SignificanceThe use of heterologous systems to express spider silk has become an attractive method. However, achieving cost-effective production and high yields is still challenging. Here, we describe the establishment of a targeted gene replacement system in Bombyx mori to express the major ampullate spidroin-1 gene (MaSp1) from the spider Nephila clavipes. With the aid of transcription activator-like effector nuclease-mediated homology-directed repair, we genetically replaced the silkworm fibroin heavy chain gene with MaSp1 with considerable transformation efficiency, and the chimeric MaSp1 yields reached up to 35.2% wt/wt of cocoon shells in transformed silkworms. The genetically modified silk fiber had significant changes in mechanical properties, with improved extensibility. This system will shed light on the future mass production of new biomaterials, including spider silk.

Rheological, mechanical properties and shape memory properties of PDLLA could be greatly improved through solution blending with sc-PLA.

Newly discovered peloidal limestone from the summit of Mount Qomolangma (Mount Everest) contains skeletal fragments of trilobites, ostracods and crinoids. They are small pebble-sized debris interbedded in micritic bedded limestone of the Qomolangma Formation, and are interpreted to have been derived from a bank margin and redeposited in peri-platform environments. An exposure of the Qomolangma detachment at the base of the first step (8520 m), on the northern slope of Mount Qomolangma was also found. Non-metamorphosed, strongly fractured Ordovician limestone is separated from underlying metamorphosed Yellow Band by a sharp fault with a breccia zone. The 40 Ar-39 Ar ages of muscovite from the Yellow Band show two-phase metamorphic events of approximately 33.3 and 24.5 Ma. The older age represents the peak of a Barrovian-type Eo-Himalayan metamorphic event and the younger age records a decompressional high-temperature Neo-Himalayan metamorphic event. A muscovite whole-rock 87 Rb-86 Sr isochron of the Yellow Band yielded 40.06 ± 0.81 Ma, which suggests a Pre-Himalayan metamorphism, probably caused by tectonic stacking of the Tibetan Tethys sediments in the leading margin of the Indian subcontinent. Zircon and apatite grains, separated from the Yellow Band, gave pooled fission-track ages of 14.4 ± 0.9 and 14.4 ± 1.4 Ma, respectively. These new chronologic data indicate rapid cooling of the hanging wall of the Qomolangma detachment from approximately 350°C to 130°C during a short period .