06-04 30 01 0104 71985377X z 14-05-05 40 01 0007 653455518 ksn 23-06-04 60 01 0705 653554125 z 23-06-04 110 01 3110 719853788 xz 14-05-05 285 01 0517 117738504X OLR-EXT z 18-08-10 370 01 4370 822431599 x 08-06-07 20 01 0084 http://d-nb.info/968701655 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 30 01 0104 http://d-nb.info/968701655 40 01 0007 http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf 40 01 0007 Lizenzbedingungen http://creativecommons.org/licenses/by-nc-sa/3.0/de/ 60 01 0705 http://d-nb.info/968701655 110 01 3110 http://d-nb.info/968701655 285 01 0517 Open Access http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 370 01 4370 http://deposit.ddb.de/cgi-bin/dokserv?idn=968701655 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TQ 01040 285 00 DE-517 00 TP 05078 285 00 DE-517 00 TP 5078 285 00 DE-517 00 TQ 1040 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 285 01 0517 OLR-EXT 40 01 0007 2004-06 9
allfieldsGer	03,A41,0885 dnb 968701655 DE-101 urn:nbn:de:kobv:b103-030084 urn (DE-627)37021854X (DE-599)DNB968701655 (OCoLC)76627281 DE-627 ger DE-627 rakwb ger XA-DE 31 sdnb 32 sdnb 16,13 ssgn RB 10360 SEPA rvk (DE-625)rvk/142220:12707 38.21 bkl 38.19 bkl Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel Geoforschungszentrum Potsdam. Von Janina Baier Potsdam Geoforschungszentrum [2003] Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Scientific technical report / Geoforschungszentrum Potsdam 2003,03 Zugl.: Potsdam, Univ., Diss, 2002 The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability. Diatoms, Fossil Germany Holzmaar, Lake Paleoclimatology Holocene Paleolimnology Germany Holzmaar, Lake Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4398290-6 (DE-627)19167446X (DE-576)212026127 Holzmaar gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4189157-0 (DE-627)105259101 (DE-576)210057874 Warve gnd s (DE-588)4030509-0 (DE-627)106269615 (DE-576)208987908 Kieselalgen gnd s (DE-588)4173114-1 (DE-627)105382361 (DE-576)209947950 Paläolimnologie gnd DE-101 Baier, Janina 1971- (DE-588)124993850 (DE-627)369631536 (DE-576)294609334 oth Potsdam uvp Erscheint auch als Druck-Ausgabe Baier, Janina Diatomeen als Indikatoren für Umwelt- und Klimaänderungen Potsdam : GeoForschungsZentrum, 2003 XVI, 181 S. (DE-627)117676571X (DE-576)10676571X GeoForschungsZentrum Potsdam Scientific technical report 2003,03 200303 (DE-627)528840622 (DE-576)281277311 (DE-600)2295786-8 1610-0956 ns http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf Verlag Volltext http://www.gfz-potsdam.de/bib/pub/str0303/0303.pdf Verlag Volltext http://d-nb.info/968701655 Verlag Volltext http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 RB 10360 Stehende Gewässer (Seenkunde, Limnologie) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Mathematische Geografie und Physiogeografie Hydrogeografie Gewässerkunde (Hydrologie) Teilgebiete und Einzelfragen Stehende Gewässer (Seenkunde, Limnologie) (DE-627)1271498529 (DE-625)rvk/142220:12707 (DE-576)201498529 38.21 Paläobotanik SEPA (DE-627)106408216 38.19 Historische Geologie: Sonstiges SEPA (DE-627)106408232 BO 20 01 0084 653258089 x 22-06-04 21 01 0046 659683059 z 13-08-04 22 01 0018 653359993 SUBolrd xu 22-06-04 30 01 0104 71985377X z 14-05-05 40 01 0007 653455518 ksn 23-06-04 60 01 0705 653554125 z 23-06-04 110 01 3110 719853788 xz 14-05-05 285 01 0517 117738504X OLR-EXT z 18-08-10 370 01 4370 822431599 x 08-06-07 20 01 0084 http://d-nb.info/968701655 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 30 01 0104 http://d-nb.info/968701655 40 01 0007 http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf 40 01 0007 Lizenzbedingungen http://creativecommons.org/licenses/by-nc-sa/3.0/de/ 60 01 0705 http://d-nb.info/968701655 110 01 3110 http://d-nb.info/968701655 285 01 0517 Open Access http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 370 01 4370 http://deposit.ddb.de/cgi-bin/dokserv?idn=968701655 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TQ 01040 285 00 DE-517 00 TP 05078 285 00 DE-517 00 TP 5078 285 00 DE-517 00 TQ 1040 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 285 01 0517 OLR-EXT 40 01 0007 2004-06 9
