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  • 1
    In: eBioMedicine, Elsevier BV, Vol. 87 ( 2023-01), p. 104402-
    Type of Medium: Online Resource
    ISSN: 2352-3964
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2023
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  • 2
    In: Journal of Animal Science, Oxford University Press (OUP), Vol. 99, No. 6 ( 2021-06-01)
    Abstract: One hundred and ninety nonlactating, pregnant beef cows (¾ Bos taurus and ¼ Bos indicus; 138 multiparous and 52 primiparous) were assigned to this experiment at 117 ± 2.2 d of gestation (day 0). Cows were ranked by parity, pregnancy type (artificial insemination = 102, natural service = 88), body weight (BW) and body condition score, and assigned to receive a supplement containing: (1) sulfate sources of Cu, Co, Mn, and Zn (INR; n = 95) or (2) an organic complexed source of Cu, Mn, Co, and Zn (AAC; Availa4; Zinpro Corporation, Eden Prairie, MN; n = 95). The INR and AAC provided the same daily amount of Cu, Co, Mn, and Zn, based on 7 g of the AAC source. From day 0 to calving, cows were maintained in a single pasture and segregated 3 times weekly into 1 of 24 individual feeding pens to receive treatments. Calves were weaned on day 367 (200 ± 2 d of age), managed as a single group for a 45-d preconditioning period (days 367 to 412), and transferred to a single oat (Avena sativa L.) pasture on day 412. Heifer calves were moved to an adjacent oat pasture on day 437, where they remained until day 620. Heifer puberty status was verified weekly (days 437 to 619) based on plasma progesterone concentrations. Steer calves were shipped to a commercial feedlot on day 493, where they were managed as a single group until slaughter (day 724). Plasma cortisol concentration was greater (P = 0.05) in AAC calves at weaning but tended to be less (P = 0.10) on day 370 compared with INR calves. Mean plasma haptoglobin concentration was greater (P = 0.03) in INR vs. AAC calves during preconditioning, and no treatment effects were noted (P = 0.76) for preconditioning average daily gain (ADG). Puberty attainment was hastened in AAC heifers during the experiment (treatment × day; P & lt; 0.01), despite similar (P = 0.39) ADG between treatments from days 412 to 620. Expression of myogenin mRNA in the longissimus muscle was greater (P = 0.05) in INR vs. AAC heifers on day 584. No treatment effects were detected (P ≥ 0.24) for steer ADG from day 412 until slaughter, nor for carcass quality traits. Hepatic mRNA expression of metallothionein 1A was greater (P = 0.02) in INR vs. AAC steers on day 586. In summary, supplementing Co, Cu, Zn, and Mn as organic complexed instead of sulfate sources to beef cows during the last 5 mo of gestation did not improve performance and physiological responses of the steer progeny until slaughter, but hastened puberty attainment in the female progeny reared as replacement heifers.
    Type of Medium: Online Resource
    ISSN: 0021-8812 , 1525-3163
    Language: English
    Publisher: Oxford University Press (OUP)
    Publication Date: 2021
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  • 3
    In: Horticulturae, MDPI AG, Vol. 8, No. 9 ( 2022-09-09), p. 831-
    Abstract: Potassium (K) fertilization is a crucial component of sweet potato (Ipomoea batatas L.) production. The basis for K fertilizer recommendations in sweet potato production varies greatly and relies on studies conducted in the late 1950s–1970s. Changes in agronomic practices and increasing costs emphasize the need to revisit fertilizer recommendations. A field experiment was conducted to investigate the impact of seven different K fertilizer (K2O) application rates on sweet potato storage root yield, tissue K concentration, and economic implications in Mississippi. Incremental applications of K fertilizer did not influence sweet potato yield at any grade. Leaf tissue K concentration exhibited a quadratic trend in response to K fertilizer rate, with maximum leaf and root K content achieved at 269 and 404 kg·ha−1 K2O, respectively. Both the predicted K application rate for maximum yield and maximum profitability were the same, at 174 kg·ha−1 K2O. Accordingly, comparable sweet potato yields were achieved while applying substantially less fertilizer than the recommended rate. Further research is warranted to examine the impacts of only potassium fertilizer applications on soil characteristics and temporal trends in sweet potato potassium uptake, as well as refine fertilization recommendations for sweet potato production.
