Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Pat Lohmann"'
Autor:
Hannah C. Barkley, Hanny E. Rivera, Sangeeta Mangubhai, Russell E. Brainard, Nathaniel R. Mollica, Elizabeth J. Drenkard, Charles W. Young, Andrew R. Solow, Pat Lohmann, Alice E. Alpert, Kathryn R. Pietro, Jessica Carilli, Celina Scott-Buechler, Thomas M. DeCarlo, Randi D. Rotjan, Anne L. Cohen
Publikováno v:
Coral Reefs. 38:743-757
Ocean warming is negatively impacting coral reef ecosystems and considerable effort is currently invested in projecting coral reef futures under 21st century climate change. A limiting factor in these projections is lack of quantitative data on the t
Autor:
George T.F. Wong, Kristen A. Davis, Kathryn E. F. Shamberger, Thomas M. DeCarlo, Anne L. Cohen, Fuh-Kwo Shiah, Steven J. Lentz, Pat Lohmann
Publikováno v:
Journal of Geophysical Research: Oceans. 122:745-761
Coral reefs are built of calcium carbonate (CaCO3) produced biogenically by a diversity of calcifying plants, animals, and microbes. As the ocean warms and acidifies, there is mounting concern that declining calcification rates could shift coral reef
Autor:
Celina Scott-Buechler, Sangeeta Mangubhai, Randi D. Rotjan, Andrew R. Solow, Hanny E. Rivera, Russell E. Brainard, Nathaniel R. Mollica, Thomas M. DeCarlo, Anne L. Cohen, Hannah C. Barkley, Elizabeth J. Drenkard, Alice E. Alpert, Kathryn R. Pietro, Pat Lohmann, Charles W. Young, Jessica Carilli
Publikováno v:
Coral Reefs. 38:1351-1352
Figure 2 in the original article has been updated with this figure 2 due to discrepancies related to incorrect mapping with one of the islands.
Autor:
Anne L. Cohen, Kristen A. Davis, Keryea Soong, Thomas M. DeCarlo, Pat Lohmann, George T.F. Wong
Publikováno v:
Scientific Reports
Nature
Nature
A 2 °C increase in global temperature above pre-industrial levels is considered a reasonable target for avoiding the most devastating impacts of anthropogenic climate change. In June 2015, sea surface temperature (SST) of the South China Sea (SCS) i
Publikováno v:
Geo-Marine Letters. 17:4-11
The Cote d’Ivoire–Ghana transform margin is bounded to the south by a prominent marginal ridge. ODP Leg 159 shipboard analyses on sediments from four sites document three distinct transform margin sedimentary and tectonic stages of evolution: (1)