Biology, 03.02.2020 01:48, marqueen1

Select all that apply.

which characteristics are not necessarily true of all living things?

movement
heredity
reproduction
homeostasis
sensitivity
metabolism
cells

Answers: 2

Show answers

Answers

answered: u8p4

Sensitivity
movement
heredity
hope it help have a wonderful day/night

answered: jos1319

The correct answer will be options-

1. Movement

2. Reproduction

Explanation:

Biologists have tried to distinguish the living thing from the non-living thing on the basis of eight characteristics that are unique to the living world.

Out of these eight characters, there are few characters which are not necessarily present or shown by the living organisms like movement and reproduction. Take the case of plants which do not show movement but still considered a living thing and the sterile organisms which cannot reproduce or produce offsprings.

Thus, movement and reproduction are the correct answer.

answered: Guest

relative humidity, temperature and dew point -- are bound together in the mathematical relationship below. relative humidity changes when temperatures change. because warm air can hold more water vapor than cool air, relative humidity falls when the temperature rises if no moisture is added to the air. so i would say a

Hello everyone extra easy question for large amount of ! meh

answered: Guest

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.