You have isolated a decapeptide (a 10-residue peptide) called FP, which has anticancer activity. Determine the sequence of the peptide from the following information. (Note that amino acids are separated by commas when their sequence is not known.)

(a) One cycle of Edman degradation of intact FP yields 2 mol of PTH-aspartate per mole of FP.
(b) Treatment of a solution of FP with 2-mercaptoethanol followed by the addition of trypsin yields three peptides with the composition (Ala, Cys, Phe), (Arg, Asp), and (Asp, Cys, Gly, Met, Phe). The intact (Ala, Cys, Phe) peptide yields PTH-cysteine in the first cycle of Edman degradation.
(c) Treatment of 1 mol of FP with carboxypeptidase (which cleaves the C-terminal residue from peptides) yields 2 mol of phenylalanine.
(d) Treatment of the intact pentapeptide (Asp, Cys, Gly, Met, Phe) with CNBr yields two peptides with the composition (homoserine lactone, Asp) and (Cys, Gly, Phe). The (Cys, Gly, Phe) peptide yields PTH-glycine in the first cycle of Edman degradation.

Mantle convection  is the slow  creepingmotion of earth's solid silicate  mantle  caused by  convection  currents carrying  heat from the interior  to the planet's surface.[1][2]  the earth's surface  lithosphere, which rides atop the  asthenosphere  (the two components of the  upper mantle), is divided into a number of  plates  that are continuously being created and consumed at their opposite  plate boundaries. accretion occurs as mantle is added to the growing edges of a plate, associated with  seafloor spreading. this hot added material cools down by  conduction  and  convection  of heat. at the consumption edges of the plate, the material has thermally contracted to become dense, and it sinks under its own weight in the process of  subduction  usually at an  ocean trench.[3]this subducted material sinks through the earth's interior. some subducted material appears to reach the lower mantle,[4]  while in other regions, this material is impeded from sinking further, possibly due to a phase transition from  spinel  to  silicate perovskiteand  magnesiowustite, an  endothermic reaction.[5]the subducted oceanic crust triggers  volcanism, although the basic mechanisms are varied. volcanism may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.secondary forms of convection that may result in surface volcanism are postulated to occur as a consequence of intraplate extension[6]  and  mantle plumes.[7]it is because the mantle can convect that the  tectonic plates  are able to move around the earth's surface.[8]mantle convection seems to have been much more active during the  hadean  period, resulting in gravitational sorting of heavier molten  iron, and  nickel  elements and  sulphides  in the core, and lighter  silicate minerals  in the  mantle.