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Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability. Diatoms, Fossil Germany Holzmaar, Lake Paleoclimatology Holocene Paleolimnology Germany Holzmaar, Lake Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4398290-6 (DE-627)19167446X (DE-576)212026127 Holzmaar gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4189157-0 (DE-627)105259101 (DE-576)210057874 Warve gnd s (DE-588)4030509-0 (DE-627)106269615 (DE-576)208987908 Kieselalgen gnd s (DE-588)4173114-1 (DE-627)105382361 (DE-576)209947950 Paläolimnologie gnd DE-101 Baier, Janina 1971- (DE-588)124993850 (DE-627)369631536 (DE-576)294609334 oth Potsdam uvp Erscheint auch als Druck-Ausgabe Baier, Janina Diatomeen als Indikatoren für Umwelt- und Klimaänderungen Potsdam : GeoForschungsZentrum, 2003 XVI, 181 S. (DE-627)117676571X (DE-576)10676571X GeoForschungsZentrum Potsdam Scientific technical report 2003,03 200303 (DE-627)528840622 (DE-576)281277311 (DE-600)2295786-8 1610-0956 ns http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf Verlag Volltext http://www.gfz-potsdam.de/bib/pub/str0303/0303.pdf Verlag Volltext http://d-nb.info/968701655 Verlag Volltext http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 RB 10360 Stehende Gewässer (Seenkunde, Limnologie) Geografie Nicht regional gebundene Darstellungen Allgemeine Geografie Mathematische Geografie und Physiogeografie Hydrogeografie Gewässerkunde (Hydrologie) Teilgebiete und Einzelfragen Stehende Gewässer (Seenkunde, Limnologie) (DE-627)1271498529 (DE-625)rvk/142220:12707 (DE-576)201498529 38.21 Paläobotanik SEPA (DE-627)106408216 38.19 Historische Geologie: Sonstiges SEPA (DE-627)106408232 BO 20 01 0084 653258089 x 22-06-04 21 01 0046 659683059 z 13-08-04 22 01 0018 653359993 SUBolrd xu 22-06-04 30 01 0104 71985377X z 14-05-05 40 01 0007 653455518 ksn 23-06-04 60 01 0705 653554125 z 23-06-04 110 01 3110 719853788 xz 14-05-05 285 01 0517 117738504X OLR-EXT z 18-08-10 370 01 4370 822431599 x 08-06-07 20 01 0084 http://d-nb.info/968701655 21 01 0046 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 30 01 0104 http://d-nb.info/968701655 40 01 0007 http://webdoc.sub.gwdg.de/ebook/serien/tm-v/STR/0303.pdf 40 01 0007 Lizenzbedingungen http://creativecommons.org/licenses/by-nc-sa/3.0/de/ 60 01 0705 http://d-nb.info/968701655 110 01 3110 http://d-nb.info/968701655 285 01 0517 Open Access http://nbn-resolving.de/urn:nbn:de:kobv:b103-030084 370 01 4370 http://deposit.ddb.de/cgi-bin/dokserv?idn=968701655 60 01 0705 10 ho 285 00 DE-517 00 TF 04999 285 00 DE-517 00 TQ 01040 285 00 DE-517 00 TP 05078 285 00 DE-517 00 TP 5078 285 00 DE-517 00 TQ 1040 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 285 01 0517 OLR-EXT 40 01 0007 2004-06 9
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fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a2200265 4500</leader><controlfield tag="001">37021854X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240708235312.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">030924s2003 gw \|\|\|\|\|om 00\| \|\|ger c</controlfield><datafield tag="015" ind1=" " ind2=" "><subfield code="a">03,A41,0885</subfield><subfield code="2">dnb</subfield></datafield><datafield tag="016" ind1="7" ind2=" "><subfield code="a">968701655</subfield><subfield code="2">DE-101</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">urn:nbn:de:kobv:b103-030084</subfield><subfield code="2">urn</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)37021854X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DNB968701655</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)76627281</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">ger</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">31</subfield><subfield code="2">sdnb</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">32</subfield><subfield code="2">sdnb</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">16,13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RB 