Showing posts with label San Benito County. Show all posts
Showing posts with label San Benito County. Show all posts

Wednesday, 6 January 2016

Townsendiella ensifera: A new species of Cuckoo Bee from the Pinnacles National Park in California.

Cuckoo Bees, Nomadinae, are cleptoparasitic Bees which resemble Wasps in appearance, and to some extent behavior. The group get their name from their habit of laying their eggs inside the nests of other Bees, the larvae emerging withing the sealed cells of the host species, killing the host's larvae with specialized elongate mandibles, then proceeding to eat both the host larvae and the food provided for it by its mother (cleptoparasitism).

In a paper published in the journal ZooTaxa on 16 December 2015, Michael Orr of the Biology Department at Utah State University and Terry Griswold of the United States Department of Agriculture Agricultural Research Institute's Pollinating Insects Research Unit describe a new species of Cuckoo Bee from the Pinnacles National Park in San Benito County, California.

The new species if placed in the genus Townsendiella, which is indigenous to the southwest United States and northwest of Mexico, and is given the specific name ensifera, meaning 'sword-bearer', in reference to the shape of the mouthparts and cleptoparasitic lifestyle. These are black Bees with a covering of largely white fur, though this is brownish or even reddish in places. The fur of the males is whiter than that of the females.

Townsendiella ensifera, female specimen in lateral view. Scale bar is 0.25 mm. Orr & Griswold (2015).

The Bees were active from early May to late August on the flowers of California Buckwheat, Eriogonum fasciculatum, and Greasewood, Adenostoma fasciculatum. The host Bee for this species is unknown, though Orr and Greenwold note that Townsendiella ensifera is closely related to Townsendiella pulchra, which parasitzes Bees of the genus Hesperapis. Two species of Hesperapis are known to be present in the Pinnacles National Park, Hesperapis regularis, which is considerably larger than Townsendiella ensifera, and Hesperapis ilicifoliae which is approximately the same size, leading to the suggesting that this may be the host species for Townsendiella ensifera.

See also...

http://sciencythoughts.blogspot.co.uk/2014/07/nest-cells-of-leafcutter-bees-from.htmlNest cells of Leafcutter Bees from the Rancho La Brea Tar Pits.                       Leafcutter Bees (Megachilidae) cut their name from their habit of cutting disk-shaped segments from leaves, from which they build their nests. Each female...
http://sciencythoughts.blogspot.co.uk/2014/05/two-new-species-of-orchid-bee-from.htmlTwo new species of Orchid Bee from Columbia and Brazil.                                    The Orchid Bees (Euglossini) of Central and South America have an unusual relationship with the Orchids they pollenate, in that the Orchids do not produce a food substance with which to attract the Bees, but rather...
http://sciencythoughts.blogspot.co.uk/2014/05/a-new-species-of-leafcutter-bee-from.htmlA new species of Leafcutter Bee from Mexico.                                                   Leafcutter Bees (Megachilidae) get their name from their habit of cutting segments from leaves with which to line their nests. They are solitary Bees, each female Bee building her own nest in a wood cavity, plant...
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Monday, 28 October 2013

Magnitude 2.5 Earthquake in San Benito County, California.

The United States Geological Survey recorded a Magnitude 2.5 Earthquake at a depth of 7.5 km, in southern San Benito County, California, slightly before 7.00 am local time (slightly before 2.00 pm GMT) on Saturday 26 October 2013. This is not a large quake, and is unlikely to have caused any damage or injuries, though it was felt as far away as Los Gatos in Santa Clara County, 115 km to the northeast.

The approximate location of the 26 October 2013 San Benito County Earthquake. Google Maps.

California is extremely prone to Earthquakes due to the presence of the San Andreas Fault, a tectonic plate margin that effectively bisects the state. The west of California, including Santa Barbara and Los Angeles, is located on the Pacific Plate, and is moving to the northwest. The east of California, including Fresno and Bakersfield is on the North American Plate, and is moving to the southeast. The plates do not move smoothly past one-another, but constantly stick together then break apart as the pressure builds up. This has led to a network of smaller faults that criss-cross the state, so that Earthquakes can effectively occur anywhere.

Witness accounts of Earthquakes can help geologists to understand these events and the underlying structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) then you can report it to the United States Geological Survey here.


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Monday, 30 September 2013

Magnitude 2.5 Earthquake in northwest San Benito County, California.

The United States Geological Survey recorded a Magnitude 2.5 Earthquake at a depth of 5.5 km, 3 km southwest of San Juan Bautista in San Benito County, California, slightly before 2.05 pm local time (slightly before 9.05 pm GMT) on Saturday 28 September 2013. This is a small quake, highly unlikely to have caused any damage or casualties, though people did report feeling it in Santa Clara County to the north of the epicenter.

The approximate location of the 28 September 2013 San Juan Bautista Earthquake. Google Maps.

California is extremely prone to Earthquakes due to the presence of the San Andreas Fault, a tectonic plate margin that effectively bisects the state. The west of California, including Santa Barbara and Los Angeles, is located on the Pacific Plate, and is moving to the northwest. The east of California, including Fresno and Bakersfield is on the North American Plate, and is moving to the southeast. The plates do not move smoothly past one-another, but constantly stick together then break apart as the pressure builds up. This has led to a network of smaller faults that criss-cross the state, so that Earthquakes can effectively occur anywhere.

Witness accounts of Earthquakes can help geologists to understand these events and the underlying structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) then you can report it to the United States Geological Survey here.


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Friday, 27 September 2013

Magnitude 2.8 Earthquake in San Benito County, California.

The United Stated Geological Survey recorded a Magnitude 2.8 Earthquake at a depth of 8.2 km, 11 km to the southeast of Hollister in San Benito County, California, slightly after 0.55 am local time (slightly after 7.55 am GMT) on Thursday 26 September 2013. This is not a large quake, and is unlikely to have caused any damage or casualties, but is likely to have been felt locally.

The approximate location of the 26 September 2013 San Benito County Earthquake. Google Maps.

California is extremely prone to Earthquakes due to the presence of the San Andreas Fault, a tectonic plate margin that effectively bisects the state. The west of California, including Santa Barbara and Los Angeles, is located on the Pacific Plate, and is moving to the northwest. The east of California, including Fresno and Bakersfield is on the North American Plate, and is moving to the southeast. The plates do not move smoothly past one-another, but constantly stick together then break apart as the pressure builds up. This has led to a network of smaller faults that criss-cross the state, so that Earthquakes can effectively occur anywhere.

Witness accounts of Earthquakes can help geologists to understand these events and the underlying structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) then you can report it to the United States Geological Survey here.


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