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从静脉血氧廓清中得到的启示:潜水加利福尼亚海狮的氧利用和管理。

Insights from venous oxygen profiles: oxygen utilization and management in diving California sea lions.

机构信息

Center for Marine Biotechnology and Biomedicine, Scripps Institution of Oceanography, La Jolla, CA 92093-0204, USA.

出版信息

J Exp Biol. 2013 Sep 1;216(Pt 17):3332-41. doi: 10.1242/jeb.085985.

Abstract

The management and depletion of O2 stores underlie the aerobic dive capacities of marine mammals. The California sea lion (Zalophus californianus) presumably optimizes O2 store management during all dives, but approaches its physiological limits during deep dives to greater than 300 m depth. Blood O2 comprises the largest component of total body O2 stores in adult sea lions. Therefore, we investigated venous blood O2 depletion during dives of California sea lions during maternal foraging trips to sea by: (1) recording venous partial pressure of O2 (P(O2)) profiles during dives, (2) characterizing the O2-hemoglobin (Hb) dissociation curve of sea lion Hb and (3) converting the P(O2) profiles into percent Hb saturation (S(O2)) profiles using the dissociation curve. The O2-Hb dissociation curve was typical of other pinnipeds (P50=28±2 mmHg at pH 7.4). In 43% of dives, initial venous S(O2) values were greater than 78% (estimated resting venous S(O2)), indicative of arterialization of venous blood. Blood O2 was far from depleted during routine shallow dives, with minimum venous S(O2) values routinely greater than 50%. However, in deep dives greater than 4 min in duration, venous S(O2) reached minimum values below 5% prior to the end of the dive, but then increased during the last 30-60 s of ascent. These deep dive profiles were consistent with transient venous blood O2 depletion followed by partial restoration of venous O2 through pulmonary gas exchange and peripheral blood flow during ascent. These differences in venous O2 profiles between shallow and deep dives of sea lions reflect distinct strategies of O2 store management and suggest that underlying cardiovascular responses will also differ.

摘要

氧气储存的管理和消耗是海洋哺乳动物有氧潜水能力的基础。加利福尼亚海狮(Zalophus californianus)在所有潜水过程中可能都会优化氧气储存管理,但在深度超过 300 米的深潜中会接近其生理极限。血液中的氧气是成年海狮体内总氧气储存的最大组成部分。因此,我们通过以下方式研究了加利福尼亚海狮在母性觅食期间进行海上潜水时的静脉血氧耗竭情况:(1)记录潜水过程中的静脉血氧分压(P(O2))曲线,(2)描述海狮血红蛋白(Hb)的氧合血红蛋白(Hb)解离曲线,(3)使用解离曲线将 P(O2)曲线转换为血红蛋白饱和度(S(O2))曲线。海狮的氧合血红蛋白解离曲线与其他鳍足类动物典型的曲线相似(在 pH 值为 7.4 时 P50=28±2mmHg)。在 43%的潜水过程中,初始静脉 S(O2)值大于 78%(估计静息静脉 S(O2)),表明静脉血发生了动脉化。在常规的浅潜水过程中,血液中的氧气几乎没有耗尽,最小静脉 S(O2)值通常大于 50%。然而,在持续时间超过 4 分钟的深潜中,静脉 S(O2)在潜水结束前降至 5%以下,但在上升的最后 30-60 秒内会增加。这些深潜曲线与短暂的静脉血氧耗竭一致,随后通过肺部气体交换和上升过程中的外周血流部分恢复静脉血氧。海狮浅潜和深潜之间静脉血氧廓清曲线的差异反映了氧气储存管理的不同策略,并表明潜在的心血管反应也会有所不同。

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