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Primary production export flux in Marguerite Bay (western Antarctic Peninsula shelf): linking upper water-column production to sediment trap derived flux 玛格丽特湾(南极半岛西部陆架)初级生产输出通量:将上层水柱生产与沉积物圈闭衍生通量联系起来
Pub Date : 2013-05-01 DOI: 10.1016/J.DSR.2013.02.001
K. Weston, T. Jickells, D. Carson, A. Clarke, M. Meredith, M. Brandon, M. I. Wallace, S. Ussher, K. Hendry
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引用次数: 27
Estimating turbulent dissipation rates from acoustic backscatter 从声波后向散射估计湍流耗散率
Pub Date : 2005-12-01 DOI: 10.1016/J.DSR.2005.07.002
T. Ross, R. Lueck
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引用次数: 18
Simple models of steady deep maxima in chlorophyll and biomass 叶绿素和生物量稳定深层最大值的简单模型
Pub Date : 2004-08-01 DOI: 10.1016/J.DSR.2004.02.009
B. A. Hodges, D. Rudnick
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引用次数: 62
A benthic carbon budget for the Continental Slope off Cape Hatteras, NC 北卡罗来纳州哈特拉斯角大陆斜坡底栖生物的碳收支
Pub Date : 1999-01-31 DOI: 10.2172/765626
N. Blair
The continental slope off Cape Hatteras, N.C. from approximately 36{degree} 00 minutes N to 35{degree} 20 minutes N is a region of relatively rapid sediment accumulation, organic matter deposition and subsequent remineralization. The measured fluxes are the highest reported for the slope off the eastern US Sediment accumulation rates range from 40 to 140 cm ky{sup -1}. Organic carbon deposition rates range from 3.5 to 7.4 moles C m{sup -2} yr{sup -1}. The areal coverage of this ''depocenter'' is probably controlled by interactions between physical oceanographic processes and the rugged topography of the seafloor. The organic matter deposited on the seafloor is primarily marine in origin and a mix of old and fresh particles. 73-93% of the depositing detritus is rapidly oxidized near the sediment/water interface. The controls on subsurface remineralization appear to be a complex function of the relative amount of metabolizable carbon delivered to the seabed both now and in the distant past (>=500ybp) and the extent of seabed irrigation. The age of DIC and CH{sub 4} produced within the seabed indicates that relatively young, reactive carbon is advected below the sediment surface and fuels subsurface remineralization. The stable isotopic composition of DIC produced within the seabed indicates the selective degradation of {sup 13}C-enriched fractions of the organic matter. The metabolizable fraction has a carbon isotopic signature of approx. -18{per_thousand};, while the organic matter that survives degradation and is buried has a d {sup 13}C closer to -20{per_thousand}.
在北纬36{°}00分至35{°}20分之间,北纬36{°}00分至35{°}20分之间的哈特拉斯角陆坡是一个相对快速的沉积物堆积、有机质沉积和再矿化的区域。据报道,美国东部斜坡的测量通量最高,沉积物积累速率为40至140厘米/天。有机碳沉积速率为3.5 ~ 7.4 mol cm {sup -2} yr{sup -1}。这个“沉积中心”的面积可能是由海洋物理过程和海底崎岖地形之间的相互作用控制的。沉积在海底的有机物主要来自海洋,是新旧颗粒的混合物。73-93%的沉积碎屑在沉积物/水界面附近被快速氧化。对地下再矿化的控制似乎是一个复杂的函数,包括现在和遥远的过去(>=500ybp)输送到海底的可代谢碳的相对量和海底灌溉的程度。海床内产生的DIC和CH{sub 4}的年龄表明,相对年轻的活性碳被平流到沉积物表面以下,并为地下再矿化提供燃料。海底产生的DIC的稳定同位素组成表明有机质中{sup 13} c富组分的选择性降解。可代谢部分的碳同位素特征约为。-18{per_thousand};,而存活下来并被掩埋的有机物的d {sup 13}C更接近于-20{per_thousand}。
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引用次数: 2
On the transport of the gulf stream between cape hatteras and the grand banks 关于哈特拉斯角和大浅滩之间的墨西哥湾流的运输
Pub Date : 1992-07-01 DOI: 10.1016/0198-0149(92)90066-3
N. Hogg
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引用次数: 139
Carbon and nitrogen export during the JGOFS North Atlantic Bloom experiment estimated from 234Th: 238U disequilibria 由234:238U不平衡估算的JGOFS北大西洋水华实验期间的碳氮输出
Pub Date : 1992-07-01 DOI: 10.1016/0198-0149(92)90060-7
K. Buesseler, M. Bacon, J. Cochran, H. Livingston
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引用次数: 424
Nutrient dynamics and new production in a warm-core eddy from the Eastern Mediterranean Sea 东地中海暖核涡旋的营养动态和新产物
Pub Date : 1992-03-01 DOI: 10.1016/0198-0149(92)90083-6
M. Krom, S. Brenner, N. Kress, A. Neori, L. Gordon
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引用次数: 156
Biomass of bacteria, cyanobacteria, prochlorophytes and photosynthetic eukaryotes in the Sargasso Sea 马尾藻海中细菌、蓝藻、原绿藻和光合真核生物的生物量
Pub Date : 1992-03-01 DOI: 10.1016/0198-0149(92)90085-8
William K. W. Li, P. Dickie, B. Irwin, A. Wood
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引用次数: 236
Design and calibration of a new optical plankton counter capable of sizing small zooplankton 一种新型光学浮游生物计数器的设计和校准,能够测定小型浮游动物的大小
Pub Date : 1992-03-01 DOI: 10.1016/0198-0149(92)90080-D
A. Herman
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引用次数: 217
Experimental evidence for filter-feeding by the hydrothermal vent mussel, Bathymodiolus thermophilus 热液喷口贻贝滤食的实验证据
Pub Date : 1991-12-01 DOI: 10.1016/0198-0149(91)90084-S
H. Page, A. Fiala-Médioni, C. Fisher, J. Childress
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引用次数: 115
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