Zobrazeno 1 - 10
of 72
pro vyhledávání: '"Matthew S. Lachniet"'
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-11 (2022)
Abstract While climatic triggers for collapse and population migrations of ancestral Pueblo communities have been proposed, little is known about the overall climatic backdrop for the entire pre-Hispanic Pueblo period (ca. 1300 to 460 B2K). Here, we
Externí odkaz:
https://doaj.org/article/8bcc0a0803dd47778b471b046acec9a8
Autor:
J. P. Bernal, F. Revolorio, M. Cu-Xi, F. Lases-Hernández, P. Piacsek, Matthew S. Lachniet, Patrica A. Beddows, G. Lucia, K. López-Aguiar, S. Capella-Vizcaíno, R. López-Martínez, O. J. Vásquez
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Guatemala is located at the core of one of the largest warming pools in the planet, the Western Hemisphere Warm Pool, an important source of tropical moisture to middle and high latitudes and, thus, a key area for paleoclimatic studies. This, along t
Externí odkaz:
https://doaj.org/article/74b90acb34224565987ee7784d20d7db
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-7 (2017)
Abstract Large ocean-atmosphere and hydroclimate changes occurred during the last deglaciation, although the interplay between these changes remains ambiguous. Here, we present a speleothem-based high resolution record of Northern Hemisphere atmosphe
Externí odkaz:
https://doaj.org/article/45744b27e0234dc89cf9cffb98160359
Autor:
Andrew M. Lorrey, Paul W. Williams, John-Mark Woolley, Nicolas C. Fauchereau, Adam Hartland, Helen Bostock, Shaun Eaves, Matthew S. Lachniet, James A. Renwick, Vidya Varma
Publikováno v:
Quaternary, Vol 3, Iss 3, p 24 (2020)
We re-evaluated speleothem isotope series from Aotearoa New Zealand that were recently contributed to the Speleothem Isotopes Synthesis and AnaLysis (SISAL) database. COnstructing Proxy Records from Age Models (COPRA) software was used to produce Bay
Externí odkaz:
https://doaj.org/article/43fcb9e4d1d147fbb686c6e4148584c5
Autor:
Rhawn F. Denniston, S. A. Truebe, Naomi E. Levin, Julie E. Cole, David McGee, Benjamin H. Passey, Matthew S. Lachniet, Tyler E. Huth
Publikováno v:
Geochimica et Cosmochimica Acta. 319:191-219
Speleothem oxygen isotope (δ18O) records provide key insight into the rate and timing of terrestrial paleoclimate changes during the late Quaternary. However, it can be difficult to deconvolve the δ18O signal into individual components, which inclu
Publikováno v:
New Mexico Geological Society, 2022 Annual Spring Meeting, Proceedings Volume, Theme: "Karst in New Mexico in recognition of 2022 being the International Year of Caves and Karst".
Publikováno v:
Scientific reports. 12(1)
While climatic triggers for collapse and population migrations of ancestral Pueblo communities have been proposed, little is known about the overall climatic backdrop for the entire pre-Hispanic Pueblo period (ca. 1300 to 460 B2K). Here, we report da
Autor:
Ashley L. Brundrett, Kevin M. Theissen, Matthew S. Lachniet, Sarah E. Horns, Thomas A. Hickson
Publikováno v:
Quaternary Research. 92:352-364
We present a continuous, sediment core-based record of paleohydroclimate spanning ~5800 cal yr BP to recent from Lower Pahranagat Lake (LPAH), a shallow, alkaline lake in southern Nevada. We apply stable isotopes (δ18O and δ13C) from fine-fraction
Autor:
Matthew S. Lachniet, Haroon Stephen, Christina R. Riesselman, Andrew Lorrey, Christopher M. Moy
Publikováno v:
Paleoceanography and Paleoclimatology. 36
Autor:
Adam Hartland, Nicolas Fauchereau, James A. Renwick, Helen C Bostock, Shaun R. Eaves, Matthew S. Lachniet, Paul W. Williams, John-Mark Woolley, Andrew Lorrey, Vidya Varma
Publikováno v:
Quaternary
Volume 3
Issue 3
Quaternary, Vol 3, Iss 24, p 24 (2020)
Volume 3
Issue 3
Quaternary, Vol 3, Iss 24, p 24 (2020)
We re-evaluated speleothem isotope series from Aotearoa New Zealand that were recently contributed to the Speleothem Isotopes Synthesis and AnaLysis (SISAL) database. COnstructing Proxy Records from Age Models (COPRA) software was used to produce Bay
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::51b6c89d6bfac493baf1357d79c136dd
https://doi.org/10.26686/wgtn.13821866
https://doi.org/10.26686/wgtn.13821866