2004
DOI: 10.1029/2004eo490010
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Global impact of the Panamanian seaway closure

Abstract: Closure of the Isthmus of Panama about 3 million years ago (Ma) was accompanied by dramatic changes in Earth's climate and biosphere. The Greenland ice sheet grew to continental extent and the great cycles of ice ages commenced dominating climate variability henceforth. Disruption of water mass exchange between the Atlantic and the Pacific Oceans led to different evolution of marine species on either side of the land bridge, while land‐based organisms including mammals and other animals took the advantage to c… Show more

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Cited by 20 publications
(3 citation statements)
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“…However, with the Central American Seaway open, AMOC overturning is weakened bỹ 33% relative to the case of Drake Passage open but Central American Seaway closed (Fig. 2b), due to a steric-height-driven 17 Sv influx of fresher Pacific water into the Atlantic through the Central American Seaway, in agreement with previous studies (Keigwin, 1982;Schmittner et al, 2004;Schneider and Schmittner, 2006;Yang et al, 2014). In the southern hemisphere, for all CO 2 concentrations, the AABW circulation cell is stronger and larger when the Drake Passage is closed, in agreement with previous studies (Mikolajewicz et al, 1993) (Fig.…”
Section: Drake Passage Openingsupporting
confidence: 90%
“…However, with the Central American Seaway open, AMOC overturning is weakened bỹ 33% relative to the case of Drake Passage open but Central American Seaway closed (Fig. 2b), due to a steric-height-driven 17 Sv influx of fresher Pacific water into the Atlantic through the Central American Seaway, in agreement with previous studies (Keigwin, 1982;Schmittner et al, 2004;Schneider and Schmittner, 2006;Yang et al, 2014). In the southern hemisphere, for all CO 2 concentrations, the AABW circulation cell is stronger and larger when the Drake Passage is closed, in agreement with previous studies (Mikolajewicz et al, 1993) (Fig.…”
Section: Drake Passage Openingsupporting
confidence: 90%
“…Applying a common crustacean mtCOI mutation rate of 1.4% per million years (Knowlton and Weigt, 1998), PLAB1 and PLAB2 share a common ancestor dating back to the Miocene (11.6-16.0 million years ago) or before. A global-scale cooling event began in the middle Miocene (Zachos et al, 2001), and both the ocean environment and geography have changed towards the present, including the formation of the Isthmus of Panama (Schmittner et al, 2004) and increased primary productivity in equatorial regions (Barron, 1985;Rea et al, 1991).…”
Section: Mechanisms Determining the Biogeography Of Mtcoi Cladesmentioning
confidence: 99%
“…The low genetic divergence of M. geyeri and M. bracteosa, could be an example of vicariance related to the Panamanian seaway closure (Schmittner et al 2004). Species are genetically close and share similar niches in geographically separated areas (Faure et al 2015;Hiller & Lessios 2019).…”
Section: Tablementioning
confidence: 99%