10360</subfield><subfield code="q">SEPA</subfield><subfield code="2">rvk</subfield><subfield code="0">(DE-625)rvk/142220:12707</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.21</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.19</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Diatomeen als Indikatoren für Umwelt- und Klimaänderungen</subfield><subfield code="b">eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel</subfield><subfield code="c">Geoforschungszentrum Potsdam. Von Janina Baier</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Potsdam</subfield><subfield code="b">Geoforschungszentrum</subfield><subfield code="c">[2003]</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource (PDF-Datei: XVI, 181 S., 22 MB)</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">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="490" ind1="1" ind2=" "><subfield code="a">Scientific technical report / Geoforschungszentrum Potsdam</subfield><subfield code="v">2003,03</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="a">Zugl.: Potsdam, Univ., Diss, 2002</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. 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title	Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel
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title_full	Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel Geoforschungszentrum Potsdam. Von Janina Baier
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title_sort	diatomeen als indikatoren für umwelt- und klimaänderungeneine mittel- bis spätholozäne paläolimnologische studie am holzmaar, westeifel
title_auth	Diatomeen als Indikatoren für Umwelt- und Klimaänderungen eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel
abstract	The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability.
abstractGer	The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability.
abstract_unstemmed	The objective of this study was to reconstruct the palaeolimnological history of Lake Holzmaar, Germany in order to infer palaeoclimatological changes and to track anthropogenic activity during the time-span investigated (ca. 6340 - 1470 cal yr BP). Fossil diatom assemblages, geochemical parameters and varve substructure were used as basic tools for further reconstructions. The combined consideration of all proxy gathered information allowed to infer causally determined changes in diatom assemblage composition, annual algae succession and productivity. For example, it was deduced that changes in lake circulation patterns, precipitation rates and/or erosion rates which are ultimately controlled by climate, caused shifts in nutrient ratios and/or concentrations (e.g., silica and phosphorus) and subsequently in fossil algae composition. Major lacustrine changes which occurred ca. 5800, 5100, 4500, 3660 and 2660 cal yr BP correspond to glacier movements or to lake level changes observed at different locations in western Europe which may reflect large-scale Holocene variability over western Europe. In how far decreasing solar activity as it is proposed for the time around 2660 cal yr BP led to major changes within the lake and in the lake's catchment is difficult to disentangle from anthropogenic activity which increased sharply with the beginning of the Iron Age as evidenced by palynology and archaeology. A satisfying discrimination of anthropogenic and climate influence upon the lake is one of the future goals. A further aim is to look for possible periodicities inherent in the varve formation investigated. Answering those questions will help to better understand natural climatic processes and will allow to make suggestions upon future climate variability.
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title_short	Diatomeen als Indikatoren für Umwelt- und Klimaänderungen
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Diatomeen als Indikatoren für Umwelt- und Klimaänderungen : eine mittel- bis spätholozäne paläolimnologische Studie am Holzmaar, Westeifel

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