Carotenoid diagenesis in recent marine sediments--I. The Peru continental shelf (15°S, 75°W) *

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

3

Scientific paper

We report here the distribution of carotenoids in Peru marine surface sediments, including partial identification of 37 pigments, 33 of which have not been previously reported to occur in marine sediments. Our analysis demonstrates that zooplanktonic crustacea, diatoms, dinoflagellates, cryptomonads, purple nonsulfur photosynthetic bacteria, and unidentified species of photosynthetic bacteria are contributors to sedimentary organic matter. Fucoxanthin, fucoxanthinol, diadinoxanthin, peridinin and peridininol, the principal carotenoids of diatoms and dinoflagellates observed in sediment traps, are nearly absent from our sample, even though these phytoplankton are the primary source of organic matter. We attribute this to the presence of 5,6 epoxides in these pigments, a feature which causes rapid cleavage of the polyene and fragmentation to low molecular weight compounds.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Carotenoid diagenesis in recent marine sediments--I. The Peru continental shelf (15°S, 75°W) * does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Carotenoid diagenesis in recent marine sediments--I. The Peru continental shelf (15°S, 75°W) *, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Carotenoid diagenesis in recent marine sediments--I. The Peru continental shelf (15°S, 75°W) * will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1348001

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.