The probability that the impactor just happened to have
the same isotopic signature as the Earth was vanishingly small.
The probability that the impactor just happened to have
the same isotopic signature as Earth was vanishingly small.
Not exact matches
But planetary bodies that formed in different parts of the solar system generally have different
isotopic compositions, so different that the
isotopic signatures serve as «fingerprints» for planets and meteorites from the
same body.
Yehoshua Kolodny at the Hebrew University in Jerusalem doubts whether the
isotopic make - up of the T. rex skeleton is the
same as it was when the animal was alive.
Referred to as the «lunar
isotopic crisis,» this was a problem for the main theory of lunar formation, because it's highly unlikely the isotopes would be exactly the
same for two random objects in the solar system.
The measurements show that 4 - Vesta contains the
same hydrogen
isotopic composition as carbonaceous chondrites, which is also that of Earth.
The UniChem connectivity search function allows users to find not only exact matches of their chemical structure across 60 million related molecules from 21 data sources worldwide, but also identifies «equivalent» structures that have the
same atom connectivity while differing in stereochemistry or
isotopic composition, or which exist in a different salt form.
Potassium - Argon Dating I Limitations of the If you read further in my second potassium - argon dating page: K - Ar - dating page 2 You will see that Ar dating method can overcome these limitations of conventional k - ar dating, and has the added advantage that potassium and argon are determined on the
same sample and that only measurements of the
isotopic ratios of argon are required.
Ar dating method can overcome these limitations of conventional k - ar dating, and has the added advantage that potassium and argon are determined on the
same sample and that only measurements of the
isotopic ratios of argon are required.
[Response: Unfortunately, you seem to have conveniently forgotten that Keigwin (and Pickart) published a paper in Science just a few years later in 1999 pointing that the appparent cooling (actually, the oxygen
isotopic signal in question isn't entirely temperature, it is salinity as well, so the quantative 1 deg cooling estimate you cite is not actually reliable) in the Sargasso Sea is diametrically opposed by a substantial warming at the
same time in the Laurentian Fan region of the North Atlantic off the coast of Newfoundland.
[Response: My recollection is that Zachos had the
same observation from ODP cores, that surface - dwelling forams were either isotopically heavy or light, never transitional, but bottom - dwellers could be found with transitional
isotopic composition.
Here's a more proper conclusion: Since the three
isotopics of Carbon (in CO2) follow almost exactly the
same laws, the response of any of them (or all of them together) to an injected excess in the atmosphere will be almost exactly the
same.
Note that ppm and delta13C are not the
same at all altitudes and evolve progressively, as illustrated by the airborne measurements of Nakazawa et al., Time and space variations of the carbon
isotopic ratio, Tellus, 1993.
The content of the air is made of two sets (CO2 anthropic from emissions)(t) and (CO2 natural)(t); the lifetime of the molecules is the
same for both sets and is known to be in the range 3 to 7 years; once a lifetime is assumed the (CO2 anthropic from emissions)(t) and its delta13C can be computed to get (CO2 natural)(t) and its
isotopic signature; this is done for several assumed lifetimes of CO2 molecules in the air.
This method gives the
same overall CO2 level as the cold crushing method, but more accurate
isotopic measurements.