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| 001 | 655439 | ||
| 005 | 20231030041344.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\21562 | ||
| 035 | _aRU\TPU\network\21557 | ||
| 090 | _a655439 | ||
| 100 | _a20170904a2005 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 102 | _aUS | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aThe East Siberian Sea as a transition zone between pacific-derived waters and Arctic shelf waters _fI. P. Semiletov [et al.] |
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| 203 |
_aText _celectronic |
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| 300 | _aTitle screen | ||
| 320 | _a[References: 18 tit.] | ||
| 330 | _aIn the present study we report hydrological (T and S) and hydrochemical data obtained during a Russian Trans-Arctic cruise in 2000 onboard the Hydrographic Vessel (HV) Nikolay Kolomeytsev, and describe the top layer of the sediment (a typical sample was taken from the upper 0-5 cm layer of bottom sediment) and the distribution of the organic carbon (δ13Corg) and nitrogen (δ15Norg) isotope ratios. Using both historical water data and data from our cruise, we divide the ESS into two specific areas: the Western area, influenced strongly by Lena River input, and the Eastern area, under direct influence of Pacific-derived water. We also used the stable δ13Corg and δ15Norg isotopes to detect the sediment geochemical boundary (or “geochemical FZ”) between Pacific “marine-derived sediments” and “terrestrial derived sediments” which can be considered to reflect the long-term (on a scale of 102 years) position of the most westward extension of Pacific water. These are among the first reliable hydrological and geochemical data reported for the ESS from the Dmitry Laptev Strait to the Long Strait, and they reveal novel insights about interaction between Pacific water and local shelf water. | ||
| 333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
| 461 | _tGeophysical Research Letters | ||
| 463 |
_tVol. 32, iss. 10 _v[P. L10614/1-L10614/5] _d2005 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aводные массы | |
| 610 | 1 | _aраспространение | |
| 610 | 1 | _aфронтальные зоны | |
| 610 | 1 | _aСеверный Ледовитый океан | |
| 701 | 1 |
_aSemiletov _bI. P. _cgeographer _cProfessor of Tomsk Polytechnic University, doctor of geographical Sciences _f1955- _gIgor Petrovich _2stltpush _3(RuTPU)RU\TPU\pers\34220 |
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| 701 | 1 |
_aDudarev _bO. V. _cgeologist _cresearcher of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences _f1955- _gOleg Viktorovich _2stltpush _3(RuTPU)RU\TPU\pers\35379 |
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| 701 | 1 |
_aLuchin _bV. |
|
| 701 | 1 |
_aCharkin _bA. N. _cgeologist _cengineer-researcher of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences _f1980- _gAleksandr Nikolaevich _2stltpush _3(RuTPU)RU\TPU\pers\35441 |
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| 701 | 1 | _aShin Kyung-Hoon | |
| 701 | 1 | _aTanaka Nori | |
| 801 | 2 |
_aRU _b63413507 _c20180220 _gRCR |
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| 856 | 4 | _uhttp://dx.doi.org/10.1029/2005GL022490 | |
| 942 | _cCF | ||