Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Annette Olivarez Lyle"'
Publikováno v:
Paleoceanography. 27
[1] The equatorial Pacific is an important part of the global carbon cycle and has been affected by climate change through the Cenozoic (65 Ma to present). We present a Miocene (12–24 Ma) biogenic sediment record from Deep Sea Drilling Project (DSD
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18e25fee53a6d40493dd0a33cbdfa845
https://doi.org/10.1029/2011pa002236
https://doi.org/10.1029/2011pa002236
Autor:
C. Ravelo, Dyke Andreasen, Annette Olivarez Lyle, Noah S. Diffenbaugh, Linda E. Heusser, Mitchell W Lyle
Publikováno v:
Paleoceanography. 25
[1] Coastal marine sediments contain mixtures of terrestrial and marine paleoclimate proxies that record how the coastal water cycle has behaved over long time frames. We explore a 600 kyr marine record from ODP Site 1018, located due west of Santa C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9af92fcc87c791b993beb2f15366cb5
https://doi.org/10.1029/2009pa001836
https://doi.org/10.1029/2009pa001836
Autor:
Adina Paytan, Annette Olivarez-Lyle, Kristen Averyt, Michael Calhoun, Elizabeth M. Griffith, Andrea M. Erhardt, Mitch Lyle, Ellen Thomas, Timothy J. Bralower
Publikováno v:
Paleoceanography. 25
[1] The late Eocene through earliest Oligocene (40–32 Ma) spans a major transition from greenhouse to icehouse climate, with net cooling and expansion of Antarctic glaciation shortly after the Eocene/Oligocene (E/O) boundary. We investigated the re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b1dcc703758d5145506e18fe60079b4
https://doi.org/10.1029/2010pa001932
https://doi.org/10.1029/2010pa001932
Autor:
A. Christina Ravelo, David K. Rea, Timothy J. Bralower, Paul A. Wilson, Mitchell W Lyle, Annette Olivarez Lyle, Matthew Huber, John A. Barron
Publikováno v:
Department of Earth, Atmospheric, and Planetary Sciences Faculty Publications
[1] The Pacific Ocean has played a major role in climate evolution throughout the Cenozoic (65–0 Ma). It is a fundamental component of global heat transport and circulation, the dominant locus of primary productivity, and, consequently, the largest
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9c35bd18d606c063c2bfd7c1d7acc695
https://doi.org/10.1029/2005rg000190
https://doi.org/10.1029/2005rg000190
Publikováno v:
Paleoceanography. 23
[2] The Eocene biosiliceous oozes of the tropical Pacific are an easily recognizable sediment type having a reddish brown color and sugary texture. These sediments are dominated by radiolarian tests, with traces of terrigenous debris, hydrothermal ox
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a11472b5c818215fa20d10f6aa8d6e1a
https://doi.org/10.1029/2007pa001514
https://doi.org/10.1029/2007pa001514
Autor:
Annette Olivarez Lyle, Mitchell W Lyle
Publikováno v:
Paleoceanography. 21
[1] Ocean chemistry is affected by pCO2 in the atmosphere by increasing the dissolution of solid calcium carbonate and elevating the dissolved inorganic carbon concentrations in seawater. Positive feedbacks between the ocean and atmosphere can mainta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9cb45ba171d97b9a768668c5ec1dc4a
https://doi.org/10.1029/2005pa001230
https://doi.org/10.1029/2005pa001230
Autor:
Mitchell W Lyle, Annette Olivarez Lyle, Michael W. Wara, Dyke Andreasen, Ana Christina Ravelo
Publikováno v:
Nature. 429(6989)
The Earth's climate has undergone a global transition over the past four million years, from warm conditions with global surface temperatures about 3 degrees C warmer than today, smaller ice sheets and higher sea levels to the current cooler conditio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c9c22823e3f247a578ce4c57a7c2991f
https://pubmed.ncbi.nlm.nih.gov/15152244
https://pubmed.ncbi.nlm.nih.gov/15152244