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Showing posts with label ALASKA. Show all posts
Showing posts with label ALASKA. Show all posts

Friday, 8 July 2016

solation and Total Synthesis of Stolonines A–C, Unique Taurine Amides from the Australian Marine Tunicate Cnemidocarpa stolonifera

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Figure 1. Structures of stolonines A-C (13), 11-hydroxyascididemin (4) and cnemidine A (5) isolated from the tunicate C. stolonifera.
Marinedrugs 13 04556 g001 1024

Table 1. NMR data for 1 in DMSO-d6 a.
PositionδCδH (J in Hz)gCOSYgHMBCAD
112.20, br.s2
2138.58.82, d (3.0)13, 3a, 7a
3112.1
3a126.2
4121.38.22, dd (1.8, 7.2)56, 7a
5122.47.24, dt (1.8, 7.2)4, 63a, 7
6123.37.26, dt (1.8, 7.2)5, 74, 7a
7112.57.52, dd (1.8, 7.2)63a, 5
7a136.2
8181.6
9162.7
108.78, t (5.4)119
1135.53.50, dd (6.0, 6.6)10, 129, 12
1249.82.66, t (6.6)1111
a 1H NMR at 600 MHz referenced to residual DMSO solvent (δH 2.50 ppm) and 13C NMR at 150 MHz referenced to residual DMSO solvent (δC 39.52 ppm).

Stolonine A (1) was obtained as a white amorphous solid. The (−)-HRESIMS spectrum displayed a molecular ion [M−H]at m/z 295.0390, which was consistent with the molecular formula C12H12N2O5S. The IR spectrum indicated the presence of an S=O stretching band at 1205 cm−1 [16]. A 1H NMR spectrum of 1 showed two exchangeable protons (δH 12.20 and 8.78 ppm), five aromatic protons (δH 8.82, 8.22, 7.52, 7.26 and 7.24 ppm) and two methylenes (δH 3.50 and 2.66 ppm). Further analysis of the 13C NMR and gHSQCAD spectra indicated that the molecule contained two carbonyls (δC 181.6 and 162.7 ppm), eight aromatic carbons (δC 138.5, 136.2, 126.2, 123.3, 122.4, 121.3, 112.5 and 112.1 ppm) and two methylenes (δC 49.8 and 35.5 ppm) (Table 1). J coupling constants of aromatic protons H-4 (δH 8.22, dd, 1.8, 7.2 Hz), H-5 (δH 7.24, dt, 1.8, 7.2 Hz), H-6 (δH 7.26, dt, 1.8, 7.2 Hz) and H-7 (δH 7.52, dd, 1.8, 7.2 Hz) and their COSY correlations were characteristic of a 1,2-disubstituted benzene ring (aFigure 2). A gCOSY spectrum displayed correlations from the exchangeable proton H-1 (δH12.20, br.s) to H-2 (δH 8.82, d, 3.0 Hz) and also from H-11 (δH 3.50, dd, 6.0, 6.6 Hz) to the triplet exchangeable proton H-10 (δH 8.78, t, 5.4 Hz) and H-12 (δH 2.66, t, 6.6 Hz) facilitating the establishment of two other spin systems, –NH–CH= (b,Figure 2) and –NH–CH2–CH2– (cFigure 2) respectively. The aromatic carbon C-3 (δC 112.1 ppm) was attached to C-2 (δC138.5 ppm) in the moiety b determined by a HMBC correlation from H-2 to C-3. A HMBC correlation from H-2 to C-7a (δC136.2 ppm) supported the linkage from a to b at C-7a (Figure 2). Both protons H-10 and H-11 in the moiety c showed HMBC correlations with a carbonyl carbon at δC 162.7 ppm suggesting the connection of this carbonyl to N-10 to form an amide bond (cFigure 2). Two methylene signals at δH 3.50 and 2.66 ppm corresponding to carbons C-11 (δC 35.5 ppm) and C-12 (δC 49.8 ppm) as well as the relatively downfield resonance of the methylene C-12 were diagnostic of methylenes in a taurine moiety (cFigure 2) [17,18,19].
Table 1. NMR data for 1 in DMSO-d6 a.
Figure 2. Partial structures (ab and c) of 1 and their key HMBC correlations.
Figure 2. Partial structures (ab and c) of 1 and their key HMBC correlations.
Marinedrugs 13 04556 g002 1024