    Type of Medium: Online Resource
    ISSN: 2311-7524
    Language: English
    Publisher: MDPI AG
    Publication Date: 2022
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  • 4
    In: Journal of Animal Science, Oxford University Press (OUP), Vol. 99, No. 5 ( 2021-05-01)
    Abstract: One hundred and ninety non-lactating, pregnant beef cows (three-fourth Bos taurus and one-fourth Bos indicus; 138 multiparous and 52 primiparous) were assigned to this experiment at 117 ± 2.2 d of gestation (day 0). Cows were ranked by parity, pregnancy type (artificial insemination = 102 and natural service = 88), body weight (BW), and body condition score (BCS) and assigned to receive a supplement containing: 1) sulfate sources of Cu, Co, Mn, and Zn (INR; n = 95) or 2) an organic-complexed source of Cu, Mn, Co, and Zn (AAC; Availa 4; Zinpro Corporation, Eden Prairie, MN; n = 95). The INR and AAC provided the same daily amount of Cu, Co, Mn, and Zn, based on 7 g of the AAC source. From day 0 to calving, cows were maintained in a single pasture and were segregated three times weekly into 1 of the 24 individual feeding pens to receive treatments. Cow BW and BCS were recorded on days −30, 97, upon calving, and at weaning (day 367). Milk production was estimated at 42 ± 0.5 d postpartum via weigh–suckle–weigh (WSW) method. Liver biopsies were performed in 30 cows per treatment on days −30, 97, upon calving, and the day after WSW. Calf BW was recorded at birth and weaning. Liver and longissimus muscle (LM) biopsies were performed in 30 calves per treatment upon calving and 24 h later, the day after WSW, and at weaning. No treatment effects were detected (P ≥ 0.49) for cow BCS during gestation, despite AAC cows having greater (P = 0.04) BW on day 97. Liver Co concentrations were greater (P & lt; 0.01) for AAC compared with INR cows, and liver concentrations of Cu were greater (P = 0.02) for INR compared with AAC cows on day 97. Upon calving, INR cows had greater (P ≤ 0.01) liver Cu and Zn concentrations compared with AAC cows. No other treatment differences were noted (P ≥ 0.17) for cow and calf liver trace mineral concentrations. Cows receiving AAC had greater (P = 0.04) hepatic mRNA expression of metallothionein 1A at calving, and their calves had greater (P = 0.04) hepatic mRNA expression of superoxide dismutase at weaning. Milk production did not differ between AAC and INR cows (P = 0.70). No treatment effects were detected (P ≥ 0.29) for mRNA expression of LM genes associated with adipogenic or muscle development activities in calves at birth and weaning. Calf birth and weaning BW also did not differ (P ≥ 0.19) between treatments. In summary, supplementing AAC or INR to beef cows during the last 5 mo of gestation yielded similar cow–calf productive responses until weaning.
    Type of Medium: Online Resource
    ISSN: 0021-8812 , 1525-3163
    Language: English
    Publisher: Oxford University Press (OUP)
    Publication Date: 2021
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    SSG: 12
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  • 5
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 79, No. 23 ( 1998-06-09), p. 269-275
    Abstract: Except for the recent rumblings of a few moderate earthquakes and the eruption of Mt. St. Helen's, all has been relatively quiet on the Pacific Northwestern front. The Cascades region in the Pacific Northwest, a sporadically active earthquake and volcanic zone, still has great seismic potential [ Atwater , 1987], as comparisons with other subduction zones around the world have shown [ Heaton and Kanamori , 1984]. Recent tsunami propagation models [ Satake , 1996] and tree ring studies suggest that the last great Cascadia earthquake occurred in the winter of 1700 A.D. and had a magnitude of −8.9. The North Cascades or Wenatchee earthquake followed in 1872. With an estimated magnitude greater than 7, it was the largest earthquake in the written history of Washington and Oregon.
