FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4205800900> ?p ?o ?g. }

• W4205800900 endingPage "107345" @default.
• W4205800900 startingPage "107345" @default.
• W4205800900 abstract "Global and regional reconstructions of past climate conditions often incorporate sea surface temperature (SST) estimates from multiple proxies because not every paleotemperature proxy is applicable in all geographic locations. This practice of assimilating estimates from different proxies in global or regional temperature syntheses makes the implicit assumption that estimates derived from different proxies can be meaningfully intercompared. However, evidence to support the validity of this assumption is limited. Using paleotemperature data from sediments collected from ODP Site 1125 in the Southwest Pacific, we conduct a ∼1 Myr, orbital-scale SST proxy comparison of a recently published alkenone-derived SST record with a previously published foraminiferal assemblage-based SST record. These alkenone and foraminiferal assemblage SST datasets show strong structural similarity and yield remarkably similar estimates for basic climate metrics, including mean, median, standard deviation, and range. Statistical analysis indicates that the correlation between the two SST records is highly significant. In the spectral domain, the records share the same dominant 100 kyr beat, are coherent and in phase with each other at this frequency, and have the same coherence and phase relationship with benthic foraminiferal δ 18 O. Results from this work demonstrate that these two proxies would yield very similar estimates for the paleoclimate metrics most commonly used in empirical paleoclimate reconstructions that seek to document the evolution of climate over this interval. However, significant disparities between SST estimates derived from the two proxies exist for some time periods, particularly during glacial and interglacial extrema. This comparison suggests that treating estimates from these proxies as equivalent in studies that focus on short time windows (e.g. a few thousand to tens-of-thousands of years), particularly in investigations that seek to characterize glacial or interglacial extrema, could be potentially problematic. However, the sensitive location of Site 1125, just north of the Subtropical Front, likely accentuates the difference between temperature estimates from these proxies, which may be attenuated in other oceanographic settings. We attribute the discrepancies between the two SST records to two main causes: seasonal leakages of cold water across the Subtropical Front during glacial extrema and differential seasonality of maximum alkenone and foraminiferal production. • U k’ 37 and foraminiferal temperature proxies produce similar estimates of basic metrics. • Results suggest these paleothermometers can be used interchangeably in most contexts. • Temperature discrepancies occur during some glacial and interglacial extrema. • We attribute proxy differences to seasonal changes in circulation and production. • A sensitive site location accentuates the differences in proxy temperature estimates." @default.
• W4205800900 created "2022-01-25" @default.
• W4205800900 creator A5047495201 @default.
• W4205800900 creator A5052301786 @default.
• W4205800900 creator A5064756534 @default.
• W4205800900 creator A5084973294 @default.
• W4205800900 date "2022-02-01" @default.
• W4205800900 modified "2023-10-17" @default.
• W4205800900 title "A comparison of orbital-resolution, Late Pleistocene Alkenone and foraminiferal assemblage-based sea surface temperature reconstructions from the Southwest Pacific" @default.
• W4205800900 cites W1481746305 @default.
• W4205800900 cites W1496478109 @default.
• W4205800900 cites W1524265891 @default.
• W4205800900 cites W1529788121 @default.
• W4205800900 cites W1552639527 @default.
• W4205800900 cites W1553679754 @default.
• W4205800900 cites W1583929961 @default.
• W4205800900 cites W1591226734 @default.
• W4205800900 cites W1602499579 @default.
• W4205800900 cites W1624405180 @default.
• W4205800900 cites W1625329436 @default.
• W4205800900 cites W1658855455 @default.
• W4205800900 cites W169497166 @default.
• W4205800900 cites W1697017870 @default.
• W4205800900 cites W1731626208 @default.
• W4205800900 cites W1938705403 @default.
• W4205800900 cites W1963864161 @default.
• W4205800900 cites W1964474941 @default.
• W4205800900 cites W1968769526 @default.
• W4205800900 cites W1971681662 @default.
• W4205800900 cites W1973193929 @default.
• W4205800900 cites W1973333868 @default.
• W4205800900 cites W1975437766 @default.
• W4205800900 cites W1985342839 @default.
• W4205800900 cites W1986272933 @default.
• W4205800900 cites W1986785608 @default.
• W4205800900 cites W1991795942 @default.
• W4205800900 cites W1998429604 @default.
• W4205800900 cites W1999651672 @default.
• W4205800900 cites W2001575273 @default.
• W4205800900 cites W2011698375 @default.
• W4205800900 cites W2012592445 @default.
• W4205800900 cites W2014145546 @default.
• W4205800900 cites W2019161985 @default.
• W4205800900 cites W2024614197 @default.
• W4205800900 cites W2026985846 @default.
• W4205800900 cites W2027204577 @default.
• W4205800900 cites W2031171042 @default.
• W4205800900 cites W2032286202 @default.
• W4205800900 cites W2032720950 @default.
• W4205800900 cites W2037580998 @default.
• W4205800900 cites W2038706413 @default.
• W4205800900 cites W2045522086 @default.
• W4205800900 cites W2047273304 @default.
• W4205800900 cites W2052353740 @default.
• W4205800900 cites W2053251742 @default.
• W4205800900 cites W2054903019 @default.
• W4205800900 cites W2064341563 @default.
• W4205800900 cites W2067139325 @default.
• W4205800900 cites W2071510155 @default.
• W4205800900 cites W2073675853 @default.
• W4205800900 cites W2083345887 @default.
• W4205800900 cites W2088899781 @default.
• W4205800900 cites W2091232642 @default.
• W4205800900 cites W2091284813 @default.
• W4205800900 cites W2094849893 @default.
• W4205800900 cites W2095888397 @default.
• W4205800900 cites W2096425009 @default.
• W4205800900 cites W2096904991 @default.
• W4205800900 cites W2100867515 @default.
• W4205800900 cites W2101283217 @default.
• W4205800900 cites W2115280287 @default.
• W4205800900 cites W2118387673 @default.
• W4205800900 cites W2120259424 @default.
• W4205800900 cites W2120537950 @default.
• W4205800900 cites W2120560331 @default.
• W4205800900 cites W2122670956 @default.
• W4205800900 cites W2133830815 @default.
• W4205800900 cites W2149432953 @default.
• W4205800900 cites W2152621432 @default.
• W4205800900 cites W2288613658 @default.
• W4205800900 cites W2418090251 @default.
• W4205800900 cites W2522906567 @default.
• W4205800900 cites W2560207916 @default.
• W4205800900 cites W2589961917 @default.
• W4205800900 cites W2734484686 @default.
• W4205800900 cites W2792554943 @default.
• W4205800900 cites W2987073494 @default.
• W4205800900 cites W3007134866 @default.
• W4205800900 cites W3025085465 @default.
• W4205800900 cites W3123157889 @default.
• W4205800900 cites W4252684946 @default.
• W4205800900 doi "https://doi.org/10.1016/j.quascirev.2021.107345" @default.
• W4205800900 hasPublicationYear "2022" @default.
• W4205800900 type Work @default.
• W4205800900 citedByCount "0" @default.
• W4205800900 crossrefType "journal-article" @default.
• W4205800900 hasAuthorship W4205800900A5047495201 @default.
• W4205800900 hasAuthorship W4205800900A5052301786 @default.

• next