Miss Barbara Finn and Mr. E.J. Stanistreet to Mr. Meredith (11 October 1962)

https://egrove.olemiss.edu/mercorr_pro/2131/thumbnail.jp

Mammal community structure analysis

Peer reviewe

Late Glacial and Holocene avulsions of the Rio Pastaza Megafan (Ecuador- Peru): frequency and controlling factors

International audienceThe geomorphological study by mean of remote sensing imagery of the Rio Pastaza Megafan (Ecuador and northern Peru), reveals the traces of numerous avulsions. 108 avulsion sites have been defined. The location of these sites, the available radiocarbon ages as well as historical maps of the 17th century, enable us to propose an evolution history of the migration and avulsions of the Rio Pastaza since the Last Glacial Maximum. The first avulsions of the Río Pastaza occurred after the LGM in a zone close to and roughly parallel to the sudandean front, where the developed avulsion gave a distributive pattern to the ancient stream of the Río Pastaza in an area located between the modern Río Morona and Pastaza, where they caused the Rio Pastaza to develop a fan-like distributary pattern. This is interpreted as a response to thrust related forelimb tilt, progressively shifting eastward the Rio Pastaza and the apex of the megafan. This sequence of events ended with the Great Diversion of the Rio Pastaza toward the modern Rios Corrientes and Tigre. Avulsions occurred in the Tigre-Corrientes Area between 9200 and 8500 yrsCal BP. Afterward, the Río Pastaza was diverted to its present-day north-south course. This last significant avulsion occurred before AD 1691. In the area located between the modern Río Morona and Pastaza, avulsion frequency - probably overestimated - ranges between 100 to 200yrs. In the Ríos Tigre and Corrientes area, avulsion frequency - probably underestimated - ranges from 300 to 400 yrs. Regional tectonics is likely to have triggered most of the avulsions in the Morona-Pastaza area but its influence is restricted to this area. The factors controlling the avulsions in the Tigre-Corrientes area are less clear because the frequently described "hydrologic"-driven avulsion as observed in areas characterized by contrasted hydrologic cycles are inconsistent with the characteristics of the hydrologic cycles of the Rio Pastaza

Signals from the deep: Spatial and temporal acoustic occurrence of beaked whales off western Ireland - Fig 4

<p><b>Mean Cuvier’s beaked whale detections per recording day bubble plot (right) and with standard error bars (left) for stations 1 (SE = ±0.70), 2 (SE = ±0.59), 3 (SE = ±2.61), 4 (SE = ±4.48), 5 (SE = ±1.08), 6 (SE = ±1.38), 7 (SE = ±1.35), and 8 (SE = ±1.26) off western Ireland from May to Dec 2015 (stations 1–4) and Mar to Nov 2016 (stations 3 and 5–8).</b> Results of Kruskall-Wallis tests are given and results from Tukey-Kramer multiple comparisons tests are represented by coloured means (left) with different colours denoting a statistically significant difference. *Station 8 differs from 7, but not from 3, 5, and 6.</p