No HMBC correlation from any proton to the carbonyl C-8 (δC 181.6 ppm) was observed when HMBC experiments were performed and optimized with different JHC couplings. Therefore, two different isomers 1-I and 1-II were conceivable from these data (Figure 3). Detailed HMBC analysis showed that H-2 had a HMBC correlation with C-3a (δC 126.2 ppm). This suggested that 1 was favorable to 1-I since the H-2 to C-3a correlation in 1-I was a three-bond coupling while the H-2 to C-3a correlation in 1-II was a four-bond coupling (Figure 3).
Figure 3. Two possible structures 1-I and 1-II of 1 (1-I and 1-II are possible structural isomers of 1).

Figure 3. Two possible structures 1-I and 1-II of 1 (1-I and 1-II are possible structural isomers of 1).
Marinedrugs 13 04556 g003 1024


Table 2. Comparison of experimental and calculated 13C and 1H chemical shifts for 1 in DMSO-d6.
PositionδC (Exp.)1-I1-IIδH (Exp.)1-I1-II
δC (Calc.)δC (Scaled)δC (Calc.)δC (Scaled)δH (Calc.)δH (Scaled)δH (Calc.)δH (Scaled)
2138.5136.9140.3141.3142.88.828.748.618.848.67
3112.1111.5112.9111.2110.2
3a126.2124.1126.5123.0122.9
4121.3118.9120.9124.3124.48.228.628.488.408.19
5122.4120.1122.1121.1120.97.247.637.407.637.35
6123.3120.9123.0129.4129.97.267.597.368.007.76
7112.5108.7109.9114.8114.17.527.557.317.537.24
7a136.2131.9134.9134.4135.3
8181.6176.7183.2172.5176.5
9162.7156.8161.7159.4162.4
1135.537.132.636.929.83.503.693.113.713.08
1249.857.254.458.453.12.663.552.953.572.93
CMAE1.53.10.230.25
DP4100.0%0.0%85.3%14.7%

Stolonine A (1): white, amorphous solid; UV (MeOH) λmax (log ε) 210 (3.8), 252 (3.5) and 325 (3.3) nm; IR (film) νmax 3307, 1681, 1205, 1049 and 802 cm−11H (600 MHz, DMSO-d6) and 13C (150 MHz, DMSO-d6) NMR data are summarized in Table 1; (−)-HRESIMS m/z 295.0390 [M − H] (calcd for [C12H11N2O5S], 295.0394, Δ −1.4 ppm).


Mar. Drugs 201513(7), 4556-4575; doi:10.3390/md13074556
Article
Isolation and Total Synthesis of Stolonines A–C, Unique Taurine Amides from the Australian Marine Tunicate Cnemidocarpa stolonifera
Trong D. Tran 1, Ngoc B. Pham 1, Merrick Ekins 2, John N. A. Hooper 1,2 and Ronald J. Quinn 1,*
1
Eskitis Institute for Drug Discovery, Griffith University, Brisbane, Queensland 4111, Australia
2
Queensland Museum, Brisbane, Queensland 4101, Australia
*
Author to whom correspondence should be addressed; Tel.: +61-7-3735-6009; Fax: +61-7-3735-6001.

http://www.mdpi.com/1660-3397/13/7/4556/htm
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RAIN FOREST, KODIAK ISLAND, ALASKA, USA
 