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1998
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    detail.hit.zdb_id: 2118760-5
    detail.hit.zdb_id: 240154-X
    SSG: 16,13
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  • 6
    Online Resource
    Online Resource
    Geological Society of America ; 1998
    In:  Geological Society of America Bulletin Vol. 110, No. 9 ( 1998-9), p. 1123-1148
    In: Geological Society of America Bulletin, Geological Society of America, Vol. 110, No. 9 ( 1998-9), p. 1123-1148
    Type of Medium: Online Resource
    ISSN: 0016-7606
    Language: Unknown
    Publisher: Geological Society of America
    Publication Date: 1998
    detail.hit.zdb_id: 2028776-8
    detail.hit.zdb_id: 2008165-0
    detail.hit.zdb_id: 449720-X
    detail.hit.zdb_id: 1351-1
    SSG: 13
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  • 7
    In: Geology, Geological Society of America, Vol. 32, No. 1 ( 2004), p. 9-
    Type of Medium: Online Resource
    ISSN: 0091-7613
    Language: English
    Publisher: Geological Society of America
    Publication Date: 2004
    detail.hit.zdb_id: 184929-3
    detail.hit.zdb_id: 2041152-2
    SSG: 13
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  • 8
    In: Geology, Geological Society of America, Vol. 43, No. 8 ( 2015-08), p. 675-678
    Type of Medium: Online Resource
    ISSN: 0091-7613 , 1943-2682
    Language: English
    Publisher: Geological Society of America
    Publication Date: 2015
    detail.hit.zdb_id: 184929-3
    detail.hit.zdb_id: 2041152-2
    SSG: 13
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1995
    In:  Tectonics Vol. 14, No. 1 ( 1995-02), p. 1-18
    In: Tectonics, American Geophysical Union (AGU), Vol. 14, No. 1 ( 1995-02), p. 1-18
    Abstract: The accretionary margin of the Hikurangi forearc on the southeast coast of the North Island of New Zealand is part of the leading edge of the Australian plate, which is overriding the obliquely converging Pacific plate. We investigate the last 10 m.y. of deformation history of the innermost (western) quarter of the total width of the forearc through analysis of the sedimentologic and structural evolution of the Eketahuna area on the east coast of the North Island. The Eketahuna area is ideal for such a study because emergence of the margin in the Quaternary has exposed a complete late Neogene rock record. This record has allowed us to chronicle the strain history. From 10 Ma to about 2.5 Ma this forearc region was the locus of subsidence and marine deposition. In the latest Pliocene this part of the margin began to shorten through folding and reverse faulting, bringing an end to basin filling. The period of shortening was brief, and by the late Pleistocene, reverse faulting had ceased and was immediately succeeded by dextral strike‐slip faulting, in some cases along the same faults. Presently, the dominant strain regime in the inner quarter of the forearc is strike‐slip faulting. This structural history illustrates that, over time, the pattern of strain partitioning has changed in the Hikurangi forearc. The switch from crustal shortening to dextral shear along the major faults in this area in the last 1 m.y. may be a response to more than 10° of clockwise rotation in the southern Hikurangi forearc in Pliocene and Pleistocene time. This rotation is a consequence of the fact that the accretionary margin is undergoing continuous deformation between the obliquely converging Australian and Pacific plates in this area at the southernmost end of the Kermadec‐Hikurangi subduction system. The inboard portion of this young accretionary margin is exceptionally well exposed today, probably in part because of the late Neogene subduction of relatively thick, buoyant crust of the Hikurangi‐Chatham plateau.
    Type of Medium: Online Resource
    ISSN: 0278-7407 , 1944-9194
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1995
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    detail.hit.zdb_id: 780264-X
    SSG: 16,13
    SSG: 13
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  • 10
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Tectonics Vol. 9, No. 1 ( 1990-02), p. 23-44
    In: Tectonics, American Geophysical Union (AGU), Vol. 9, No. 1 ( 1990-02), p. 23-44
    Abstract: The Maraetotara Plateau‐Cape Kidnappers area in southern Hawke's Bay, New Zealand, lies in the forearc region of the obliquely convergent Hikurangi margin, where the Pacific Plate is presently subducting beneath the leading edge of the Australian Plate. Uplift accompanied by extensional faulting has been the dominant style of deformation in this area since mid‐Pleistocene time. Principal strain directions and strain ratios, determined from mesoscale fault arrays associated with major faults, document the regional extension. In the Cape Kidnappers area, fault arrays record plane strain with northwest horizontal extension and vertical shortening. In the Maraetotara Plateau area, fault arrays record triaxial strain with roughly equal magnitudes of horizontal extension in two principal strain directions, either east‐west and north‐south, or northwest and northeast, and vertical shortening. The morphology, seismicity, and nature and distribution of active faults of the southern Hawke's Bay region suggest that the Maraetotara Plateau‐Cape Kidnappers area is the on‐land expression of an outer‐arc high, which is developed between the accretionary wedge on the east and the forearc basin on the west. The cause of uplift and extension in the Maraetotara Plateau‐Cape Kidnappers area may be either upper plate deformation related to structural evolution of the outer‐arc high and underlying backstop, underplating on the Hikurangi subduction zone, or a combination of these processes. The uplift and horizontal extension occurring in the Maraetotara Plateau‐Cape Kidnappers area contrast sharply with active deformation in adjacent parts of the forearc, reflecting a distinct partitioning of strain in this part of the obliquely convergent plate boundary.
    Type of Medium: Online Resource
    ISSN: 0278-7407 , 1944-9194
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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    detail.hit.zdb_id: 780264-X
    SSG: 16,13
    SSG: 13
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