Historical reconstruction of sediment accumulation rates as an indicator of global change impacts in a tropical crater lake
Lakes are effective sentinels of global change owing to their sensitivity to land-use changes and climate variability in their catchment. Santa María del Oro Lake (SAMO, NW Mexico) is of interest both for global change studies and as a natural resource to sustain the economy of local communities. Fo...
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| Veröffentlicht in: | Journal of paleolimnology 2022-12, Vol.68 (4), p.395-413 |
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| creator | Ruiz-Fernández, A. C. Sanchez-Cabeza, J. A. Blaauw, M. Pérez-Bernal, L. H. Cardoso-Mohedano, J. G. Aquino-López, M. A. Keaveney, E. Giralt, S. |
| description | Lakes are effective sentinels of global change owing to their sensitivity to land-use changes and climate variability in their catchment. Santa María del Oro Lake (SAMO, NW Mexico) is of interest both for global change studies and as a natural resource to sustain the economy of local communities. Four sediment cores were used to evaluate the temporal variations of sediment accumulation, under the hypothesis that changes in sediment input are mostly driven by anthropic activities developed in the lake surroundings. Radiocarbon (
14
C) dating of SAMO sediments was precluded by a large and variable reservoir effect, inducing an age offset of ~ 4000 years. Well-constrained chronologies over the past century were obtained by
210
Pb dating, corroborated by the stratigraphic markers
137
Cs,
239+240
Pu, and
14
C-fraction modern. Geochemical, magnetic susceptibility, and meteorological data were used to elucidate the main controls of sedimentation processes in the lake. Mass accumulation rates were high, likely because of the natural vulnerability of catchment soils to hydric and aeolian erosion. The highest values, observed towards the lakeshore, were attributed to the influence of seasonal runoff from the surrounding steep hills, and the proximity of human settlements and agricultural fields. Mean mass accumulation rates increased with time (from 0.03 ± 0.01 g cm
−2
year
−1
between 1900 and 1950, to 0.14 ± 0.10 g cm
−2
year
−1
after the 1950s), although the most recent values were comparable to the mean values during the pre-1950 period. Accumulation maxima across the lake, occurring mostly since the 1980s, concurred with precipitation minima and were related to terrigenous pulses associated with soil erosion, likely favored by lower soil humidity and the occurrence of wildfires during dryer years. Controls on the development of human settlement and agriculture practices should be included in the long-term environmental management plans for the conservation of the lake resources. |
| doi_str_mv | 10.1007/s10933-022-00254-9 |
| format | Article |
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14
C) dating of SAMO sediments was precluded by a large and variable reservoir effect, inducing an age offset of ~ 4000 years. Well-constrained chronologies over the past century were obtained by
210
Pb dating, corroborated by the stratigraphic markers
137
Cs,
239+240
Pu, and
14
C-fraction modern. Geochemical, magnetic susceptibility, and meteorological data were used to elucidate the main controls of sedimentation processes in the lake. Mass accumulation rates were high, likely because of the natural vulnerability of catchment soils to hydric and aeolian erosion. The highest values, observed towards the lakeshore, were attributed to the influence of seasonal runoff from the surrounding steep hills, and the proximity of human settlements and agricultural fields. Mean mass accumulation rates increased with time (from 0.03 ± 0.01 g cm
−2
year
−1
between 1900 and 1950, to 0.14 ± 0.10 g cm
−2
year
−1
after the 1950s), although the most recent values were comparable to the mean values during the pre-1950 period. Accumulation maxima across the lake, occurring mostly since the 1980s, concurred with precipitation minima and were related to terrigenous pulses associated with soil erosion, likely favored by lower soil humidity and the occurrence of wildfires during dryer years. Controls on the development of human settlement and agriculture practices should be included in the long-term environmental management plans for the conservation of the lake resources.</description><identifier>ISSN: 0921-2728</identifier><identifier>EISSN: 1573-0417</identifier><identifier>DOI: 10.1007/s10933-022-00254-9</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Accumulation ; Agricultural land ; Agricultural practices ; Caesium 137 ; Catchment area ; Cesium 137 ; Cesium isotopes ; Cesium radioisotopes ; Climate Change ; Climate variability ; Cores ; Dating ; Earth and Environmental Science ; Earth Sciences ; Environmental management ; Freshwater & Marine Ecology ; Geology ; Human settlements ; Lake shores ; Lakes ; Land use ; Lead isotopes ; Local communities ; Magnetic permeability ; Magnetic susceptibility ; Meteorological data ; Natural resources ; Original Paper ; Paleontology ; Physical Geography ; Plutonium isotopes ; Radiocarbon dating ; Radiometric dating ; Runoff ; Sediment ; Sedimentology ; Sediments ; Soil erosion ; Stratigraphy ; Temporal variations ; Vulnerability ; Wildfires</subject><ispartof>Journal of paleolimnology, 2022-12, Vol.68 (4), p.395-413</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2022. Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-e079454762780f4542c6a96aa7ec94190a519f64d9cd93dfb0238996764a24ba3</citedby><cites>FETCH-LOGICAL-c319t-e079454762780f4542c6a96aa7ec94190a519f64d9cd93dfb0238996764a24ba3</cites><orcidid>0000-0002-2515-1249</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10933-022-00254-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10933-022-00254-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Ruiz-Fernández, A. C.</creatorcontrib><creatorcontrib>Sanchez-Cabeza, J. A.</creatorcontrib><creatorcontrib>Blaauw, M.</creatorcontrib><creatorcontrib>Pérez-Bernal, L. H.</creatorcontrib><creatorcontrib>Cardoso-Mohedano, J. G.</creatorcontrib><creatorcontrib>Aquino-López, M. A.</creatorcontrib><creatorcontrib>Keaveney, E.</creatorcontrib><creatorcontrib>Giralt, S.</creatorcontrib><title>Historical reconstruction of sediment accumulation rates as an indicator of global change impacts in a tropical crater lake</title><title>Journal of paleolimnology</title><addtitle>J Paleolimnol</addtitle><description>Lakes are effective sentinels of global change owing to their sensitivity to land-use changes and climate variability in their catchment. Santa María del Oro Lake (SAMO, NW Mexico) is of interest both for global change studies and as a natural resource to sustain the economy of local communities. Four sediment cores were used to evaluate the temporal variations of sediment accumulation, under the hypothesis that changes in sediment input are mostly driven by anthropic activities developed in the lake surroundings. Radiocarbon (
14
C) dating of SAMO sediments was precluded by a large and variable reservoir effect, inducing an age offset of ~ 4000 years. Well-constrained chronologies over the past century were obtained by
210
Pb dating, corroborated by the stratigraphic markers
137
Cs,
239+240
Pu, and
14
C-fraction modern. Geochemical, magnetic susceptibility, and meteorological data were used to elucidate the main controls of sedimentation processes in the lake. Mass accumulation rates were high, likely because of the natural vulnerability of catchment soils to hydric and aeolian erosion. The highest values, observed towards the lakeshore, were attributed to the influence of seasonal runoff from the surrounding steep hills, and the proximity of human settlements and agricultural fields. Mean mass accumulation rates increased with time (from 0.03 ± 0.01 g cm
−2
year
−1
between 1900 and 1950, to 0.14 ± 0.10 g cm
−2
year
−1
after the 1950s), although the most recent values were comparable to the mean values during the pre-1950 period. Accumulation maxima across the lake, occurring mostly since the 1980s, concurred with precipitation minima and were related to terrigenous pulses associated with soil erosion, likely favored by lower soil humidity and the occurrence of wildfires during dryer years. Controls on the development of human settlement and agriculture practices should be included in the long-term environmental management plans for the conservation of the lake resources.</description><subject>Accumulation</subject><subject>Agricultural land</subject><subject>Agricultural practices</subject><subject>Caesium 137</subject><subject>Catchment area</subject><subject>Cesium 137</subject><subject>Cesium isotopes</subject><subject>Cesium radioisotopes</subject><subject>Climate Change</subject><subject>Climate variability</subject><subject>Cores</subject><subject>Dating</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental management</subject><subject>Freshwater & Marine Ecology</subject><subject>Geology</subject><subject>Human settlements</subject><subject>Lake shores</subject><subject>Lakes</subject><subject>Land use</subject><subject>Lead isotopes</subject><subject>Local communities</subject><subject>Magnetic permeability</subject><subject>Magnetic susceptibility</subject><subject>Meteorological data</subject><subject>Natural resources</subject><subject>Original Paper</subject><subject>Paleontology</subject><subject>Physical Geography</subject><subject>Plutonium isotopes</subject><subject>Radiocarbon dating</subject><subject>Radiometric dating</subject><subject>Runoff</subject><subject>Sediment</subject><subject>Sedimentology</subject><subject>Sediments</subject><subject>Soil erosion</subject><subject>Stratigraphy</subject><subject>Temporal variations</subject><subject>Vulnerability</subject><subject>Wildfires</subject><issn>0921-2728</issn><issn>1573-0417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kEFLwzAYhoMoOKd_wFPAc_VLmjbNUYY6YeBFz-Fbms7OtqlJehD_vNkqeBMCCcnzvB95CblmcMsA5F1goPI8A84zAF6ITJ2QBStkuhJMnpIFKM4yLnl1Ti5C2AOAqmSxIN_rNkTnW4Md9da4IUQ_mdi6gbqGBlu3vR0iRWOmfurw-OAx2kAxrYG2Q53clHDAd53bphzzjsPO0rYf0cSQEIo0ejceh5iD7WmHH_aSnDXYBXv1uy_J2-PD62qdbV6enlf3m8zkTMXMglSiELLksoImnbgpUZWI0holmAIsmGpKUStTq7xutsDzSqlSlgK52GK-JDdz7ujd52RD1Hs3-SGN1KkRphILLFF8pox3IXjb6NG3PfovzUAfStZzyTqVrI8la5WkfJZCgtOn_V_0P9YPKfmAeQ</recordid><startdate>20221201</startdate><enddate>20221201</enddate><creator>Ruiz-Fernández, A. 