HI EVERYONE - YESTERDAY, WE WERE IN THE ROCKY MOUNTAINS.
TODAY, WE ARE GOING TO KODIAK ISLAND IN ALASKA
TO CHECK OUT A RAINFOREST.
IN ORDER TO BE CONSIDERED A RAINFOREST,
IT HAS TO RECEIVE BETWEEN 98 AND 180 INCHES OF
PERCIPITATION, INCLUDING SNOW. ALASKA'S RAINFOREST SANCTUARY IS A
TEMPERATE RAINFOREST, AS OPPOSED TO A TROPICAL RAINFOREST.
KODIAK ISLAND HAS FOUR SEASONS. SPRING HAS A
LOT OF RAIN, CAUSING TREES AND PLANTS TO BLOOM.
SUMMER HAS WARM TEMPERATURES OF 70 - 80 DEGREES FARENHEIT.
AUTUMN HAS COOL TEMPERATURES AND RAIN. WINTER HAS
VERY COLD TEMPERATURES AND SNOW. THE AVERAGE
ANNUAL TEMPERATURE IS 50 DEGREES F.
KODIAK ISLAND'S RAINFOREST RESERVE IS 40 ACRES AND
INCLUDES TALL STANDS OF SPRUCE, HEMLOCK AND
CEDAR TREES WITH A FOREST FLOOR SATURATED WITH MOSSES,
WILD FLOWERS AND A VARIETY OF BERRIES.
THE SANCTUARY IS LOCATED AT PISCURESQUE HERRING COVE.
ON-SITE EXPERIENCES INCLUDE INTERACTING WITH A
HERD OF ALASKAN REINDEER, VISITING THE ALASKA WILDLIFE
FOUNDATION CENTER, WATCHING A NATIVE MASTER TOTEM-POLE
CARVER AT WORK AND VISITING A HISTORIC ALASKAN SAWMILL.
THE ALASKA RAINFOREST SANCTUARY IS A UNIQUE ALASKA
EXPERIENCE AND PERFECT FOR THE NATURE LOVER.
EAGLE CREEK, ONE OF ALASKA'S RICHEST SALMON SPAWNING STREAMS,
FLOWS THROUGH THIS DIVERSE ECOSYSTEM, INTO THE OCEAN.
A MAJOR FISH HATCHERY IS LOCATED ACROSS
THE CREEK FROM THE SANCTUARY BOARDWALK.
I HOPE YOU HAVE ENJOYED YOUR VIST TO
KODIAK ISLAND, ALASKA TO SEE THE RAINFOREST.

RAINFOREST VEGETATION

BROWN BEAR

KODIAK BEAR FAMILY

LORIKEET BIRDS IN RAINFOREST - HARLEQUIN DUCK
 
BLUE GROUSE - CLARK'S NUTCRACKER

KODIAK ISLAND HAS LOTS OF BALD EAGLES

SWORD FERN - WILD STRAWBERRIES


Map of Kodiak Island
Kodiak Island
Island in Alaska
Kodiak Island is a large island on the south coast of the U.S. state of Alaska, separated from the Alaska mainland by the Shelikof Strait. Wikipedia














 
 Kodiak Municipal Airport, Kodiak Island, Alaska


 

 

 
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Taurine

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2-aminoethanesulfonic acid


C2 H7 N O3 S

TAURINE




Picture#1.png

This is an H-NMR of Taurine depicting all peaks.

picture_clipping_1.png
This is a magnified view of the H-NMR of Taurine. This is a set of two triplet of peaks at 3.38 to 3.42 ppm which corresponds to the “Ha” protons attached to the carbon at the “1” position and at 3.23 to 3.28 ppm which corresponds to the “Hb” protons attached to the carbon at the “2” position. These peaks correspond to the sp3 hybridized hydrogen atoms bonded to the first and second carbon in the compound. There is splitting of the signal in the form of three peaks as the hydrogens are affected by two equavalent adjacent protons present bonded to the first and second carbon; from the N+1 rule, N would then equal 2 for each proton, so N+1, (2+1 = 3), 3 peaks would be observed. The three peaks corresponding to “Ha” deshielded by the electron-withdrawing group SO3H, as well causing a chemical shift to the left. This is so because normally without deshielding an sp3 hydrogen attached to a carbon is around 1.4 ppm. For “Hb” is deshielded by an amine group, which is less electronegative, and therefore less electron withdrawing than the effect seen on “Ha” so it is moved to the left less. The triplet peaks exhibit similar heights because the height of peaks corresponds to the ratio of protons between carbons; since both carbons have two H’s, the ratio is 1:1, so their heights are similar.


