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• W2904866577 endingPage "75" @default.
• W2904866577 startingPage "62" @default.
• W2904866577 abstract "Diatom-based transfer functions for salinity, precipitation and temperature were developed using a training set that included data from 40 sites along central Mexico. These transfer functions showed good performance parameters and were subsequently applied to the previously published diatom record from lake Chalco, southern Basin of Mexico. Heinrich stadials (HS-3 to HS-0) were reconstructed as cold and dry events, with HS-2 representing the coldest and driest conditions, while HS-1 shows a complex bimodal cooling pattern. Orbital scale variability is also recorded. High and variable lake salinities from ∼34 to 29 ka BP (marine isotope stage 3, MIS-3) corresponded with times of maximum summer insolation and evidences of frequent fires. MIS-2 was identified as a cold period, with low lake salinity associated with low evaporation, with two cold intervals during the minima in spring (∼25.5 ka BP) and summer (∼20 ka BP) insolation. The ∼20 ka BP cold event together with HS-2 (24-23 ka BP), defined a bimodal maximum cooling during the last glacial maximum (LGM: 24.5–19.5 ka BP) within the range of pollen-based estimates, further supporting a maximum tropical cooling of 4–5 °C for the LGM. The deglacial (19.5–11.5 ka BP) showed the highest precipitation anomalies with three peaks that closely correlated with glacier advances in the nearby mountains (Iztaccihuatl). The early Holocene marked a change towards high lake salinities and the highest positive temperature anomalies (+3.5 °C) during a peak in summer insolation. Even though at orbital scale Chalco showed a nearly opposite trend to the record from the more southerly lake Peten-Itza (Guatemala), at millennial scale it showed a common pattern of cold and dry conditions during HSs, comparable to other tropical latitude sites in the northern hemisphere and further supporting the idea that there is a strong coupling between tropical and higher latitudes climates, in particular with the North Atlantic." @default.
• W2904866577 created "2018-12-22" @default.
• W2904866577 creator A5000338590 @default.
• W2904866577 creator A5040889393 @default.
• W2904866577 creator A5041678044 @default.
• W2904866577 creator A5055989895 @default.
• W2904866577 date "2019-02-01" @default.
• W2904866577 modified "2023-09-30" @default.
• W2904866577 title "Quantitative estimates of orbital and millennial scale climatic variability in central Mexico during the last ∼40,000 years" @default.
• W2904866577 cites W1083341005 @default.
• W2904866577 cites W1491826018 @default.
• W2904866577 cites W1510012572 @default.
• W2904866577 cites W1587911419 @default.
• W2904866577 cites W1892393967 @default.
• W2904866577 cites W1923552056 @default.
• W2904866577 cites W1964845163 @default.
• W2904866577 cites W1968721411 @default.
• W2904866577 cites W1970850180 @default.
• W2904866577 cites W1971261222 @default.
• W2904866577 cites W1975075226 @default.
• W2904866577 cites W1975715178 @default.
• W2904866577 cites W1976191192 @default.
• W2904866577 cites W1977192625 @default.
• W2904866577 cites W1977355907 @default.
• W2904866577 cites W1980411723 @default.
• W2904866577 cites W1981594027 @default.
• W2904866577 cites W1981817013 @default.
• W2904866577 cites W1982444887 @default.
• W2904866577 cites W1990021520 @default.
• W2904866577 cites W1994654438 @default.
• W2904866577 cites W1999125016 @default.
• W2904866577 cites W2001072306 @default.
• W2904866577 cites W2002149221 @default.
• W2904866577 cites W2002518221 @default.
• W2904866577 cites W2002717773 @default.
• W2904866577 cites W2006604282 @default.
• W2904866577 cites W2008875043 @default.
• W2904866577 cites W2010236289 @default.
• W2904866577 cites W2013488438 @default.
• W2904866577 cites W2015208407 @default.
• W2904866577 cites W2015738534 @default.
• W2904866577 cites W2022175623 @default.
• W2904866577 cites W2026775241 @default.
• W2904866577 cites W2029438656 @default.
• W2904866577 cites W2039969769 @default.
• W2904866577 cites W2040979489 @default.
• W2904866577 cites W2043424679 @default.
• W2904866577 cites W2048327809 @default.
• W2904866577 cites W2051126029 @default.
• W2904866577 cites W2051785786 @default.
• W2904866577 cites W2058767524 @default.
• W2904866577 cites W2059286950 @default.
• W2904866577 cites W2061696469 @default.
• W2904866577 cites W2063866263 @default.
• W2904866577 cites W2064470080 @default.
• W2904866577 cites W2064680900 @default.
• W2904866577 cites W2065036851 @default.
• W2904866577 cites W2066909033 @default.
• W2904866577 cites W2067984119 @default.
• W2904866577 cites W2068473379 @default.
• W2904866577 cites W2071555715 @default.
• W2904866577 cites W2072848460 @default.
• W2904866577 cites W2076291503 @default.
• W2904866577 cites W2084428435 @default.
• W2904866577 cites W2086192317 @default.
• W2904866577 cites W2087115681 @default.
• W2904866577 cites W2091794178 @default.
• W2904866577 cites W2094173026 @default.
• W2904866577 cites W2096075169 @default.
• W2904866577 cites W2103109669 @default.
• W2904866577 cites W2111220291 @default.
• W2904866577 cites W2112829287 @default.
• W2904866577 cites W2115758280 @default.
• W2904866577 cites W2118282237 @default.
• W2904866577 cites W2126404012 @default.
• W2904866577 cites W2156207679 @default.
• W2904866577 cites W2157088641 @default.
• W2904866577 cites W2157975078 @default.
• W2904866577 cites W2167941657 @default.
• W2904866577 cites W2191532423 @default.
• W2904866577 cites W2271570680 @default.
• W2904866577 cites W2396275005 @default.
• W2904866577 cites W2752988389 @default.
• W2904866577 cites W2770305774 @default.
• W2904866577 cites W2770412130 @default.
• W2904866577 cites W3043877689 @default.
• W2904866577 cites W320971603 @default.
• W2904866577 cites W4246027503 @default.
• W2904866577 cites W4249751050 @default.
• W2904866577 cites W80417349 @default.
• W2904866577 doi "https://doi.org/10.1016/j.quascirev.2018.12.002" @default.
• W2904866577 hasPublicationYear "2019" @default.
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