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A.</creator><creator>Keaveney, E.</creator><creator>Giralt, S.</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7T7</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H94</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M7N</scope><scope>M7P</scope><scope>P64</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><orcidid>https://orcid.org/0000-0002-2515-1249</orcidid></search><sort><creationdate>20221201</creationdate><title>Historical reconstruction of sediment accumulation rates as an indicator of global change impacts in a tropical crater lake</title><author>Ruiz-Fernández, A. C. ; Sanchez-Cabeza, J. A. ; Blaauw, M. ; Pérez-Bernal, L. H. ; Cardoso-Mohedano, J. G. ; Aquino-López, M. 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C.</au><au>Sanchez-Cabeza, J. A.</au><au>Blaauw, M.</au><au>Pérez-Bernal, L. H.</au><au>Cardoso-Mohedano, J. G.</au><au>Aquino-López, M. A.</au><au>Keaveney, E.</au><au>Giralt, S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Historical reconstruction of sediment accumulation rates as an indicator of global change impacts in a tropical crater lake</atitle><jtitle>Journal of paleolimnology</jtitle><stitle>J Paleolimnol</stitle><date>2022-12-01</date><risdate>2022</risdate><volume>68</volume><issue>4</issue><spage>395</spage><epage>413</epage><pages>395-413</pages><issn>0921-2728</issn><eissn>1573-0417</eissn><abstract>Lakes are effective sentinels of global change owing to their sensitivity to land-use changes and climate variability in their catchment. Santa María del Oro Lake (SAMO, NW Mexico) is of interest both for global change studies and as a natural resource to sustain the economy of local communities. Four sediment cores were used to evaluate the temporal variations of sediment accumulation, under the hypothesis that changes in sediment input are mostly driven by anthropic activities developed in the lake surroundings. Radiocarbon (
14
C) dating of SAMO sediments was precluded by a large and variable reservoir effect, inducing an age offset of ~ 4000 years. Well-constrained chronologies over the past century were obtained by
210
Pb dating, corroborated by the stratigraphic markers
137
Cs,
239+240
Pu, and
14
C-fraction modern. Geochemical, magnetic susceptibility, and meteorological data were used to elucidate the main controls of sedimentation processes in the lake. Mass accumulation rates were high, likely because of the natural vulnerability of catchment soils to hydric and aeolian erosion. The highest values, observed towards the lakeshore, were attributed to the influence of seasonal runoff from the surrounding steep hills, and the proximity of human settlements and agricultural fields. Mean mass accumulation rates increased with time (from 0.03 ± 0.01 g cm
−2
year
−1
between 1900 and 1950, to 0.14 ± 0.10 g cm
−2
year
−1
after the 1950s), although the most recent values were comparable to the mean values during the pre-1950 period. Accumulation maxima across the lake, occurring mostly since the 1980s, concurred with precipitation minima and were related to terrigenous pulses associated with soil erosion, likely favored by lower soil humidity and the occurrence of wildfires during dryer years. Controls on the development of human settlement and agriculture practices should be included in the long-term environmental management plans for the conservation of the lake resources.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-022-00254-9</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0002-2515-1249</orcidid></addata></record> |
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| ispartof | Journal of paleolimnology, 2022-12, Vol.68 (4), p.395-413 |
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| language | eng |
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| source | SpringerNature Journals |
| subjects | Accumulation Agricultural land Agricultural practices Caesium 137 Catchment area Cesium 137 Cesium isotopes Cesium radioisotopes Climate Change Climate variability Cores Dating Earth and Environmental Science Earth Sciences Environmental management Freshwater & Marine Ecology Geology Human settlements Lake shores Lakes Land use Lead isotopes Local communities Magnetic permeability Magnetic susceptibility Meteorological data Natural resources Original Paper Paleontology Physical Geography Plutonium isotopes Radiocarbon dating Radiometric dating Runoff Sediment Sedimentology Sediments Soil erosion Stratigraphy Temporal variations Vulnerability Wildfires |
| title | Historical reconstruction of sediment accumulation rates as an indicator of global change impacts in a tropical crater lake |
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