scholarly journals Nesting ecology of East Pacific green turtles at Playa Cabuyal, Gulf of Papagayo, Costa Rica

2014 ◽  
Vol 36 (3) ◽  
pp. 506-516 ◽  
Author(s):  
Pilar Santidrián Tomillo ◽  
Spencer A. Roberts ◽  
Ricardo Hernández ◽  
James R. Spotila ◽  
Frank V. Paladino
2018 ◽  
Vol 17 (2) ◽  
pp. 169
Author(s):  
Luis G. Fonseca ◽  
Pilar Santidrián Tomillo ◽  
Wilbert N. Villachica ◽  
Wagner M. Quirós ◽  
Marta Pesquero ◽  
...  

2006 ◽  
Vol 37 (4) ◽  
pp. 549-552 ◽  
Author(s):  
Mario Santoro ◽  
Giovanna Hernández ◽  
Magaly Caballero ◽  
Fernando García

2009 ◽  
Vol 46 (2) ◽  
pp. 97-99 ◽  
Author(s):  
M. Santoro ◽  
P. Brandmayr ◽  
E. Greiner ◽  
J. Morales ◽  
B. Rodríguez-Ortíz

AbstractCharaxicephaloides polyorchis Groschaft and Tenora, 1978 is redescribed on the basis of specimens collected from the stomach of green turtles Chelonia mydas in Costa Rica. Our specimens are consistent with the original description which was based on four flukes from the same host species from the northwest coast of Cuba. Our redescription provides a new range of variations and adds new information on this species. This represents only the second record of C. polyorchis in green turtles.


2008 ◽  
Vol 21 (17) ◽  
pp. 4149-4167 ◽  
Author(s):  
Eric D. Maloney ◽  
Dudley B. Chelton ◽  
Steven K. Esbensen

Abstract Boreal summer intraseasonal (30–90-day time scale) sea surface temperature (SST) variability in the east Pacific warm pool is examined using Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) sea surface temperatures during 1998–2005. Intraseasonal SST variance maximizes at two locations in the warm pool: in the vicinity of 9°N, 92°W near the Costa Rica Dome and near the northern edge of the warm pool in the vicinity of 19°N, 108°W. Both locations exhibit a significant spectral peak at 50–60-day periods, time scales characteristic of the Madden–Julian oscillation (MJO). Complex empirical orthogonal function (CEOF) and spectra coherence analyses are used to show that boreal summer intraseasonal SST anomalies are coherent with precipitation anomalies across the east Pacific warm pool. Spatial variations of phase are modest across the warm pool, although evidence exists for the northward progression of intraseasonal SST and precipitation anomalies. Intraseasonal SSTs at the north edge of the warm pool lag those in the vicinity of the Costa Rica Dome by about 1 week. The MJO explains 30%–40% of the variance of intraseasonal SST anomalies in the east Pacific warm pool during boreal summer. Peak-to-peak SST variations of 0.8°–1.0°C occur during MJO events. SST is approximately in quadrature with MJO precipitation, with suppressed (enhanced) MJO precipitation anomalies leading positive (negative) SST anomalies by 7–10 days. Consistent with the CEOF and coherence analyses, MJO-related SST and precipitation anomalies near the Costa Rica Dome lead those at the northern edge of the warm pool by about 1 week.


2018 ◽  
Vol 146 ◽  
pp. 23-31 ◽  
Author(s):  
R. Majewska ◽  
M. De Stefano ◽  
B. Van de Vijver

2011 ◽  
Vol 76 (4) ◽  
pp. 841-846 ◽  
Author(s):  
Gabriela S. Blanco ◽  
Stephen J. Morreale ◽  
Elizabeth Vélez ◽  
Rotney Piedra ◽  
Wilder M. Montes ◽  
...  

Copeia ◽  
2002 ◽  
Vol 2002 (3) ◽  
pp. 653-664 ◽  
Author(s):  
Richard D. Reina ◽  
Philippe A. Mayor ◽  
James R. Spotila ◽  
Rotney Piedra ◽  
Frank V. Paladino

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