1D 13C, 7.4 spectrum for Taurine

PicutureCNMR.png
This is the C-NMR spectra of Taurine depicting all peaks.

PictureCNMR#2.png
This is a magnified view of the C-NMR of Taurine. It depicts a single peak from 50.1-50.23ppm and corresponding to the first carbon bonded to both the sulfur as well as the second carbon. The reason why the C-NMR would correspond to 50.1-50.23 is because the H-NMR corresponding to the protons attached to Carbon #1 is around 3.4 ppm. Since C-NMR peaks represent 15-20 times the amount of ppm of the protons attached to it, 3.4 x 15 is approximately 51 ppm. (See above explanation for H-NMR peak at 3.4 ppm)

PictureCNMR#3.png

This is a magnified view of the C-NMR of Taurine. There is a single peak at approximately 38.20 ppm, which corresponds to the second carbon bonded to the nitrogen group. The reason why the C-NMR would correspond to 38.2 is because the H-NMR corresponding to the protons attached to Carbon #2 is around 3.2 ppm. Since C-NMR peaks represent approximately 15-20 times the amount of ppm of the protons attached to it, 3.2 x 15 is approximately 48 ppm. (See above explanation for H-NMR peak at 3.2 ppm). Although the peak doesn’t exactly match with the H-NMR prediction, it can be deduced that this C-NMR peak correlates with Carbon #2 because it is the lesser ppm of the two C-NMR peaks.

2D [1H,1H]-TOCSY


2D [1H,1H]-TOCSY, 7.4 spectrum for Taurine

1D DEPT90

1D DEPT90, 7.4 spectrum for Taurine

1D DEPT135

1D DEPT135, 7.4 spectrum for Taurine

2D [1H,13C]-HSQC

2D [1H,13C]-HSQC, 7.4 spectrum for Taurine




2D [1H,13C]-HMBC



2D [1H,13C]-HMBC, 7.4 spectrum for Taurine

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MT. MC KINLEY, DENALI, ALASKA, USA

Map of Denali
Denali
Mountain in Alaska
Denali /dᵻˈnɑːli/ is the highest mountain peak in North America, with a summit elevation of 20,310 feet above sea level. At some 18,000 ft, the base-to-peak rise is the largest of any mountain situated entirely above sea level. Wikipedia

HI EVERYONE. YESTERDAY, WE WERE AT THE GATEWAY ARCH IN
ST. LOUIS, MISSOURI. TODAY WE ARE TAKING A BIG TRIP,
BACK TO ALASKA. I KNOW WE WERE THERE BEFORE BUT
THERE IS MORE TO SEE THERE. THIS TRIP IS GOING
TO TAKE IN ALL KINDS OF SIGHTS.
WE ARE GOING TO START OUT IN A BOAT ON
LAKE WONDER. AS WE TRAVEL ON THE BOAT, WE WILL
SEE ALDER AND WILLOW CARPETED HILLS ALONG WITH SOME SMALLER
PONDS. KEEP YOUR EYES OPEN CAUSE THERE IS A LOT OF
WATERFOWL AND OTHER WILDLIFE AROUND.
SOMETHING THAT WON'T BE HARD TO SEE IS THE STUNNING
VIEW OF MOUNT MCKINLEY AND THE ALASKA RANGE. MT. MCKINLEY
IS THE HIGHEST MOUNTAIN PEAK IN NORTH AMERICA, WITH A
SUMMIT ELEVATION OF 20,320 FEET ABOUT SEA LEVEL. YOU WILL
SEE SNOW ON THE MOUNTAIN TOP AT ANY TIME OF
THE YEAR. THERE ARE FIVE LARGE GLACIERS THAT FLOW OFF
THE SLOPES OF THE MOUNTAIN. LAKE WONDER THAT WE ARE
TRAVELING ON WAS CREATED BY RETREATING GLACIERS. IF ANYONE
IS ENERGENIC, YOU CAN HIKE THE MOUNTAIN.
I HOPE YOU ENJOYED YOUR RIDE ON THE BOAT WITH
THE SPECTACULAR VIEWS OF THE MOUNTAINS AND WILDLIFE...


 

 

 

 

 

 

 
 

 
 
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